Articles | Volume 9, issue 6
https://doi.org/10.5194/se-9-1375-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-1375-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Nov 2018
Research article |
| 29 Nov 2018
New insights on the early Mesozoic evolution of multiple tectonic regimes in the northeastern North China Craton from the detrital zircon provenance of sedimentary strata
Yi Ni Wang
College of Earth Sciences, Jilin University, Changchun, 130061, China
Wen Liang Xu
CORRESPONDING AUTHOR
College of Earth Sciences, Jilin University, Changchun, 130061, China
Key Laboratory of Mineral Resources Evaluation in Northeast Asia,
Ministry of Land and Resources of China, Changchun, 130061, China
Feng Wang
College of Earth Sciences, Jilin University, Changchun, 130061, China
Xiao Bo Li
College of Earth Sciences, Jilin University, Changchun, 130061, China
Related subject area
Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Structural geology and tectonics, paleoseismology, rock physics, experimental deformation | Discipline: Tectonics
Analogue modelling of basin inversion: a review and future perspectives
Insights into the interaction of a shale with CO2
Tectonostratigraphic evolution of the Slyne Basin
Control of crustal strength, tectonic inheritance, and stretching/ shortening rates on crustal deformation and basin reactivation: insights from laboratory models
Construction of the Ukrainian Carpathian Wedge from low-temperature thermochronology and tectono-stratigraphic analysis
Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)
The analysis of slip tendency of major tectonic faults in Germany
Earthquake ruptures and topography of the Chilean margin controlled by plate interface deformation
Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines
Rare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scale
Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building
The Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiences
Chronology of thrust propagation from an updated tectono-sedimentary framework of the Miocene molasse (western Alps)
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq
The Subhercynian Basin: an example of an intraplate foreland basin due to a broken plate
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
Holocene surface-rupturing earthquakes on the Dinaric Fault System, western Slovenia
Contribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tilting
Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics
Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models
Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids
Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece
Stress rotation – impact and interaction of rock stiffness and faults
Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift
Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Effects of basal drag on subduction dynamics from 2D numerical models
Hydrocarbon accumulation in basins with multiple phases of extension and inversion: examples from the Western Desert (Egypt) and the western Black Sea
Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes
A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The enigmatic curvature of Central Iberia and its puzzling kinematics
Control of 3-D tectonic inheritance on fold-and-thrust belts: insights from 3-D numerical models and application to the Helvetic nappe system
Plio-Quaternary tectonic evolution of the southern margin of the Alboran Basin (Western Mediterranean)
Surface deformation relating to the 2018 Lake Muir earthquake sequence, southwest Western Australia: new insight into stable continental region earthquakes
Seismic reflection data reveal the 3D structure of the newly discovered Exmouth Dyke Swarm, offshore NW Australia
Cenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monazite
Uncertainties in break-up markers along the Iberia–Newfoundland margins illustrated by new seismic data
Tectonic inheritance controls nappe detachment, transport and stacking in the Helvetic nappe system, Switzerland: insights from thermomechanical simulations
Can subduction initiation at a transform fault be spontaneous?
The Geodynamic World Builder: a solution for complex initial conditions in numerical modeling
From mapped faults to fault-length earthquake magnitude (FLEM): a test on Italy with methodological implications
Lithosphere tearing along STEP faults and synkinematic formation of lherzolite and wehrlite in the shallow subcontinental mantle
A systematic comparison of experimental set-ups for modelling extensional tectonics
Improving subduction interface implementation in dynamic numerical models
The Bortoluzzi Mud Volcano (Ionian Sea, Italy) and its potential for tracking the seismic cycle of active faults
The Ulakhan fault surface rupture and the seismicity of the Okhotsk–North America plate boundary
Control of increased sedimentation on orogenic fold-and-thrust belt structure – insights into the evolution of the Western Alps
Anticlockwise metamorphic pressure–temperature paths and nappe stacking in the Reisa Nappe Complex in the Scandinavian Caledonides, northern Norway: evidence for weakening of lower continental crust before and during continental collision
Frank Zwaan, Guido Schreurs, Susanne J. H. Buiter, Oriol Ferrer, Riccardo Reitano, Michael Rudolf, and Ernst Willingshofer
Solid Earth, 13, 1859–1905, https://doi.org/10.5194/se-13-1859-2022, https://doi.org/10.5194/se-13-1859-2022, 2022
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When a sedimentary basin is subjected to compressional tectonic forces after its formation, it may be inverted. A thorough understanding of such
basin inversionis of great importance for scientific, societal, and economic reasons, and analogue tectonic models form a key part of our efforts to study these processes. We review the advances in the field of basin inversion modelling, showing how the modelling results can be applied, and we identify promising venues for future research.
Eleni Stavropoulou and Lyesse Laloui
Solid Earth, 13, 1823–1841, https://doi.org/10.5194/se-13-1823-2022, https://doi.org/10.5194/se-13-1823-2022, 2022
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Shales are identified as suitable caprock formations for geolocigal CO2 storage thanks to their low permeability. Here, small-sized shale samples are studied under field-representative conditions with X-ray tomography. The geochemical impact of CO2 on calcite-rich zones is for the first time visualised, the role of pre-existing micro-fissures in the CO2 invasion trapping in the matererial is highlighted, and the initiation of micro-cracks when in contact with anhydrous CO2 is demonstrated.
Conor M. O'Sullivan, Conrad J. Childs, Muhammad M. Saqab, John J. Walsh, and Patrick M. Shannon
Solid Earth, 13, 1649–1671, https://doi.org/10.5194/se-13-1649-2022, https://doi.org/10.5194/se-13-1649-2022, 2022
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The Slyne Basin is a sedimentary basin located offshore north-western Ireland. It formed through a long and complex evolution involving distinct periods of extension. The basin is subdivided into smaller basins, separated by deep structures related to the ancient Caledonian mountain-building event. These deep structures influence the shape of the basin as it evolves in a relatively unique way, where early faults follow these deep structures, but later faults do not.
Benjamin Guillaume, Guido M. Gianni, Jean-Jacques Kermarrec, and Khaled Bock
Solid Earth, 13, 1393–1414, https://doi.org/10.5194/se-13-1393-2022, https://doi.org/10.5194/se-13-1393-2022, 2022
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Under tectonic forces, the upper part of the crust can break along different types of faults, depending on the orientation of the applied stresses. Using scaled analogue models, we show that the relative magnitude of compressional and extensional forces as well as the presence of inherited structures resulting from previous stages of deformation control the location and type of faults. Our results gives insights into the tectonic evolution of areas showing complex patterns of deformation.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
EGUsphere, https://doi.org/10.5194/egusphere-2022-828, https://doi.org/10.5194/egusphere-2022-828, 2022
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We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial and subsequent exhumation of the wedge’s nappes, from 34 to ~12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
Andrzej Głuszyński and Paweł Aleksandrowski
Solid Earth, 13, 1219–1242, https://doi.org/10.5194/se-13-1219-2022, https://doi.org/10.5194/se-13-1219-2022, 2022
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Old seismic data recently reprocessed with modern software allowed us to study at depth the Late Cretaceous tectonic structures in the Permo-Mesozoic rock sequences in the Sudetes. The structures formed in response to Iberia collision with continental Europe. The NE–SW compression undulated the crystalline basement top and produced folds, faults and joints in the sedimentary cover. Our results are of importance for regional geology and in prospecting for deep thermal waters.
Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, and Frank Schilling
Solid Earth, 13, 1087–1105, https://doi.org/10.5194/se-13-1087-2022, https://doi.org/10.5194/se-13-1087-2022, 2022
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Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
Nadaya Cubas, Philippe Agard, and Roxane Tissandier
Solid Earth, 13, 779–792, https://doi.org/10.5194/se-13-779-2022, https://doi.org/10.5194/se-13-779-2022, 2022
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Earthquake extent prediction is limited by our poor understanding of slip deficit patterns. From a mechanical analysis applied along the Chilean margin, we show that earthquakes are bounded by extensive plate interface deformation. This deformation promotes stress build-up, leading to earthquake nucleation; earthquakes then propagate along smoothed fault planes and are stopped by heterogeneously distributed deformation. Slip deficit patterns reflect the spatial distribution of this deformation.
Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha
Solid Earth, 13, 553–582, https://doi.org/10.5194/se-13-553-2022, https://doi.org/10.5194/se-13-553-2022, 2022
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We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
Malcolm Aranha, Alok Porwal, Manikandan Sundaralingam, Ignacio González-Álvarez, Amber Markan, and Karunakar Rao
Solid Earth, 13, 497–518, https://doi.org/10.5194/se-13-497-2022, https://doi.org/10.5194/se-13-497-2022, 2022
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Rare earth elements (REEs) are considered critical mineral resources for future industrial growth due to their short supply and rising demand. This study applied an artificial-intelligence-based technique to target potential REE-deposit hosting areas in western Rajasthan, India. Uncertainties associated with the prospective targets were also estimated to aid decision-making. The presented workflow can be applied to similar regions elsewhere to locate potential zones of REE mineralisation.
Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita de Nardis, Debora Presti, Federica Ferrarini, Simone Bello, and Francesco Brozzetti
Solid Earth, 13, 205–228, https://doi.org/10.5194/se-13-205-2022, https://doi.org/10.5194/se-13-205-2022, 2022
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The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.
Steven Whitmeyer, Lynn Fichter, Anita Marshall, and Hannah Liddle
Solid Earth, 12, 2803–2820, https://doi.org/10.5194/se-12-2803-2021, https://doi.org/10.5194/se-12-2803-2021, 2021
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Field trips in the Stratigraphy, Structure, Tectonics (SST) course transitioned to a virtual format in Fall 2020, due to the COVID pandemic. Virtual field experiences (VFEs) were developed in web Google Earth and were evaluated in comparison with on-location field trips via an online survey. Students recognized the value of VFEs for revisiting outcrops and noted improved accessibility for students with disabilities. Potential benefits of hybrid field experiences were also indicated.
Amir Kalifi, Philippe Hervé Leloup, Philippe Sorrel, Albert Galy, François Demory, Vincenzo Spina, Bastien Huet, Frédéric Quillévéré, Frédéric Ricciardi, Daniel Michoux, Kilian Lecacheur, Romain Grime, Bernard Pittet, and Jean-Loup Rubino
Solid Earth, 12, 2735–2771, https://doi.org/10.5194/se-12-2735-2021, https://doi.org/10.5194/se-12-2735-2021, 2021
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Molasse deposits, deposited and deformed at the western Alpine front during the Miocene (23 to 5.6 Ma), record the chronology of that deformation. We combine the first precise chronostratigraphy (precision of ∼0.5 Ma) of the Miocene molasse, the reappraisal of the regional structure, and the analysis of growth deformation structures in order to document three tectonic phases and the precise chronology of thrust westward propagation during the second one involving the Belledonne basal thrust.
Mark R. Handy, Stefan M. Schmid, Marcel Paffrath, Wolfgang Friederich, and the AlpArray Working Group
Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, https://doi.org/10.5194/se-12-2633-2021, 2021
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New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
Maurizio Ercoli, Daniele Cirillo, Cristina Pauselli, Harry M. Jol, and Francesco Brozzetti
Solid Earth, 12, 2573–2596, https://doi.org/10.5194/se-12-2573-2021, https://doi.org/10.5194/se-12-2573-2021, 2021
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Past strong earthquakes can produce topographic deformations, often
memorizedin Quaternary sediments, which are typically studied by paleoseismologists through trenching. Using a ground-penetrating radar (GPR), we unveiled possible buried Quaternary faulting in the Mt. Pollino seismic gap region (southern Italy). We aim to contribute to seismic hazard assessment of an area potentially prone to destructive events as well as promote our workflow in similar contexts around the world.
Luca Smeraglia, Nathan Looser, Olivier Fabbri, Flavien Choulet, Marcel Guillong, and Stefano M. Bernasconi
Solid Earth, 12, 2539–2551, https://doi.org/10.5194/se-12-2539-2021, https://doi.org/10.5194/se-12-2539-2021, 2021
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In this paper, we dated fault movements at geological timescales which uplifted the sedimentary successions of the Jura Mountains from below the sea level up to Earth's surface. To do so, we applied the novel technique of U–Pb geochronology on calcite mineralizations that precipitated on fault surfaces during times of tectonic activity. Our results document a time frame of the tectonic evolution of the Jura Mountains and provide new insight into the broad geological history of the Western Alps.
Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli
Solid Earth, 12, 2479–2501, https://doi.org/10.5194/se-12-2479-2021, https://doi.org/10.5194/se-12-2479-2021, 2021
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As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.
David Hindle and Jonas Kley
Solid Earth, 12, 2425–2438, https://doi.org/10.5194/se-12-2425-2021, https://doi.org/10.5194/se-12-2425-2021, 2021
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Central western Europe underwent a strange episode of lithospheric deformation, resulting in a chain of small mountains that run almost west–east across the continent and that formed in the middle of a tectonic plate, not at its edges as is usually expected. Associated with these mountains, in particular the Harz in central Germany, are marine basins contemporaneous with the mountain growth. We explain how those basins came to be as a result of the mountains bending the adjacent plate.
Andreas Eberts, Hamed Fazlikhani, Wolfgang Bauer, Harald Stollhofen, Helga de Wall, and Gerald Gabriel
Solid Earth, 12, 2277–2301, https://doi.org/10.5194/se-12-2277-2021, https://doi.org/10.5194/se-12-2277-2021, 2021
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We combine gravity anomaly and topographic data with observations from thermochronology, metamorphic grades, and the granite inventory to detect patterns of basement block segmentation and differential exhumation along the southwestern Bohemian Massif. Based on our analyses, we introduce a previously unknown tectonic structure termed Cham Fault, which, together with the Pfahl and Danube shear zones, is responsible for the exposure of different crustal levels during late to post-Variscan times.
Christoph Grützner, Simone Aschenbrenner, Petra Jamšek
Rupnik, Klaus Reicherter, Nour Saifelislam, Blaž Vičič, Marko Vrabec, Julian Welte, and Kamil Ustaszewski
Solid Earth, 12, 2211–2234, https://doi.org/10.5194/se-12-2211-2021, https://doi.org/10.5194/se-12-2211-2021, 2021
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Several large strike-slip faults in western Slovenia are known to be active, but most of them have not produced strong earthquakes in historical times. In this study we use geomorphology, near-surface geophysics, and fault excavations to show that two of these faults had surface-rupturing earthquakes during the Holocene. Instrumental and historical seismicity data do not capture the strongest events in this area.
Michael Warsitzka, Prokop Závada, Fabian Jähne-Klingberg, and Piotr Krzywiec
Solid Earth, 12, 1987–2020, https://doi.org/10.5194/se-12-1987-2021, https://doi.org/10.5194/se-12-1987-2021, 2021
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A new analogue modelling approach was used to simulate the influence of tectonic extension and tilting of the basin floor on salt tectonics in rift basins. Our results show that downward salt flow and gravity gliding takes place if the flanks of the rift basin are tilted. Thus, extension occurs at the basin margins, which is compensated for by reduced extension and later by shortening in the graben centre. These outcomes improve the reconstruction of salt-related structures in rift basins.
Torsten Hundebøl Hansen, Ole Rønø Clausen, and Katrine Juul Andresen
Solid Earth, 12, 1719–1747, https://doi.org/10.5194/se-12-1719-2021, https://doi.org/10.5194/se-12-1719-2021, 2021
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We have analysed the role of deep salt layers during tectonic shortening of a group of sedimentary basins buried below the North Sea. Due to the ability of salt to flow over geological timescales, the salt layers are much weaker than the surrounding rocks during tectonic deformation. Therefore, complex structures formed mainly where salt was present in our study area. Our results align with findings from other basins and experiments, underlining the importance of salt tectonics.
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, https://doi.org/10.5194/se-12-1473-2021, 2021
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We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
Laurent Jolivet, Laurent Arbaret, Laetitia Le Pourhiet, Florent Cheval-Garabédian, Vincent Roche, Aurélien Rabillard, and Loïc Labrousse
Solid Earth, 12, 1357–1388, https://doi.org/10.5194/se-12-1357-2021, https://doi.org/10.5194/se-12-1357-2021, 2021
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Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.
Miguel Cisneros, Jaime D. Barnes, Whitney M. Behr, Alissa J. Kotowski, Daniel F. Stockli, and Konstantinos Soukis
Solid Earth, 12, 1335–1355, https://doi.org/10.5194/se-12-1335-2021, https://doi.org/10.5194/se-12-1335-2021, 2021
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Constraining the conditions at which rocks form is crucial for understanding geologic processes. For years, the conditions under which rocks from Syros, Greece, formed have remained enigmatic; yet these rocks are fundamental for understanding processes occurring at the interface between colliding tectonic plates (subduction zones). Here, we constrain conditions under which these rocks formed and show they were transported to the surface adjacent to the down-going (subducting) tectonic plate.
