Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2463-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-11-2463-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Dec 2020
Research article |
| 14 Dec 2020
| 14 Dec 2020
Birth and closure of the Kallipetra Basin: Late Cretaceous reworking of the Jurassic Pelagonian–Axios/Vardar contact (northern Greece)
Lydia R. Bailey
CORRESPONDING AUTHOR
Department of Geosciences, University of Arizona, Tucson, AZ 85721,
USA
Department of Earth Sciences, Institute of Geology, ETH Zurich, 8092
Zurich, Switzerland
Filippo L. Schenker
Institute of Earth Sciences, University of Applied Sciences and Arts
of Southern Switzerland, 6952 Canobbio, Switzerland
Maria Giuditta Fellin
Department of Earth Sciences, Institute of Geology, ETH Zurich, 8092
Zurich, Switzerland
Miriam Cobianchi
Department of Earth and Environmental Sciences, University of Pavia,
Pavia, 27100, Italy
Thierry Adatte
Institute of Earth Sciences, University of Lausanne, 1015 Lausanne,
Switzerland
Vincenzo Picotti
Department of Earth Sciences, Institute of Geology, ETH Zurich, 8092
Zurich, Switzerland
Related authors
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Nikhil Sharma, Jorge E. Spangenberg, Thierry Adatte, Torsten Vennemann, László Kocsis, Jean Vérité, Luis Valero, and Sébastien Castelltort
Clim. Past, 20, 935–949, https://doi.org/10.5194/cp-20-935-2024, https://doi.org/10.5194/cp-20-935-2024, 2024
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The Middle Eocene Climatic Optimum (MECO) is an enigmatic global warming event with scarce terrestrial records. To contribute, this study presents a new comprehensive geochemical record of the MECO in the fluvial Escanilla Formation, Spain. In addition to identifying the regional preservation of the MECO, results demonstrate continental sedimentary successions, as key archives of past climate and stable isotopes, to be a powerful tool in correlating difficult-to-date fluvial successions.
Cécile Charles, Nora Khelidj, Lucia Mottet, Bao Ngan Tu, Thierry Adatte, Brahimsamba Bomou, Micaela Faria, Laetitia Monbaron, Olivier Reubi, Natasha de Vere, Stéphanie Grand, and Gianalberto Losapio
EGUsphere, https://doi.org/10.5194/egusphere-2024-991, https://doi.org/10.5194/egusphere-2024-991, 2024
Preprint archived
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We found that novel ecosystems created by glacier retreat are first characterized by an increase in plant diversity that is driven by a shift in soil texture. Plant diversity in turn increases soil organic matter and nutrient. Soils gradually acidifies and leads to a final stage where a dominance of few plant species reduces plant diversity. Understanding plant–soil interactions is crucial to anticipate how glacier retreat shapes biodiversity and landscapes.
Morgan T. Jones, Ella W. Stokke, Alan D. Rooney, Joost Frieling, Philip A. E. Pogge von Strandmann, David J. Wilson, Henrik H. Svensen, Sverre Planke, Thierry Adatte, Nicolas Thibault, Madeleine L. Vickers, Tamsin A. Mather, Christian Tegner, Valentin Zuchuat, and Bo P. Schultz
Clim. Past, 19, 1623–1652, https://doi.org/10.5194/cp-19-1623-2023, https://doi.org/10.5194/cp-19-1623-2023, 2023
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There are periods in Earth’s history when huge volumes of magma are erupted at the Earth’s surface. The gases released from volcanic eruptions and from sediments heated by the magma are believed to have caused severe climate changes in the geological past. We use a variety of volcanic and climatic tracers to assess how the North Atlantic Igneous Province (56–54 Ma) affected the oceans and atmosphere during a period of extreme global warming.
Sabí Peris Cabré, Luis Valero, Jorge E. Spangenberg, Andreu Vinyoles, Jean Verité, Thierry Adatte, Maxime Tremblin, Stephen Watkins, Nikhil Sharma, Miguel Garcés, Cai Puigdefàbregas, and Sébastien Castelltort
Clim. Past, 19, 533–554, https://doi.org/10.5194/cp-19-533-2023, https://doi.org/10.5194/cp-19-533-2023, 2023
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The Middle Eocene Climatic Optimum (MECO) was a global warming event that took place 40 Myr ago and lasted ca. 500 kyr, inducing physical, chemical, and biotic changes on the Earth. We use stable isotopes to identify the MECO in the Eocene deltaic deposits of the Southern Pyrenees. Our findings reveal enhanced deltaic progradation during the MECO, pointing to the important impact of global warming on fluvial sediment transport with implications for the consequences of current climate change.