Karsten Reiter
Solid Earth, 12, 1287–1307, https://doi.org/10.5194/se-12-1287-2021, https://doi.org/10.5194/se-12-1287-2021, 2021
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The influence and interaction of elastic material properties (Young's modulus, Poisson's ratio), density and low-friction faults on the resulting far-field stress pattern in the Earth's crust is tested with generic models. A Young's modulus contrast can lead to a significant stress rotation. Discontinuities with low friction in homogeneous models change the stress pattern only slightly, away from the fault. In addition, active discontinuities are able to compensate stress rotation.
Hilmar von Eynatten, Jonas Kley, István Dunkl, Veit-Enno Hoffmann, and Annemarie Simon
Solid Earth, 12, 935–958, https://doi.org/10.5194/se-12-935-2021, https://doi.org/10.5194/se-12-935-2021, 2021
Eline Le Breton, Sascha Brune, Kamil Ustaszewski, Sabin Zahirovic, Maria Seton, and R. Dietmar Müller
Solid Earth, 12, 885–913, https://doi.org/10.5194/se-12-885-2021, https://doi.org/10.5194/se-12-885-2021, 2021
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The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic, opened as an arm of the central Atlantic. Using plate reconstructions and geodynamic modeling, we show that the ocean reached only 250 km width between Europe and Adria. Moreover, at least 65 % of the lithosphere subducted into the mantle and/or incorporated into the Alps during convergence in Cretaceous and Cenozoic times comprised highly thinned continental crust, while only 35 % was truly oceanic.
Lior Suchoy, Saskia Goes, Benjamin Maunder, Fanny Garel, and Rhodri Davies
Solid Earth, 12, 79–93, https://doi.org/10.5194/se-12-79-2021, https://doi.org/10.5194/se-12-79-2021, 2021
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We use 2D numerical models to highlight the role of basal drag in subduction force balance. We show that basal drag can significantly affect velocities and evolution in our simulations and suggest an explanation as to why there are no trends in plate velocities with age in the Cenozoic subduction record (which we extracted from recent reconstruction using GPlates). The insights into the role of basal drag will help set up global models of plate dynamics or specific regional subduction models.
William Bosworth and Gábor Tari
Solid Earth, 12, 59–77, https://doi.org/10.5194/se-12-59-2021, https://doi.org/10.5194/se-12-59-2021, 2021
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Many of the world's hydrocarbon resources are found in rifted sedimentary basins. Some rifts experience multiple phases of extension and inversion. This results in complicated oil and gas generation, migration, and entrapment histories. We present examples of basins in the Western Desert of Egypt and the western Black Sea that were inverted multiple times, sometimes separated by additional phases of extension. We then discuss how these complex deformation histories impact exploration campaigns.
Samuel Mock, Christoph von Hagke, Fritz Schlunegger, István Dunkl, and Marco Herwegh
Solid Earth, 11, 1823–1847, https://doi.org/10.5194/se-11-1823-2020, https://doi.org/10.5194/se-11-1823-2020, 2020
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Based on thermochronological data, we infer thrusting along-strike the northern rim of the Central Alps between 12–4 Ma. While the lithology influences the pattern of thrusting at the local scale, we observe that thrusting in the foreland is a long-wavelength feature occurring between Lake Geneva and Salzburg. This coincides with the geometry and dynamics of the attached lithospheric slab at depth. Thus, thrusting in the foreland is at least partly linked to changes in slab dynamics.
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332, https://doi.org/10.5194/se-11-1313-2020, https://doi.org/10.5194/se-11-1313-2020, 2020
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We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
Daniel Pastor-Galán, Gabriel Gutiérrez-Alonso, and Arlo B. Weil
Solid Earth, 11, 1247–1273, https://doi.org/10.5194/se-11-1247-2020, https://doi.org/10.5194/se-11-1247-2020, 2020
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Pangea was assembled during Devonian to early Permian times and resulted in a large-scale and winding orogeny that today transects Europe, northwestern Africa, and eastern North America. This orogen is characterized by an
Sshape corrugated geometry in Iberia. This paper presents the advances and milestones in our understanding of the geometry and kinematics of the Central Iberian curve from the last decade with particular attention paid to structural and paleomagnetic studies.
Richard Spitz, Arthur Bauville, Jean-Luc Epard, Boris J. P. Kaus, Anton A. Popov, and Stefan M. Schmalholz
Solid Earth, 11, 999–1026, https://doi.org/10.5194/se-11-999-2020, https://doi.org/10.5194/se-11-999-2020, 2020
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We apply three-dimensional (3D) thermo-mechanical numerical simulations of the shortening of the upper crustal region of a passive margin in order to investigate the control of 3D laterally variable inherited structures on fold-and-thrust belt evolution and associated nappe formation. The model is applied to the Helvetic nappe system of the Swiss Alps. Our results show a 3D reconstruction of the first-order tectonic evolution showing the fundamental importance of inherited geological structures.
Manfred Lafosse, Elia d'Acremont, Alain Rabaute, Ferran Estrada, Martin Jollivet-Castelot, Juan Tomas Vazquez, Jesus Galindo-Zaldivar, Gemma Ercilla, Belen Alonso, Jeroen Smit, Abdellah Ammar, and Christian Gorini
Solid Earth, 11, 741–765, https://doi.org/10.5194/se-11-741-2020, https://doi.org/10.5194/se-11-741-2020, 2020
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The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
Dan J. Clark, Sarah Brennand, Gregory Brenn, Matthew C. Garthwaite, Jesse Dimech, Trevor I. Allen, and Sean Standen
Solid Earth, 11, 691–717, https://doi.org/10.5194/se-11-691-2020, https://doi.org/10.5194/se-11-691-2020, 2020
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A magnitude 5.3 reverse-faulting earthquake in September 2018 near Lake Muir in southwest Western Australia was followed after 2 months by a collocated magnitude 5.2 strike-slip event. The first event produced a ~ 5 km long and up to 0.5 m high west-facing surface rupture, and the second triggered event deformed but did not rupture the surface. The earthquake sequence was the ninth to have produced surface rupture in Australia. None of these show evidence for prior Quaternary surface rupture.
Craig Magee and Christopher Aiden-Lee Jackson
Solid Earth, 11, 579–606, https://doi.org/10.5194/se-11-579-2020, https://doi.org/10.5194/se-11-579-2020, 2020
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Injection of vertical sheets of magma (dyke swarms) controls tectonic and volcanic processes on Earth and other planets. Yet we know little of the 3D structure of dyke swarms. We use seismic reflection data, which provides ultrasound-like images of Earth's subsurface, to study a dyke swarm in 3D for the first time. We show that (1) dyke injection occurred in the Late Jurassic, (2) our data support previous models of dyke shape, and (3) seismic data provides a new way to view and study dykes.
Emmanuelle Ricchi, Christian A. Bergemann, Edwin Gnos, Alfons Berger, Daniela Rubatto, Martin J. Whitehouse, and Franz Walter
Solid Earth, 11, 437–467, https://doi.org/10.5194/se-11-437-2020, https://doi.org/10.5194/se-11-437-2020, 2020
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This study investigates Cenozoic deformation during cooling and exhumation of the Tauern metamorphic and structural dome, Eastern Alps, through Th–Pb dating of fissure monazite-(Ce). Fissure (or hydrothermal) monazite-(Ce) typically crystallizes in a temperature range of 400–200 °C. Three major episodes of monazite growth occurred at approximately 21, 17, and 12 Ma, corroborating previous crystallization and cooling ages.
Annabel Causer, Lucía Pérez-Díaz, Jürgen Adam, and Graeme Eagles
Solid Earth, 11, 397–417, https://doi.org/10.5194/se-11-397-2020, https://doi.org/10.5194/se-11-397-2020, 2020
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Here we discuss the validity of so-called “break-up” markers along the Newfoundland margin, challenging their perceived suitability for plate kinematic reconstructions of the southern North Atlantic. We do this on the basis of newly available seismic transects across the Southern Newfoundland Basin. Our new data contradicts current interpretations of the extent of oceanic lithosphere and illustrates the need for a differently constraining the plate kinematics of the Iberian plate pre M0 times.
Dániel Kiss, Thibault Duretz, and Stefan Markus Schmalholz
Solid Earth, 11, 287–305, https://doi.org/10.5194/se-11-287-2020, https://doi.org/10.5194/se-11-287-2020, 2020
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In this paper, we investigate the physical mechanisms of tectonic nappe formation by high-resolution numerical modeling. Tectonic nappes are key structural features of many mountain chains which are packets of rocks displaced, sometimes even up to 100 km, from their original position. However, the physical mechanisms involved are not fully understood. We solve numerical equations of fluid and solid dynamics to improve our knowledge. The results are compared with data from the Helvetic Alps.