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, and Anneleen Foubert
Clim. Past, 18, 1915–1945, https://doi.org/10.5194/cp-18-1915-2022, https://doi.org/10.5194/cp-18-1915-2022, 2022
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The investigation of a 9 m long sediment core recovered at ca. 300 m water depth demonstrates that cold-water coral mound build-up within the East Melilla Coral Province (southeastern Alboran Sea) took place during both interglacial and glacial periods. Based on the combination of different analytical methods (e.g. radiometric dating, micropaleontology), we propose that corals never thrived but rather developed under stressful environmental conditions.
Erica D. Erlanger, Maria Giuditta Fellin, and Sean D. Willett
Solid Earth, 13, 347–365, https://doi.org/10.5194/se-13-347-2022, https://doi.org/10.5194/se-13-347-2022, 2022
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We present an erosion rate analysis on dated rock and sediment from the Northern Apennine Mountains, Italy, which provides new insights on the pattern of erosion rates through space and time. This analysis shows decreasing erosion through time on the Ligurian side but increasing erosion through time on the Adriatic side. We suggest that the pattern of erosion rates is consistent with the present asymmetric topography in the Northern Apennines, which has likely existed for several million years.
Moussa Moustapha, Loris Deirmendjian, David Sebag, Jean-Jacques Braun, Stéphane Audry, Henriette Ateba Bessa, Thierry Adatte, Carole Causserand, Ibrahima Adamou, Benjamin Ngounou Ngatcha, and Frédéric Guérin
Biogeosciences, 19, 137–163, https://doi.org/10.5194/bg-19-137-2022, https://doi.org/10.5194/bg-19-137-2022, 2022
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We monitor the spatio-temporal variability of organic and inorganic carbon (C) species in the tropical Nyong River (Cameroon), across groundwater and increasing stream orders. We show the significant contribution of wetland as a C source for tropical rivers. Thus, ignoring the river–wetland connectivity might lead to the misrepresentation of C dynamics in tropical watersheds. Finally, total fluvial carbon losses might offset ~10 % of the net C sink estimated for the whole Nyong watershed.
Elena T. Bruni, Richard F. Ott, Vincenzo Picotti, Negar Haghipour, Karl W. Wegmann, and Sean F. Gallen
Earth Surf. Dynam., 9, 771–793, https://doi.org/10.5194/esurf-9-771-2021, https://doi.org/10.5194/esurf-9-771-2021, 2021
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The Klados River catchment contains seemingly overlarge, well-preserved alluvial terraces and fans. Unlike previous studies, we argue that the deposits formed in the Holocene based on their position relative to a paleoshoreline uplifted in 365 CE and seven radiocarbon dates. We also find that constant sediment supply from high-lying landslide deposits disconnected the valley from regional tectonics and climate controls, which resulted in fan and terrace formation guided by stochastic events.
Vincent F. Verwater, Eline Le Breton, Mark R. Handy, Vincenzo Picotti, Azam Jozi Najafabadi, and Christian Haberland
Solid Earth, 12, 1309–1334, https://doi.org/10.5194/se-12-1309-2021, https://doi.org/10.5194/se-12-1309-2021, 2021
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Balancing along geological cross sections reveals that the Giudicarie Belt comprises two kinematic domains. The SW domain accommodated at least ~ 18 km Late Oligocene to Early Miocene shortening. Since the Middle Miocene, the SW domain experienced at least ~ 12–22 km shortening, whereas the NE domain underwent at least ~ 25–35 km. Together, these domains contributed to ~ 40–47 km of sinistral offset of the Periadriatic Fault along the Northern Giudicarie Fault since the Late Oligocene.
Louis Honegger, Thierry Adatte, Jorge E. Spangenberg, Miquel Poyatos-Moré, Alexandre Ortiz, Magdalena Curry, Damien Huyghe, Cai Puigdefàbregas, Miguel Garcés, Andreu Vinyoles, Luis Valero, Charlotte Läuchli, Andrés Nowak, Andrea Fildani, Julian D. Clark, and Sébastien Castelltort
Solid Earth Discuss., https://doi.org/10.5194/se-2021-12, https://doi.org/10.5194/se-2021-12, 2021
Publication in SE not foreseen
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, Thomas Krengel, and Anneleen Foubert
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-82, https://doi.org/10.5194/cp-2020-82, 2020
Manuscript not accepted for further review
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This study describes the development of a cold-water Coral mound in the southeast alboran sea over the last 300 ky. Mound development follows interglacial-glacial cycles.
Louis Honegger, Thierry Adatte, Jorge E. Spangenberg, Jeremy K. Caves Rugenstein, Miquel Poyatos-Moré, Cai Puigdefàbregas, Emmanuelle Chanvry, Julian Clark, Andrea Fildani, Eric Verrechia, Kalin Kouzmanov, Matthieu Harlaux, and Sébastien Castelltort
Clim. Past, 16, 227–243, https://doi.org/10.5194/cp-16-227-2020, https://doi.org/10.5194/cp-16-227-2020, 2020
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A geochemical study of a continental section reveals a rapid global warming event (hyperthermal U), occurring ca. 50 Myr ago, only described until now in marine sediment cores. Documenting how the Earth system responded to rapid climatic shifts provides fundamental information to constrain climatic models. Our results suggest that continental deposits can be high-resolution recorders of these warmings. They also give an insight on the climatic conditions occurring during at the time.
F. L. Schenker, M. G. Fellin, and J.-P. Burg
Solid Earth, 6, 285–302, https://doi.org/10.5194/se-6-285-2015, https://doi.org/10.5194/se-6-285-2015, 2015
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The eastern Mediterranean is a long-lived seismically active region where the interaction of compressive and extensive tectonics is responsible for complex crustal deformation. The Pelagonian zone in the Hellenides has witnessed such deformational processes since the Mesozoic. This study combines fission-track analysis (recording temperatures <240°C), structural and stratigraphic data that were essential to constrain the polyphase evolution of the Hellenic orogen over 100 Ma.
Related subject area
Subject area: The evolving Earth surface | Editorial team: Stratigraphy, sedimentology, geomorphology, morphotectonics, and palaeontology | Discipline: Sedimentology
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Tectonic processes, variations in sediment flux, and eustatic sea level recorded by the 20 Myr old Burdigalian transgression in the Swiss Molasse basin
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Melchior Schuh-Senlis, Guillaume Caumon, and Paul Cupillard
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This paper presents the application of a numerical method for restoring models of the subsurface to a previous state in their deformation history, acting as a numerical time machine for geological structures. The method is applied to a model based on a laboratory experiment. The results show that using force conditions in the computation of the deformation allows us to assess the value of some previously unknown physical parameters of the different materials inside the model.
Onyedika Anthony Igbokwe, Jithender J. Timothy, Ashwani Kumar, Xiao Yan, Mathias Mueller, Alessandro Verdecchia, Günther Meschke, and Adrian Immenhauser
Solid Earth, 15, 763–787, https://doi.org/10.5194/se-15-763-2024, https://doi.org/10.5194/se-15-763-2024, 2024
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We present a workflow that models the impact of stress regime change on the permeability of fractured Latemar carbonate buildup using a displacement-based linear elastic finite-element method (FEM) and outcrop data. Stress-dependent heterogeneous apertures and effective permeability were calculated and constrained by the study area's stress directions. Simulated far-field stresses at NW–SE subsidence deformation and N–S Alpine deformation increased the overall fracture aperture and permeability.
Yan Cao, Zhijun Jin, Rukai Zhu, and Kouqi Liu
Solid Earth, 14, 1169–1179, https://doi.org/10.5194/se-14-1169-2023, https://doi.org/10.5194/se-14-1169-2023, 2023
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Fourier transform infrared (FTIR) was performed on shale before and after solvent extraction. The extraction yield from shale with THF is higher than other solvents. The organic-C-normalized yield of a mature sample is higher than other samples. The aromaticity of organic matter increases, and the length of organic matter aliphatic chains does not vary monotonically with increasing maturity. The results will help in the selection of organic solvents for oil-washing experiments of shale.
Zbyszek Remin, Michał Cyglicki, and Mariusz Niechwedowicz
Solid Earth, 13, 681–703, https://doi.org/10.5194/se-13-681-2022, https://doi.org/10.5194/se-13-681-2022, 2022
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Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted as the deepest and most subsiding part of the basin during the Cretaceous times. We interpret this area conversely, as representing a landmass – the Łysogóry–Dobrogea Land. Inversion-related tectonics, uplift on the one hand and enhanced subsidence on the other, drove the development of the Szozdy Delta within the axial part of the basin. New heavy mineral data suggest different burial histories.
Emilija Krsnik, Katharina Methner, Marion Campani, Svetlana Botsyun, Sebastian G. Mutz, Todd A. Ehlers, Oliver Kempf, Jens Fiebig, Fritz Schlunegger, and Andreas Mulch
Solid Earth, 12, 2615–2631, https://doi.org/10.5194/se-12-2615-2021, https://doi.org/10.5194/se-12-2615-2021, 2021
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Here we present new surface elevation constraints for the middle Miocene Central Alps based on stable and clumped isotope geochemical analyses. Our reconstructed paleoelevation estimate is supported by isotope-enabled paleoclimate simulations and indicates that the Miocene Central Alps were characterized by a heterogeneous and spatially transient topography with high elevations locally exceeding 4000 m.
Jean-Philippe Blouet, Patrice Imbert, Sutieng Ho, Andreas Wetzel, and Anneleen Foubert
Solid Earth, 12, 2439–2466, https://doi.org/10.5194/se-12-2439-2021, https://doi.org/10.5194/se-12-2439-2021, 2021
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Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine sediments. Seep carbonates may act as seals and force lateral deviations of rising hydrocarbons. However, crustacean burrows may act as efficient vertical fluid channels allowing hydrocarbons to pass through upward, thereby allowing the vertical growth of carbonate stacks over time. This mechanism may explain the origin of carbonate columns in marine sediments throughout hydrocarbon provinces worldwide.