Diane Arcay, Serge Lallemand, Sarah Abecassis, and Fanny Garel
Solid Earth, 11, 37–62, https://doi.org/10.5194/se-11-37-2020, https://doi.org/10.5194/se-11-37-2020, 2020
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We propose a new exploration of the concept of
spontaneouslithospheric collapse at a transform fault (TF) by performing a large study of conditions allowing instability of the thicker plate using 2-D thermomechanical simulations. Spontaneous subduction is modelled only if extreme mechanical conditions are assumed. We conclude that spontaneous collapse of the thick older plate at a TF evolving into mature subduction is an unlikely process of subduction initiation at modern Earth conditions.
Menno Fraters, Cedric Thieulot, Arie van den Berg, and Wim Spakman
Solid Earth, 10, 1785–1807, https://doi.org/10.5194/se-10-1785-2019, https://doi.org/10.5194/se-10-1785-2019, 2019
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Three-dimensional numerical modelling of geodynamic processes may benefit strongly from using realistic 3-D starting models that approximate, e.g. natural subduction settings in the geological past or at present. To this end, we developed the Geodynamic World Builder (GWB), which enables relatively straightforward parameterization of complex 3-D geometric structures associated with geodynamic processes. The GWB is an open-source community code designed to easily interface with geodynamic codes.
Fabio Trippetta, Patrizio Petricca, Andrea Billi, Cristiano Collettini, Marco Cuffaro, Anna Maria Lombardi, Davide Scrocca, Giancarlo Ventura, Andrea Morgante, and Carlo Doglioni
Solid Earth, 10, 1555–1579, https://doi.org/10.5194/se-10-1555-2019, https://doi.org/10.5194/se-10-1555-2019, 2019
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Considering all mapped faults in Italy, empirical scaling laws between fault dimensions and earthquake magnitude are used at the national scale. Results are compared with earthquake catalogues. The consistency between our results and the catalogues gives credibility to the method. Some large differences between the two datasets suggest the validation of this experiment elsewhere.
Károly Hidas, Carlos J. Garrido, Guillermo Booth-Rea, Claudio Marchesi, Jean-Louis Bodinier, Jean-Marie Dautria, Amina Louni-Hacini, and Abla Azzouni-Sekkal
Solid Earth, 10, 1099–1121, https://doi.org/10.5194/se-10-1099-2019, https://doi.org/10.5194/se-10-1099-2019, 2019
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Subduction-transform edge propagator (STEP) faults are the locus of continual lithospheric tearing at the edges of subducted slabs, resulting in sharp changes in the lithospheric thickness and triggering lateral and/or near-vertical mantle flow. Here, we study upper mantle rocks recovered from a STEP fault context by < 4 Ma alkali volcanism. We reconstruct how the microstructure developed during deformation and coupled melt–rock interaction, which are promoted by lithospheric tearing at depth.
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097, https://doi.org/10.5194/se-10-1063-2019, https://doi.org/10.5194/se-10-1063-2019, 2019
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This work was inspired by an effort to numerically reproduce laboratory models of extension tectonics. We tested various set-ups to find a suitable analogue model and in the process systematically charted the impact of set-ups and boundary conditions on model results, a topic poorly described in existing scientific literature. We hope that our model results and the discussion on which specific tectonic settings they could represent may serve as a guide for future (analogue) modeling studies.
Dan Sandiford and Louis Moresi
Solid Earth, 10, 969–985, https://doi.org/10.5194/se-10-969-2019, https://doi.org/10.5194/se-10-969-2019, 2019
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This study investigates approaches to implementing plate boundaries within a fluid dynamic framework, targeted at the evolution of subduction over many millions of years.
Marco Cuffaro, Andrea Billi, Sabina Bigi, Alessandro Bosman, Cinzia G. Caruso, Alessia Conti, Andrea Corbo, Antonio Costanza, Giuseppe D'Anna, Carlo Doglioni, Paolo Esestime, Gioacchino Fertitta, Luca Gasperini, Francesco Italiano, Gianluca Lazzaro, Marco Ligi, Manfredi Longo, Eleonora Martorelli, Lorenzo Petracchini, Patrizio Petricca, Alina Polonia, and Tiziana Sgroi
Solid Earth, 10, 741–763, https://doi.org/10.5194/se-10-741-2019, https://doi.org/10.5194/se-10-741-2019, 2019
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The Ionian Sea in southern Italy is at the center of active convergence between the Eurasian and African plates, with many known
Mw > 7.0 earthquakes. Here, a recently discovered mud volcano (called the Bortoluzzi Mud Volcano or BMV) was surveyed during the Seismofaults 2017 cruise (May 2017). The BMV is the active emergence of crustal fluids probably squeezed up during the seismic cycle. As such, the BMV may potentially be used to track the seismic cycle of active faults.
David Hindle, Boris Sedov, Susanne Lindauer, and Kevin Mackey
Solid Earth, 10, 561–580, https://doi.org/10.5194/se-10-561-2019, https://doi.org/10.5194/se-10-561-2019, 2019
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On one of the least studied boundaries between tectonic plates (North America–Okhotsk in northeastern Russia), which moves very similarly to the famous San Andreas fault in California, we have found the traces of earthquakes from the recent past, but before the time of historical records. This makes us a little more sure that the fault is still the place where movement between the plates takes place, and when it happens again, there could be dangerous earthquakes.
Zoltán Erdős, Ritske S. Huismans, and Peter van der Beek
Solid Earth, 10, 391–404, https://doi.org/10.5194/se-10-391-2019, https://doi.org/10.5194/se-10-391-2019, 2019
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We used a 2-D thermomechanical code to simulate the evolution of an orogen. Our aim was to study the interaction between tectonic and surface processes in orogenic forelands. We found that an increase in the sediment input to the foreland results in prolonged activity of the active frontal thrust. Such a scenario could occur naturally as a result of increasing relief in the orogenic hinterland or a change in climatic conditions. We compare our results with observations from the Alps.
Carly Faber, Holger Stünitz, Deta Gasser, Petr Jeřábek, Katrin Kraus, Fernando Corfu, Erling K. Ravna, and Jiří Konopásek
Solid Earth, 10, 117–148, https://doi.org/10.5194/se-10-117-2019, https://doi.org/10.5194/se-10-117-2019, 2019
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The Caledonian mountains formed when Baltica and Laurentia collided around 450–400 million years ago. This work describes the history of the rocks and the dynamics of that continental collision through space and time using field mapping, estimated pressures and temperatures, and age dating on rocks from northern Norway. The rocks preserve continental collision between 440–430 million years ago, and an unusual pressure–temperature evolution suggests unusual tectonic activity prior to collision.
Cited articles
Andersen, T.: Correction of common lead in U–Pb analyses that do not report
204Pb, Chem. Geol., 192, 59–79,
https://doi.org/10.1016/S0009-2541(02)00195-X, 2002.
Beijing Bureau of Geology and Mineral Resources (BBGMR): Regional Geology of
Beijing City, Geological Publishing House, Beijing, 1991 (in Chinese).
Bi, J. H., Ge, W. C., Yang, H., Wang, Z. H., Xu, W. L., Yang, J. H., Xing,
D. H., and Chen, H. J.: Geochronology and geochemistry of Late
Carboniferous–Middle Permian I-and A-type granites and gabbro-diorites in
the eastern Jiamusi Massif, NE China: implications for petrogenesis and
tectonic setting, Lithos, 266–267, 213–232, https://doi.org/10.1016/j.lithos.2016.10.001, 2016.
Cao, H. H., Xu, W. L., Pei, F. P., Guo, P. Y., and Wang, F.: Permian
tectonic evolution of the eastern section of the northern margin of the
North China Plate: constraints from zircon U–Pb geochronology and
geochemistry of the volcanic rocks, Acta Petrol. Sin., 28, 2733–2750, 2012
(in Chinese).
Cao, H. H., Xu, W. L., Pei, F. P., Wang, Z. W., Wang, F., and Wang, Z. J.:
Zircon U–Pb geochronology and petrogenesis of the Late Paleozoic–Early
Mesozoic intrusive rocks in the eastern segment of the northern margin of
the North China Block, Lithos, 170–171, 191–207,
https://doi.org/10.1016/j.lithos.2013.03.006, 2013.
Corfu, F., Hanchar, J. M., Hoskin, P. W. O., and Kinny, P.: Atlas of zircon
textures, Rev. Mineral. Geochem., 53, 469–500,
https://doi.org/10.2113/0530469, 2003.
Cui, S. Q., Li, J. R., Wu, Z. H., Yi, M. C., Shen, S. M., Yin, H. R., and
Ma, Y. S. (Eds.): Mesozoic and Cenozoic intracontinental orogenesis of the
Yanshan area, Geological Publishing House, Beijing, 2002 (in Chinese).
Davis, G. A., Zheng, Y., Wang, C., Darby, B. J., Zhang, C., and Gehrels, G.:
Mesozoic tectonic evolution of the Yanshan fold and thrust belt, with
emphasis on Hebei and Liaoning Province, northern China, Beijing Geology,
194, 171–197, https://doi.org/10.1130/0-8137-1194-0.171, 2001.
Dickinson, W. R. and Gehrels, G. E.: Sediment delivery to the Cordilleran
foreland basin: Insights from U–Pb ages of detrital zircons in upper
Jurassic and Cretaceous strata of the Colorado Plateau, Am. J. Sci., 308,
1041–1082, 2008.
Dong, Y., Ge, W. C., Yang, H., Zhao, G. C., Wang, Q. H., Zhang, Y. L., and
Su, L.: Geochronology and geochemistry of Early Cretaceous volcanic rocks
from the Baiyingaolao Formation in the central great Xing'an Range, NE
China, and its tectonic implications, Lithos, 205, 168–184,
https://doi.org/10.1016/j.lithos.2014.07.004, 2014.
Dong, Y., Ge, W. C., Yang, H., Xu, W. L., Zhang, Y. L., Bi, J. H., and Liu,
X. W.: Geochronology, geochemistry, and Hf isotopes of Jurassic
intermediate-acidic intrusions in the Xing'an Block, northeastern China:
petrogenesis and implications for subduction of the Paleo-Pacific oceanic
plate, J. Asian Earth Sci., 118, 11–31,
https://doi.org/10.1016/j.jseaes.2016.01.006, 2016.
Editing Group for Jilin Stratigraphic Chart (EGJS): The regional
stratigraphic chart in the northeastern China (Jilin Province), Geological
Publishing House, Beijing, 1975 (in Chinese).
Ernst, W. G., Tsujimori, T., Zhang, R., and Liou, J. G.: Permo–Triassic
collision, subduction-zone metamorphism, and tectonic exhumation along the
east Asian continental margin, Annu. Rev. Earth Pl. Sc., 35, 73–110,
https://doi.org/10.1146/annurev.earth.35.031306.140146, 2007.
Fukuyama, M., Ogasawara, M., Horie, K., and Lee, D. C.: Genesis of
jadeite–quartz rocks in the Yorii area of the Kanto mountains, Japan, J.
Asian Earth Sci., 63, 206–217,
https://doi.org/10.1016/j.jseaes.2012.10.031, 2013.
Gao, S., Rudnick, R. L., Yuan, H. L., Liu, X. M., Liu, Y. S., Xu, W. L.,
Liang, W. L., Ayers, J., Wang, X. C., and Wang, Q. H.: Recycling lower
continental crust in the North China Craton, Nature, 432, 892–897,
https://doi.org/10.1038/nature03162, 2004.
Ge, W. C., Wu, F. Y., Zhou, C. Y., and Zhang, J. H.: Porphyry Cu–Mo
deposits in the eastern Xing'an–Mongolia Orogenic Belt: mineralization ages
and their geodynamic implications, Chinese Sci. Bull., 52, 3416–3427,
https://doi.org/10.1007/s11434-007-0466-8, 2007 (in Chinese).
Gill, J. B.: Orogenic Andesites and Plate Tectonics, Springer, New York,
1981.
Guo, F.: Geological records of the Pacific Plate subduction in the northeast
Asian continental magin: an overview, Bull. Mineral. Petrol. Geochem., 35,
1082–1092, https://doi.org/10.3969/j.issn.1007-2082.2016.06.002, 2016.
Hebei Bureau of Geology and Mineral Resources (JBGMR): Regional Geology of
Hebei Province, Geological Publishing House, Beijing, 1989 (in Chinese).
Hu, Z. C., Gao, S., Liu, Y. S., Hu, S. H., Chen, H. H., and Yuan, H. L.:
Signal enhancement in laser ablation ICP–MS by addition of nitrogen in the
central channel gas, J. Anal. Atom. Spectrom., 23, 1093–1101,
https://doi.org/10.1039/B804760J, 2008a.
Hu, Z. C., Liu, Y. S., Gao, S., Hu, S. H., Dietiker, R., and Günther,
D.: A local aerosol extraction strategy for the determination of the aerosol
composition in laser ablation inductively coupled plasma mass spectrometry,
J. Anal. Atom. Spectrom., 23, 1192–1203, https://doi.org/10.1039/b803934h,
2008b.
Hu, Z. C., Liu, Y. S., Gao, S., Liu, W. G., Zhang, W., Tong, X. R., Lin, L.,
Zong, K. Q., Li, M., Chen, H.H., Zhou, L., and Yang, L.: Improved in situ Hf
isotope ratio analysis of zircon using newly designed X skimmer cone and jet
sample cone in combination with the addition of nitrogen by laser ablation
multiple collector ICP–MS, J. Anal. Atom. Spectrom., 27, 1391–1399,
https://doi.org/10.1039/c2ja30078h, 2012.
Inner Mongolia Bureau of Geology and Mineral Resources (IMBGMR): Regional
Geology of Inner Mongolia Province, Geological Publishing House, Beijing,
1991 (in Chinese).
Jahn, B., Capdevila, R., Liu, D., Vernon, A., and Badarch, G.: Sources of
Phanerozoic granitoids in the transect Bayanhongor–Ulaan Baatar, Mongolia:
geochemical and Nd isotopic evidence and implications for Phanerozoic
crustal growth, J. Asian Earth Sci., 23, 629–653,
https://doi.org/10.1016/S1367-9120(03)00125-1, 2004.
Jia, D., Hu, R., Yan, L., and Qiu, X.: Collision belt between the Khanka
block and the North China block in the Yanbian region, northeast China, J.
Asian Earth Sci., 23, 211–219,
https://doi.org/10.1016/S1367-9120(03)00123-8, 2004.
Jilin Bureau of Geology and Mineral Resources (JBGMR): Report of 1:200,000
regional geological research of Manjiang and Changbai area, Jilin Bureau of
Geology and Mineral Resources, Changchun, 1963 (in Chinese).
Jilin Bureau of Geology and Mineral Resources (JBGMR): Report of 1:200,000
regional geological research of Fusong area, Jilin Bureau of Geology and
Mineral Resources, Changchun, 1971 (in Chinese).
Jilin Bureau of Geology and Mineral Resources (JBGMR): Report of 1:200,000
regional geological research of Hunjiang and Ji'an area, Jilin Bureau of
Geology and Mineral Resources, Changchun, 1976 (in Chinese).
Jilin Bureau of Geology and Mineral Resources (JBGMR): Regional Geology of
Jilin Province, Geological Publishing House, Beijing, 1988 (in Chinese).
Jilin Bureau of Geology and Mineral Resources (JBGMR): Stratigraphy of Jilin
Province, China University of Geosciences Press, Wuhan, 1997 (in Chinese).
Jilin Bureau of Geology and Mineral Resources (JBGMR): Report of 1:250,000
regional geological research of Jingyu, Hunjiang, and Changbai area, Jilin
Bureau of Geology and Mineral Resources, Changchun, 2007 (in Chinese).
Li, H. Y. and Huang, X. L.: Constraints on the paleogeographic evolution of
the North China Craton during the Late Triassic–Jurassic, J. Asian Earth
Sci., 70–71, 308–320, https://doi.org/10.1016/j.jseaes.2013.03.028, 2013.
Li, H. Y., Xu, Y. G., Huang, X. L., He, B., Luo, Z. Y., and Yan, B.:
Activation of northern margino f the North China Craton in late Paleozoic:
evidence from U–Pb dating and Hf isotopics of detrial zircons from the
upper Carboniferous Taiyuan Formation in the Ningwu–Jingle basin, Chinese
Sci. Bull., 54, 677–686, https://doi.org/10.1007/s11434-008-0444-9, 2009
(in Chinese).
Li, J. Y.: Permian geodynamic setting of northeast China and adjacent
regions: closure of the Paleo-Asian Ocean and subduction of the
Paleo-Pacific Plate, J. Asian Earth Sci., 26, 207–224,
https://doi.org/10.1016/j.jseaes.2005.09.001, 2006.