Thomas Voigt, Jonas Kley, and Silke Voigt
Solid Earth, 12, 1443–1471, https://doi.org/10.5194/se-12-1443-2021, https://doi.org/10.5194/se-12-1443-2021, 2021
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Basin inversion in central Europe is believed to have started during Late Cretaceous (middle Turonian) and probably proceeded until the Paleogene. Data from different marginal troughs in central Europe point to an earlier start of basin inversion (in the Cenomanian). The end of inversion is overprinted by general uplift but had probably already occurred in the late Campanian to Maastrichtian. Both the start and end of inversion occurred with low rates of uplift and subsidence.
Arne Jacob, Markus Peltz, Sina Hale, Frieder Enzmann, Olga Moravcova, Laurence N. Warr, Georg Grathoff, Philipp Blum, and Michael Kersten
Solid Earth, 12, 1–14, https://doi.org/10.5194/se-12-1-2021, https://doi.org/10.5194/se-12-1-2021, 2021
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In this work, we combined different imaging and experimental measuring methods for analysis of cross-scale effects which reduce permeability of tight reservoir rocks. Simulated permeability of digital images of rocks is often overestimated, which is caused by non-resolvable clay content within the pores of a rock. By combining FIB-SEM with micro-XCT imaging, we were able to simulate the true clay mineral abundance to match experimentally measured permeability with simulated permeability.
Georg Schwamborn, Kai Hartmann, Bernd Wünnemann, Wolfgang Rösler, Annette Wefer-Roehl, Jörg Pross, Marlen Schlöffel, Franziska Kobe, Pavel E. Tarasov, Melissa A. Berke, and Bernhard Diekmann
Solid Earth, 11, 1375–1398, https://doi.org/10.5194/se-11-1375-2020, https://doi.org/10.5194/se-11-1375-2020, 2020
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We use a sediment core from the Gobi Desert (Ejina Basin, NW China) to illustrate the landscape history of the area. During 2.5 million years a sediment package of 223 m thickness has been accumulated. Various sediment types document that the area turned from a playa environment (shallow water environment with multiple flooding events) to an alluvial–fluvial environment after the arrival of the Heihe in the area. The river has been diverted due to tectonics.
Philippos Garefalakis and Fritz Schlunegger
Solid Earth, 10, 2045–2072, https://doi.org/10.5194/se-10-2045-2019, https://doi.org/10.5194/se-10-2045-2019, 2019
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The controls on the 20 Myr old Burdigalian transgression in the Swiss Molasse basin have been related to a reduction in sediment flux, a rise in global sea level, or tectonic processes in the adjacent Alps. Here, we readdress this problem and extract stratigraphic signals from the Upper Marine Molasse deposits in Switzerland. In conclusion, we consider rollback tectonics to be the main driving force controlling the transgression, which is related to a deepening and widening of the basin.
Laura Stutenbecker, Peter M. E. Tollan, Andrea Madella, and Pierre Lanari
Solid Earth, 10, 1581–1595, https://doi.org/10.5194/se-10-1581-2019, https://doi.org/10.5194/se-10-1581-2019, 2019
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The Aar and Mont Blanc regions in the Alps are large granitoid massifs characterized by high topography. We analyse when these granitoids were first exhumed to the surface. We test this by tracking specific garnet grains, which are exclusively found in the granitoid massifs, in the sediments contained in the alpine foreland basin. This research ties in with ongoing debates on the timing and mechanisms of mountain building.
Christian Stranne, Matt O'Regan, Martin Jakobsson, Volker Brüchert, and Marcelo Ketzer
Solid Earth, 10, 1541–1554, https://doi.org/10.5194/se-10-1541-2019, https://doi.org/10.5194/se-10-1541-2019, 2019
Maximilian Rieder, Wencke Wegner, Monika Horschinegg, Stefanie Klackl, Nereo Preto, Anna Breda, Susanne Gier, Urs Klötzli, Stefano M. Bernasconi, Gernot Arp, and Patrick Meister
Solid Earth, 10, 1243–1267, https://doi.org/10.5194/se-10-1243-2019, https://doi.org/10.5194/se-10-1243-2019, 2019
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The formation of dolomite (CaMg(CO3)2), an abundant mineral in Earth's geological record, is still incompletely understood. We studied dolomites embedded in a 100 m thick succession of coastal alluvial clays of Triassic age in the southern Alps. Observation by light microscopy and Sr isotopes suggests that dolomites may spontaneously from concentrated evaporating seawater, in coastal ephemeral lakes or tidal flats along the western margin of the Triassic Tethys sea.
Salomé Mignard, Thierry Mulder, Philippe Martinez, and Thierry Garlan
Solid Earth, 10, 851–869, https://doi.org/10.5194/se-10-851-2019, https://doi.org/10.5194/se-10-851-2019, 2019
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A large quantity a continental material is transported to the oceans by the world rivers. Once in the ocean, these particles can be transported down the continental shelf thanks to underwater avalanches. The repetition of such massive events can form very important sedimentary deposits at the continent–ocean transition. Data obtained during an oceanic cruise in 2010 allowed us to study such a system located offshore of Gabon and to evaluate the importance sediment transport in this area.
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
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A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Leandra M. Weydt, Claus-Dieter J. Heldmann, Hans G. Machel, and Ingo Sass
Solid Earth, 9, 953–983, https://doi.org/10.5194/se-9-953-2018, https://doi.org/10.5194/se-9-953-2018, 2018
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This study focuses on the assessment of the geothermal potential of two extensive upper Devonian aquifer systems within the Alberta Basin (Canada). Our work provides a first database on geothermal rock properties combined with detailed facies analysis (outcrop and core samples), enabling the identification of preferred zones in the reservoir and thus allowing for a more reliable reservoir prediction. This approach forms the basis for upcoming reservoir studies with a focus on 3-D modelling.
Ernest Chi Fru, Stephanos Kilias, Magnus Ivarsson, Jayne E. Rattray, Katerina Gkika, Iain McDonald, Qian He, and Curt Broman
Solid Earth, 9, 573–598, https://doi.org/10.5194/se-9-573-2018, https://doi.org/10.5194/se-9-573-2018, 2018
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Banded iron formations (BIFs) are chemical sediments last seen in the marine sedimentary record ca. 600 million years ago. Here, we report on the formation mechanisms of a modern BIF analog in the Cape Vani sedimentary basin (CVSB) on Milos Island, Greece, demonstrating that rare environmental redox conditions, coupled to submarine hydrothermal activity and microbial processes, are required for these types of rocks to form in the modern marine biosphere.
Cited articles
Abad, I.: Physical meaning and applications of the illite Kübler Index:
measuring reaction progress in low-grade metamorphism, Semin. la Soc.
Española Mineral., 3, 53–64, 2007.
Árkai, P., Mählmann, R. F., Suchý, V., Balogh, K.,
Sýkorová, I., and Frey, M.: Possible effects of tectonic shear strain
on phyllosilicates: a case study from the Kandersteg area, Helvetic domain,
Central Alps, Switzerland, Schweizerische Mineral. und Petrogr.
Mitteilungen, 82, 273–290, 2002.
Aubouin, J.: Contribution à l'étude géologique de la Grèce septentrionale: les confins de l'Epire et de la Thessalie, Ann. Geol. Pays Hell., 10, 1–483, 1959.
Aubouin, J.: Des tectoniques superposées et de leur signification par
rapport aux modèlesmodeles géophysiques; l'exemple des Dinarides;
paleotectonique, tectonique, tarditectonique, neotectonique, Bull. la
Société géologique Fr., 7, 426–460, 1973.
Baumgartner, P. O.: Jurassic sedimentary evolution and nappe emplacement in
the Argolis Peninsula (Peloponnesus, Greece), Mem. Soc. Helv. Sci. Nat., 99,
1–111, 1985.
Beaufort, D., Rigault, C., Billon, S., Billault, V., Inoue, A., Inoue, S.,
and Patrier, P.: Chlorite and chloritization processes through mixed-layer
mineral series in low-temperature geological systems – a review, Clay
Miner., 50, 497–523, https://doi.org/10.1180/claymin.2015.050.4.06, 2015.
Bernoulli, D. and Laubscher, H.: The palinspatic problem of the Hellenides
The Palinspastic Problem of the Hellenides, Eclogae Geol. Helv., 65,
107–118, 1972.
Bonneau, M., Godfriaux, I., Moulas, Y., Fourcade, E., and Masse, J.:
Stratigraphie et structure de la Bordure orientale de la double fenetre du
Paikon (Macedoine, Grece), Bull. Geol. Soc. Greece, 30, 105–114, 1994.
Boudagher-Fadel, M. and Price, G.: Global evolution and paleogeographic distribution of mid-Cretaceous orbitolinids, UCL Open Environ., 1, doi:10.14324/111.444/ucloe.000001, 2019.
Bortolotti, V., Kodra, A., Marroni, M., Mustafa, F., Pandolfi, L., Principi,
G., and Saccani, E.: Geology and petrology of ophiolitic sequences in the
Mirdita Region (Northern Albania), Ofioliti, 21, 3–20, 1996.
Bortolotti, V., Marroni, M., Pandolfi, L., and Principi, G.: Mesozoic to
tertiary tectonic history of the Mirdita ophiolites, northern Albania, Isl.