Li, J. Y., Niu, B. G., Song, B., Xu, W. X., Zhang, Y. H., and Zhao, Z. R.
(Eds.): Crustal formation and evolution of northern Changbai Mountains,
northeast China, Geological Publishing House, Beijing, 1999 (in Chinese).
Li, J. Y., Gao, L. M., Sun, G. H., Li, Y. P., and Wang, Y. B.: Shuangjingzi
Middle Triassic syn-collisional crust-derived granite in the east Inner
Mongolia and its constraint on the timing of collision between Siberian and
Sino-Korean paleo-plates, Acta Petrol. Sin., 23, 565–582, 2007 (in
Chinese).
Li, X. H., Liu, Y., Li, Q. L., Guo, C. H., and Chamberlain, K. R.: Precise
determination of Phanerozoic zircon Pb/Pb age by multi-collector SIMS
without external standardization, Geochem. Geophy. Geosy., 10, Q04010,
https://doi.org/10.1029/2009GC002400, 2009.
Li, Z. H., Qu, H. J., and Gong, W. B.: Late Mesozoic basin development and
tectonic setting of the northern North China Craton, J. Asian Earth Sci.,
114, 115–139, https://doi.org/10.1016/j.jseaes.2015.05.029, 2015.
Liaoning Bureau of Geology and Mineral Resources (LBGMR): Regional Geology
of Liaoning Province, Geological Publishing House, Beijing, 1989 (in
Chinese).
Lin, Q., Ge, W. C., Sun, D. Y., Wu, F. Y., Chong, K. W., Kyung, D. M.,
Myung, S. J., Moon, W., Chi, S. K., and Sung, H. Y.: Tectonic significance
of Mesozoic volcanic rocks in northeastern China, Sci. Geol. Sin., 33, 129–139, 1998 (in Chinese).
Liu, F. L., Gerdes, A., and Xue, H. M.: Differential subduction and
exhumation of crustal slices in the Sulu Hp–Uhp metamorphic terrane:
insights from mineral inclusions, trace elements, U–Pb and Lu–Hf isotope
analyses of zircon in orthogneiss, J. Metamorph. Geol., 27, 805–825,
https://doi.org/10.1111/j.1525-1314.2009.00833.x, 2009.
Liu, F. L., Gerdes, A., and Liu, P. H.: U–Pb, trace element and Lu–Hf
properties of unique dissolution-reprecipitation zircon from Uhp eclogite in
SW Sulu terrane, eastern China, Gondwana Res., 22, 169–183,
https://doi.org/10.1016/j.gr.2011.11.007, 2012.
Liu, Y. Q., Kuang, H. W., Peng, N., Xu, H., Zhang, P., Wang, N. S., and An,
W.: Mesozoic basins and associated Palaeogeographic evolution in North
China, J. Palaeogeog., 4, 189–202,
https://doi.org/10.3724/SP.J.1261.2015.00073, 2015.
Liu, Y. S., Hu, Z. C., Zong, K. Q., Gao, C. G., Gao, S., Xu, J., and Chen,
H. H.: Reappraisement and refinement of zircon U–Pb isotope and trace
element analyses by LA–ICP–MS, Chinese Sci. Bull., 55, 1535–1546,
https://doi.org/10.1007/s11434-010-3052-4, 2010.
Ludwig, K. R.: User's manual for Isoplot 3.00: A geochronological toolkit
for Microsoft excel, special publication 4, Berkeley Geochronology Center,
2003.
Ma, X. Y. and Wu, Z. W.: Early tectonic evolution of China, Precambrian
Res., 14, 185–202, https://doi.org/10.1016/0301-9268(81)90038-3, 1981.
Meng, E., Xu, W. L., Pei, F. P., Yang, D. B., Yu, Y., and Zhang, X. Z.:
Detrital-zircon geochronology of Late Paleozoic sedimentary rocks in eastern
Heilongjiang Province, NE China: implications for the tectonic evolution of
the eastern segment of the Central Asian Orogenic Belt, Tectonophysics, 485,
42–51, https://doi.org/10.1016/j.tecto.2009.11.015, 2010.
Meng, Q. R.: What drove late Mesozoic extension of the northern
China–Mongolia tract?, Tectonophysics, 369, 155–174,
https://doi.org/10.1016/S0040-1951(03)00195-1, 2003.
Meng, Q. R.: Development of sedimentary basins in eastern China during the
Yanshanian Period, Bull. Mineral. Petrol. Geochem., 36, 567–569, 2017 (in
Chinese).
Meng, Q. R., Wei, H. H., Qu, Y. Q., and Ma, S. X.: Stratigraphic and
sedimentary records of the rift to drift evolution of the northern North
China Craton at the Paleo–to Mesoproterozoic transition, Gondwana Res., 20,
205–218, https://doi.org/10.1016/j.gr.2010.12.010, 2011.
Meng, Q. R., Wei, H. H., Wu, G. L., and Duan, L.: Early Mesozoic tectonic
settings of the northern North China Craton, Tectonophysics, 611, 155–166,
https://doi.org/10.1016/j.tecto.2013.11.015, 2014.
Meng, Q. R., Wu, G. L., Fan, L. G., and Wei, H. H.: Early Mesozoic evolution
of sedimentary basins and tectonic settings of the North China Craton, Sci.
China (Earth Sci.), in review, 2018.
Pei, F. P., Xu, W. L., Yu, Y., Zhao, Q. G., and Yang, D. B.: Petrogenesis of
the Late Triassic Mayihe Pluton in southern Jilin Province: evidence from
zircon U–Pb geochronology and geochemistry, J. Jilin Univ. (Earth Sci.
Edition), 38, 351–362, 2008 (in Chinese).
Pei, F. P., Xu, W. L., Yang, D. B., Yu, Y., Meng, E., and Zhao, Q. G.:
Petrogenesis of late Mesozoic granitoids in southern Jilin Province,
northeastern China: geochronological, geochemical, and Sr–Nd–Pb isotopic
evidence, Lithos, 125, 27–39, https://doi.org/10.1016/j.lithos.2011.01.004, 2011.
Pei, F. P., Wang, Z. W., Cao, H. H., Xu, W. L., and Wang, F.: Petrogenesis
of the Early Paleozoictonalite in the central Jilin Province: evidence from
zircon U–Pb chronology and geochemistry, Acta Petrol. Sin., 30, 2009–2019,
2014 (in Chinese).
Pei, F. P., Zhang, Y., Wang, Z. W., Cao, H. H., Xu, W. L., Wang, Z. J.,
Wang, F., and Yang, C.: Early–Middle Paleozoic subduction-collision history
of the south-eastern central Asian orogenic belt: evidence from igneous and
metasedimentary rocks of central Jilin Province, NE China, Lithos, 261,
164–180, https://doi.org/10.1016/j.lithos.2015.12.010, 2016.
Safonova, I. Y. and Santosh, M.: Accretionary complexes in the Asia-Pacific
region: tracing archives of ocean plate stratigraphy and tracking mantle
plumes, Gondwana Res., 25, 126–158,
https://doi.org/10.1016/j.gr.2012.10.008, 2014.
Sengör, A. M. C. and Natal'in, B. A.: Paleotectonics of Asia: Fragments
of a synthesis, in: The Tectonic Evolution of Asia, Cambridge University
Press, London, 486–640, 1996.
Shanxi Bureau of Geology and Mineral Resources (SBGMR): Regional Geology of
Shanxi Province, Geological Publishing House, Beijing, 1989 (in Chinese).
Shen, S. Z., Zhang, H., Shang, Q. H., and Li, W. Z.: Permian stratigraphy
and correlation of northeast China: a review, J. Asian Earth Sci., 26,
304–326, https://doi.org/10.1016/j.jseaes.2005.07.007, 2006.
Shi, G. R.: The marine Permian of east and northeast Asia: an overview of
biostratigraphy, palaeobiogeography and palaeogeographical implications, J.
Asian Earth Sci., 26, 175–206,
https://doi.org/10.1016/j.jseaes.2005.11.004, 2006.
Si, X. J. and Zhou, Z. Y. (Eds.): Mesozoic continental strata in China,
Science Press, Beijing, 1962 (in Chinese).
Sun, D. Y., Wu, F. Y., Zhang, Y. B., and Gao, S.: The final closing time of
Xiramuron–Changchun–Yanji plate suture zone: evidence from the Dayushan
granitic pluton of Jilin, J. Jilin Univ. (Earth Sci. Edition), 34, 174–181,
2004 (in Chinese).