Arc, 14, 471–493, https://doi.org/10.1111/j.1440-1738.2005.00479.x, 2005.
Brandon, M. T., Roden-Tice, M. K., and Garver, J. I.: Late Cenozoic
exhumation of the Cascadia accretionary wedge in the Olympic Mountains,
northwest Washington State, GSA Bull., 110, 985–1009,
https://doi.org/10.1130/0016-7606(1998)110<0985:LCEOTC>2.3.CO;2,
1998.
Brown, S. A. M. and Robertson, A. H. F.: Sedimentary geology as a key to
understanding the tectonic evolution of the Mesozoic-Early Tertiary Paikon
Massif, Vardar suture zone, N Greece, Sediment. Geol., 160, 179–212,
https://doi.org/10.1016/S0037-0738(02)00376-7, 2003.
Brown, S. A. M. and Robertson, A. H. F.: Evidence for Neotethys rooted
within the Vardar suture zone from the Voras Massif, northernmost Greece,
Tectonophysics, 381, 143–173, https://doi.org/10.1016/j.tecto.2002.06.001, 2004.
Brun, J. P. and Sokoutis, D.: Kinematics of the Southern Rhodope Core Complex (North Greece), Int. J. Earth Sci., 96, 1079–1099, doi:10.1007/s00531-007-0174-2, 2007.
Brunn, J. H.: Geological Map of Greece, Veroia Sheet 1:50.000, IGME., Athens, Greece, 1982.
Burg, J. P.: Rhodope: From mesozoic convergence to cenozoic extension.
Review of petro-structural data in the geochronological frame, J. Virtual
Explor., 42, 1–44, https://doi.org/10.3809/jvirtex.2011.00270, 2012.
Burg, J. P., Ricou, L. E., Ivanov, Z., Godfriaux, I., Dimov, D., and Klain, L.: Syn-metamorphic nappe complex in the rhodope massif. Structure and kinematics, Terra Nov., 8, 6–15, doi:10.1111/j.1365-3121.1996.tb00720.x, 1996.
Burnett, J. A., Gallagher, L. T., and Hampton, M. J.: Upper Cretaceous, in: Calcareous nannofossil biostratigraphy, edited by: Bown, P. R., 132–199, Chapman and Hall, London, 1998.
Camoin, G.: Nature and Origin of Late Cretaceous Mud-Mounds, North Africa,
in: Carbonate Mud-Mounds: Their Origin and Evolution, edited by: Monty, C. L., Bosence, D. W., Bridges, P. H., and Pratt, B. R., Blackwell
Publishing Ltd, Oxford, UK, 385–400, 1995.
Channell, J. E. and Hovarth, F.: The African/Adriatic promontory as a
palaeogeographical premise for the Alpine orogeny and plate movements in the
Carpatho-Balkan region, Tectonophysics, 35, 71–101, 1976.
Chiari, M., Baumgartner, P. O., Bernoulli, D., Bortolotti, V., Marcucci, M.,
Photiades, A., and Principi, G.: Late Triassic, Early and Middle Jurassic
Radiolaria from ferromanganese-chert “nodules” (Angelokastron, Argolis,
Greece): Evidence for prolonged radiolarite sedimentation in the
Maliac-Vardar Ocean, Facies, 59, 391–424, https://doi.org/10.1007/s10347-012-0314-4,
2013.
Cohen, K. M., Finney, S. C., Gibbard, P. L., and Fan, J.-X.: The ICS
international chronostratigraphic chart, Episodes, 36, 199–204, 2013.
Coutand, I., Walsh, M., Louis, B., Chanier, F., Ferrière, J. and Reynaud, J. Y.: Neogene upper-crustal cooling of the Olympus range (northern Aegean): Major role of Hellenic back-arc extension over propagation of the North Anatolia Fault Zone, Terra Nov., 26, 287–297, doi:10.1111/ter.12099, 2014.
Dellisanti, F., Pini, G. A., Tateo, F., and Baudin, F.: The role of tectonic shear strain on the illitization mechanism of mixed-layers illite-smectite. A case study from a fault zone in the Northern Apennines, Italy, Int. J. Earth Sci., 97, 601–616, doi:10.1007/s00531-007-0180-4, 2008.
Dimitrijevic, M. D.: Dinarides: an outline of tectonics, Earth Evol. Sci.,
2, 4–23, 1982.
Dimo-Lahitte, A., Monié, P., and Vergély, P.: Metamorphic soles from
the Albanian ophiolites: Petrology, 40Ar ∕ 39Ar geochronology, and geodynamic
evolution, Tectonics, 20, 78–96, 2001.
Dinter, D. A. and Royden, L.: Late Cenozoic extension in northeastern
Greece: Strymon Valley detachment system and Rhodope metamorphic core
complex, Geology, 21, 45–48, 1993.