Sun, M. D., Xu, Y. G., Wilde, S. A., Chen, H. L., and Yang, S. F.: The
Permian Dongfanghong island-arc gabbro of the Wandashan Orogen, NE China:
implications for Paleo-Pacific subduction, Tectonophysics, 659, 122–136,
https://doi.org/10.1016/j.tecto.2015.07.034, 2015.
Tang, J., Xu, W. L., Wang, F., Wang, W., Xu, M. J., and Zhang, Y. H.:
Geochronology and geochemistry of Neoproterozoic magmatism in the Erguna
Massif, NE China: Petrogenesis and implications for the breakup of the
Rodinia supercontinent, Precambrian Res., 224, 597–611,
https://doi.org/10.1016/j.precamres.2012.10.019, 2013.
Tang, J., Xu, W. L., Wang, F., and Ge, W. C.: Subduction history of the
Paleo-Pacific slab beneath Eurasian continent: Mesozoic–Paleogene magmatic
records in northeast Asia, Sci. China (Earth Sci.), 61, 527–559,
https://doi.org/10.1007/s11430-017-9174-1, 2018.
Tang, J., Xu., W. L., and Wang, F.: Rock associations and their
spatial-temporal variations of the early Mesozoic igneous rocks in the NE
Asia: constraints on the initial subduction timing of the Paleo-Pacific
Plate, Bull. Mineral. Petrol. Geochem., 35, 1181–1194,
https://doi.org/10.3969/j.issn.l007-2802.2016.06.009, 2016 (in Chinese).
Wang, F., Xu, W. L., Meng, E., Cao, H. H., and Gao, F. H.: Early Paleozoic
amalgamation of the Songnen–Zhangguangcai Range and Jiamusi Massifs in the
eastern segment of the central Asian orogenic belt: geochronological and
geochemical evidence from granitoids and rhyolites, J. Asian Earth Sci., 49,
234–248, https://doi.org/10.1016/j.jseaes.2011.09.022, 2012.
Wang, F., Xu, W. L., Gao, F. H., Zhang, H. H., Pei, F. P., Zhao, L., and
Yang, Y.: Precambrian terrane within the Songnen–Zhangguangcai Range
Massif, NE China: evidence from U–Pb ages of detrital zircons from the
Dongfengshan and Tadong groups, Gondwana Res., 26, 402–413,
https://doi.org/10.1016/j.gr.2013.06.017, 2014.
Wang, F., Xu, W. L., Xu, Y. G., Gao, F. H., and Ge, W. C.: Late Triassic
bimodal igneous rocks in eastern Heilongjiang Province, NE China:
implications for the initiation of subduction of the Paleo-Pacific Plate
beneath Eurasia, J. Asian Earth Sci., 97, 406–423.
https://doi.org/10.1016/j.jseaes.2014.05.025, 2015.
Wang, F., Xu, Y. G., Xu, W. L., Yang, L., and Wu, W.: Early Jurassic
calc-alkaline magmatism in northeast China: Magmatic response to subduction
of the Paleo-Pacific Plate beneath the Eurasian continent, J. Asian Earth
Sci., 143, 249–268, https://doi.org/10.1016/j.jseaes.2017.04.018, 2017.
Wang, Z. J., Xu, W. L., Pei, F. P., Wang, Z. W., Li, Y., and Cao, H. H.:
Geochronology and geochemistry of Middle Permian–Middle Triassic intrusive
rocks from central–eastern Jilin Province, NE China: constraints on the
tectonic evolution of the eastern segment of the Paleo-Asian
ocean, Lithos, 238, 13–25, https://doi.org/10.1016/ j.lithos.2015.09.019,
2015.
Wang, Z. W., Pei, F. P., Xu, W. L., Cao, H. H., Wang, Z. J., and Zhang, Y.:
Tectonic evolution of the eastern central Asian orogenic belt: evidence from
zircon U–Pb–Hf isotopes and geochemistry of early Paleozoic rocks in
Yanbian region, NE China, Gondwana Res., 38, 334–350,
https://doi.org/10.1016/j.gr.2016.01.004, 2016.
Wilde, S. A. and Zhou, J. B.: The late Paleozoic to Mesozoic evolution of
the eastern margin of the central Asian orogenic belt in China, J. Asian
Earth Sci., 113, 909–921, https://doi.org/10.1016/j.jseaes.2015.05.005,
2015.
Wu, F. Y., Jahn, B. M., Wilde, S., and Sun, D. Y.: Phanerozoic continental
crustal growth: Sr–Nd isotopic evidence from the granitesin northeastern
China, Tectonophysics, 328, 87–113, 2000.
Wu, F. Y., Sun, D. Y., Jahn, B. M., and Wilde, S.: A Jurassic garnet-bearing
granitic pluton from NE China showing tetrad REE patterns, J. Asian Earth
Sci., 23, 731–744, https://doi.org/10.1016/S1367-9120(03)00149-4, 2004.
Wu, F. Y., Sun, D. Y., Li, H., Jahn, B. M., and Wilde, S.: A-type granites
in northeastern China: age and geochemical constraints on their
petrogenesis, Chem. Geol., 187, 143–173,
https://doi.org/10.1016/S0009-2541(02)00018-9, 2002.
Wu, F. Y., Yang, J. H., Lo, C. H., Wilde, S. A., Sun, D. Y., and Jahn, B.
M.: The Heilongjiang group: a Jurassic accretionary complex in the Jiamusi
Massif at the western pacific margin of northeastern China, Isl. Arc, 16,
156–172, https://doi.org/10.1111/j.1440-1738.2007.00564.x, 2007a.
Wu, F. Y., Zhao, G. C., Sun, D. Y., Wilde, S. A., and Yang, J. H.: The Hulan
Group: its role in the evolution of the Central Asian Orogenic Belt of NE
China, J. Asian Earth Sci., 30, 542–556,
https://doi.org/10.1016/j.jseaes.2007.01.003, 2007b.
Wu, F. Y., Sun, D. Y., Ge, W. C., Zhang, Y. B., Grant, M. L., Wilde, S. A.,
and Jahn, B. M.: Geochronology of the Phanerozoic granitoids in northeastern
China, J. Asian Earth Sci., 41, 1–30,
https://doi.org/10.1016/j.jseaes.2010.11.014, 2011.
Xu, B., Zhao, P., Bao, Q. Z., Zhou, Y. H., Wang, Y. Y., and Luo, Z. W.:
Preliminary study on the pre-Mesozoic tectonic unit division of the
Xing–Meng Orogenic Belt (XMOB), Acta Petrol. Sin., 30, 1841–1857, 2014 (in
Chinese).
Xu, B., Zhao, P., Wang, Y. Y., Liao, W., Luo, Z. W., Bao, Q. Z., and Zhou,
Y. H.: The pre–Devonian tectonic framework of Xing'an–Mongolia Orogenic
Belt (XMOB) in North China, J. Asian Earth Sci., 97, 183–196,
https://doi.org/10.1016/j.jseaes.2014.07.020, 2015.
Xu, H., Liu, Y. Q., Kuang, H. W, and Peng, N.: Sedimentary response to the
intracontinental orogenic process: insight from the anatomy of a small
Mesozoic basin in western Yanshan, northern North China, Int. Geol. Rev.,
58, 1528–1556, https://doi.org/10.1080/00206814.2016.1168323, 2016.
Xu, W. L., Ji, W. Q., Pei, F. P., Meng, E., Yu, Y., Yang, D. B., and Zhang,
X. Z.: Triassic volcanism in eastern Heilongjiang and Jilin provinces, NE
China: chronology, geochemistry, and tectonic implications, J. Asian Earth
Sci., 34, 392–402, https://doi.org/10.1016/j.jseaes.2008.07.001, 2009.
Xu, W. L., Wang, F., Meng, E., Gao, F. H., Pei, F. P., and Yu, J. J.:
Paleozoic–early Mesozoic tectonic evolution in the eastern Heilongjiang
Province, NE China: evidence from igneous rock association and U–Pb
geochronology of detrital zircons, J. Jilin Univ. (Earth Sci. Edition), 42,
1378–1389, https://doi.org/10.13278/j.cnki.jjuese.2012.05.024, 2012 (in
Chinese).
Xu, W. L., Pei, F. P., Wang, F., Meng, E., Ji, W. Q., Yang, D. B., and Wang,
W.: Spatial-temporal relationships of Mesozoic volcanic rocks in NE China:
constraints on tectonic overprinting and transformations between multiple
tectonic systems, J. Asian Earth Sci., 74, 167–193,
https://doi.org/10.1016/j.jseaes.2013.04.003, 2013.