Ferriere, J., Baumgartner, P. O., and Chanier, F.: The Maliac Ocean: the
origin of the Tethyan Hellenic ophiolites, Int. J. Earth Sci., 105,
1941–1963, https://doi.org/10.1007/s00531-016-1303-6, 2016.
Froitzheim, N., Jahn-Awe, S., Frei, D., Wainwright, A. N., Maas, R.,
Georgiev, N., Nagel, T. J., and Pleuger, J.: Age and composition of
meta-ophiolite from the Rhodope Middle Allochthon (Satovcha, Bulgaria): A
test for the maximum-allochthony hypothesis of the Hellenides, Tectonics,
33, 1477–1500, 2014.
Furlong, K. P. and Edman, J. D.: Hydrocarbon maturation in thrust belts:
Thermal considerations, in: Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources, edited by: Price, R. A., American Geophysical Union, Washington, D.C., USA, 137–144, 1989.
Galbraith, R. F.: On statistical models for fission track counts, J. Int.
Assoc. Math. Geol., 13, 471–478, https://doi.org/10.1007/BF01034498, 1981.
Gautier, P., Brun, J. P., and Jolivet, L.: Structure and kinematics of Upper
Cenozoic extensional detachment on Naxos and Paros (Cyclades Islands,
Greece), Tectonics, 12, 1180–1194, 1993.
Gautier, P., Brun, J. P., Moriceau, R., Sokoutis, D., Martinod, J., and
Jolivet, L.: Timing, kinematics and cause of Aegean extension: A scenario
based on a comparison with simple analogue experiments, Tectonophysics,
315, 31–72, https://doi.org/10.1016/S0040-1951(99)00281-4, 1999.
Gili, E., Masse, J.-P., and Skelton, P. W.: Rudists as gregarious
sediment-dwellers, not reef-builders , on Cretaceous carbonate platforms,
Palaeogeogr. Palaeocl., 118, 245–267, 1995.
Godfriaux, I. and Ricou, L. E.: Le Paikon, une fenêtre tectonique dans
les Hellènides internes (Macédoine, Grèce), Comptes rendus
l'Académie des Sci. Série 2, Mécanique, Phys. Chim. Sci.
l'univers, Sci. la Terre, 313, 1479–1484, 1991.
Godfriaux, I., Ferriere, J., and Schmitt, A.: Le développement en
contexte continental d'un métamorphisme HP/BT: les “schistes bleus”
tertiaires Thessaliens, Bull. Geol. Soc. Greece, XX, 175–192, 1988.
Graham, C. M. and England, P. C.: Thermal regimes and regional metamorphism
in the vicinity of overthrust faults: an example of shear heating and
inverted metamorphic zonation from Southern California, Earth, 31, 142–152,
1976.
Grubić, A., Radoičić, R., Knežević, M., and Cvijić,
R.: Occurrence of Upper Cretaceous pelagic carbonates within
ophiolite-related pillow basalts in the Mt. Kozara area of the Vardar zone
western belt, northern Bosnia, Lithos, 108, 126–130, 2009.
Haq, B. U.: Cretaceous eustasy revisited, Global Planet. Change, 113,
44–58, 2014.
Jaboyedoff, M., Kubler, B., Sartori, M., and Thelin, P.: Basis for meaningful
illite crystallinity measurements: an example from the Swiss Prealps,
Schweizerische Mineral. und Petrogr. Mitteilungen, 80, 75–83, 2000.
Jolivet, L. and Brun, J. P.: Cenozoic geodynamic evolution of the Aegean,
Int. J. Earth Sci., 99, 109–138, https://doi.org/10.1007/s00531-008-0366-4, 2010.
Katrivanos, E., Kilias, A., and Mountrakis, D.: Kinematics of deformation and
structural evolution of the Paikon Massif (Central Macedonia, Greece): A
Pelagonian tectonic window?, Neues Jahrb. für Geol. und
Paläontologie-Abhandlungen, 269, 149–171, 2013.
Kilias, A., Frisch, W., Avgerinas, A., Dunkl, I., Falalakis, G., and Gawlick,
H. J.: Alpine architecture and kinematics of deformation of the northern
Pelagonian nappe pile in the Hellenides, Austrian J. Earth Sci., 103,
4–28, 2010.
Kossmat, F.: Geologie der zentralen Balkanhalbinsel: Mit einer Übersicht des dinarischen Gebirgsbaus, 12th ed., Gebrüder Bornträger, Berlin, 1924.
Kübler, B. and Jaboyedoff, M.: Illite crystallinity, Comptes Rendus
l'Académie Sci. – Ser. IIa Sci. la Terre des Planetes, 331, 75–89,
https://doi.org/10.1016/S1251-8050(00)01395-1, 2000.