Yang, D. B., Yang, H. T., Shi, J. P., Xu, W. L., and Wang, F.: Sedimentary
response to the paleogeographic and tectonic evolution of the southern North
China Craton during the late Paleozoic and Mesozoic, Gondwana Res., 49,
https://doi.org/10.1016/j.gr.2017.06.009, 2017.
Yang, H., Ge, W. C., Zhao, G. C., Dong, Y., Xu, W. L., Ji, Z., and Yu, J.
J.: Late Triassic intrusive complex in the Jidong region, Jiamusi–Khanka
Block, NE China: geochemistry, zircon U–Pb ages, Lu–Hf isotopes, and
implications for magma mingling and mixing, Lithos, 224–225, 143–159,
https://doi.org/10.1016/j.lithos.2015.03.001, 2015a.
Yang, H., Ge, W. C., Zhao, G. C., Yu, J. J., and Zhang, Y. L.: Early
Permian–Late Triassic granitic magmatism in the Jiamusi–Khanka Massif,
eastern segment of the Central Asian Orogenic Belt and its implications,
Gondwana Res., 27, 1509–1533, https://doi.org/10.1016/j.gr.2014.01.011,
2015b.
Yang, H., Ge, W. C., Yu, Q., Ji, Z., Liu, X. W., Zhang, Y. L., and Tian, D. X.:
Zircon U–Pb–Hf isotopes, bulk-rock geochemistry and petrogenesis of Middle
to Late Triassic I-type granitoids in the Xing'an Block, northeast China:
implications for early Mesozoic tectonic evolution of the central great
Xing'an range, J. Asian Earth Sci., 119, 30–48,
https://doi.org/10.1016/j.jseaes.2016.01.012, 2016.
Yang, J. H., Wu, F. Y., Shao, J. A., Wilde, S. A., Xie, L. W., and Liu, X.
M.: Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt,
north China, Earth Planet. Sc. Lett., 246, 336–352,
https://doi.org/10.1016/j.epsl.2006.04.029, 2006.
Yang, J. H., Wu, F. Y., Wilde, S. A., and Liu, X. M.: Petrogenesis of Late
Triassic granitoids and their enclaves with implications for
post-collisional lithospheric thinning of the Liaodong peninsula, North
China Craton, Chem. Geol., 242, 155–175,
https://doi.org/10.1016/j.chemgeo.2007.03.007, 2007.
Yu, J. J., Wang, F., Xu, W. L., Gao, F. H., and Pei, F. P.: Early Jurassic
mafic magmatism in the lesser Xing'an–Zhangguangcai Range, NE China, and
its tectonic implications: constraints from zircon U–Pb chronology and
geochemistry, Lithos, 142–143, 256–266,
https://doi.org/10.1016/j.lithos.2012.03.016, 2012.
Yu, Y., Xu, W. L., Pei, F. P., Yang, D. B., and Zhao, Q. G.: Chronology and
geochemistry of Mesozoic volcanic rocks in the Linjiang area, Jilin Province
and their tectonic implications, Acta Geol. Sin. (English Edition), 83,
245–257, https://doi.org/10.1111/j.1755-6724.2009.00039.x, 2009.
Yuan, H. L., Gao, S., Liu, X. M., Li, H. M., Günther, D., and Wu, F. Y.:
Accurate U–Pb age and trace element determinations of zircon by laser
ablation inductively coupled plasmamass spectrometry, Geostandard Newslett., 28,
353–370, 2004.
Zhang, S. H., Zhao, Y., Kröner, A., Liu, X. M., Xie, L. W., and Chen, F.
K.: Early Permian plutons from the northern North China block: constraints
on continental arc evolution and convergent margin magmatism related to the
Central Asian Orogenic Belt, Int. J. Earth Sci., 98, 1441–1467,
https://doi.org/10.1007/s00531-008-0368-2, 2009.
Zhang, S. H., Zhao, Y., Liu, J. M., Hu, J. M., Song, B., Liu, J., and Wu,
H.: Geochronology, geochemistry and tectonic setting of the late
Paleozoic–early Mesozoic magmatism in the northern margin of the North
China Block: A preliminary review, Acta Petrol. Mineral., 29, 824–842,
https://doi.org/10.3969/j.issn.1000-6524.2010.06.017, 2010 (in Chinese).
Zhang, S. H., Zhao, Y., Davis, G. A., Ye, H., and Wu, F.: Temporal and
spatial variations of Mesozoic magmatism and deformation in the North China
Craton: implications for lithospheric thinning and decratonization, Earth
Sci. Rev., 131, 49–87, https://doi.org/10.1016/j.earscirev.2013.12.004,
2014.
Zhang, Y. B., Wu, F. Y., Wilde, S. A., Zhai, M. G., Lu, X. P., and Sun, D.
Y.: Zircon U–Pb ages and tectonic implications of “early Paleozoic”
granitoids at Yanbian, Jilin province, NE China, Isl. Arc, 13, 484–505,
https://doi.org/10.1111/j.1440-1738.2004.00442.x, 2004.
Zhao, G. C, Wilde, S. A., Cawood, P. A., and Sun, M.: Archean blocks and
their boundaries in the North China Craton: lithological, geochemical,
structural and P–T, path constraints and tectonic evolution, Precambrian
Res., 107, 45–73, https://doi.org/10.1016/S0301-9268(00)00154-6, 2001.
Zhao, L. L. and Zhang, X. Z.: Petrological and geochronological evidences
of tectonic exhumation of Heilongjiang complex in the eastern part of
Heilongjiang Province, China, Acta Petrol. Sin., 27, 1227–1234, 2011 (in
Chinese).
Zhao, P., Jahn, B. M., and Xu, B.: Elemental and Sr–Nd isotopic
geochemistry of Cretaceous to early Paleogene granites and volcanic rocks in
the Sikhote–Alin Orogenic Belt (Russian Far East) and their implication on
regional tectonic evolution, J. Asian Earth Sci., 146, 383–401,
https://doi.org/10.1016/j.jseaes.2017.06.017, 2017.
Zheng, Y. F., Fu, B., Gong, B., and Li, L.: Stable isotope geochemistry of
ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China:
implications for geodynamics and fluid regime, Earth Sci. Rev., 62,
105–161, 2003.
Zheng, Y. F., Xiao, W. J., and Zhao, G. C.: Introduction to tectonics of
China, Gondwana Res., 23, 1189–1206,
https://doi.org/10.1016/j.gr.2012.10.001, 2013.
Zhou, J. B. and Li, L.: The Mesozoic accretionary complex in northeast
China: evidence for the accretion history of Paleo-Pacific subduction, J.
Asian Earth Sci., 145, 91–100,
https://doi.org/10.1016/j.jseaes.2017.04.013, 2017.
Zhou, J. B., Wilde, S. A., Zhang, X. Z., Zhao, G. C., Zheng, C. Q., Wang, Y.
J., and Zhang, X. H.: The onset of Pacific margin accretion in NE China:
evidence from the Heilongjiang high-pressure metamorphic belt,
Tectonophysics, 478, 230–246, https://doi.org/10.1016/j.tecto.2009.08.009,
2009.
Zhou, J. B., Wilde, S. A., Zhao, G. C., Zhang, X. Z., Zheng, C. Q., and
Wang, H.: New Shrimp U–Pb zircon ages from the Heilongjiang High-Pressure
Belt: constraints on the Mesozoic evolution of NE China, Am. J. Sci., 310,
1024–1053, https://doi.org/10.2475/09.2010.10, 2010.
Zhou, J. B., Cao, J. L., Wilde, S. A., Zhao, G. C., Zhang, J. J., and Wang,
B.: Paleo-Pacific subduction-accretion: evidence from geochemical and U–Pb
zircon dating of the Nadanhada accretionary complex, NE China, Tectonics,
33, 2444–2466, https://doi.org/10.1002/2014TC003637, 2015.
Zhu, G. X.: The discovery of the assemblage of bivalve fossils in the Late
Triassic fresh water in the Xiaoyingzi Formation, Fusong, Jilin province,
Jilin Geology, 1, 13–21, 1991 (in Chinese).
Short summary
Early Triassic sediments in the northeastern North Chian Craton resulted from the subduction of the Paleo-Asian oceanic plate and collision between the North China and Yangtze cratons. Late Triassic sediments resulted from the final closure of the Paleo-Asian Ocean in the Middle Triassic and exhumation of the Su–Lu Orogenic Belt. Early Jurassic change in provenance was related to the uplift of the Xing'an–Mongolia Orogenic Belt and the subduction of the Paleo-Pacific Plate.
Early Triassic sediments in the northeastern North Chian Craton resulted from the subduction of...