Lacassin, R., Arnaud, N., Leloup, P., Armijo, R., and Meyer, B.: Syn- and
post-orogenic exhumation of metamorphic rocks in North Aegean, eEarth, 2,
51–63, 2007.
Lips, A. L. W., White, S. H., and Wijbrans, J. R.: 40Ar ∕ 39Ar laserprobe
direct dating of discrete deformational events: A continuous record of early
Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece,
Tectonophysics, 298, 133–153, https://doi.org/10.1016/S0040-1951(98)00181-4,
1998.
Lips, A. L. W., Wijbrans, J. R., and White, S. H.: New insights from 40Ar ∕ 39Ar laserprobe dating of white mica fabrics from the Pelion Massif, Pelagonian Zone, Internal Hellenides, Greece: implications for the timing of metamorphic episodes and tectonic events in the Aegean region, Geol. Soc. Spec. Publ., 156, 457–474, doi:10.1144/GSL.SP.1999.156.01.21, 1999.
Lister, G. S., Banga, G., and Feenstra, A.: Metamorphic core complexes of
Cordilleran type in the Cyclades, Aegean Sea, Greece, Geology, 12,
221–225, https://doi.org/10.1130/0091-7613(1984)12<221:MCCOCT>2.0.CO;2, 1984.
Luciani, V. and Cobianchi, M.: The Bonarelli Level and other black shales in
the Cenomanian-Turonian of the northeastern Dolomites (Italy): calcareous
nannofossil and foraminiferal data, Cretac. Res., 20, 135–167,
https://doi.org/10.1006/cres.1999.0146, 1999.
Matthews, K. J., Seton, M., and Müller, R. D.: A global-scale plate
reorganization event at 105–100 Ma, Earth Planet. Sc. Lett.,
355/356, 283–298, 2012.
Mercier, J.: Etude géologique des zones internes des Hellénides en Macédoine centrale (Grece), Ann. Geol. Pays Hell., 20, 1–792, 1968.
Mercier, J. and Vergely, P.: The Paikon massif revisited, comments on the late Cretaceous-Paleogene geodynamics of the Axios-Vardar zone: how many Jurassic ophiolitic basins? (Hellenides, Macedonia, Greece), Bull. Geol. Soc. Greece, 24, 2099–2112, https://doi.org/10.12681/bgsg.16852, 2002.
Mercier, J. L., Sorel, D. and Simeakis, K.: Changes in the state of stress in the overriding plate of a subduction zone: the Aegean Arc from the Pliocene to the Present, Ann. Tectonicae, 1, 20–39, 1987.
Merriman, R. J. and Peacor, D. R.: Very Low‐Grade Metapelites: Mineralogy, Microfabrics and Measuring Reaction Progress, in Low‐Grade Metamorphism, edited by: M. Frey and D. Robinson, Blackwell Science Ltd, Oxford, 10–60, https://doi.org/10.1002/9781444313345.ch2, 1998.
Mort, H., Jacquat, O., Adatte, T., Steinmann, P., Föllmi, K., Matera,
V., Berner, Z., and Stüben, D.: The Cenomanian/Turonian anoxic event at
the Bonarelli Level in Italy and Spain: enhanced productivity and/or better
preservation?, Cretac. Res., 28, 597–612,
https://doi.org/10.1016/j.cretres.2006.09.003, 2007.
Most, T.: Geodynamic evolution of the Eastern Pelagonian Zone in northwestern Greece and the Republic of Macedonia: Implications from U/Pb, Rb/Sr, K/Ar, 40Ar/39Ar geochronology and fission track thermochronology, Ph. D. thesis, Eberhardt-Karls-Universität Tübingen, Germany, 98 pp., 2003.
Moulas, E., Schenker, F. L., Burg, J. P., and Kostopoulos, D.: Metamorphic conditions and structural evolution of the Kesebir-Kardamos dome: Rhodope metamorphic complex (Greece-Bulgaria), Int. J. Earth Sci., 106, 2667–2685, doi:10.1007/s00531-017-1452-2, 2017.
Negra, M. H., Purser, B. H., and M'Rabet, A.: Sedimentation, Diagenesis and
Syntectonic Erosion of Upper Cretaceous Rudist Mounds in Central Tunisia, in:
Carbonate Mud-Mounds: Their Origin and Evolution, edited by: Monty, C. L.,
Bosence, D. W., Bridges, P. H., and Pratt, B. R., Blackwell
Publishing Ltd, Oxford, UK, 401–419, 1995.
Negri, A., Cobianchi, M., Luciani, V., Fraboni, R., Milani, A., and Claps,
M.: Tethyan Cenomanian pelagic rhythmic sedimentation and Pleistocene
Mediterranean sapropels: Is the biotic signal comparable?, Palaeogeogr.
Palaeocl., 190, 373–397,
https://doi.org/10.1016/S0031-0182(02)00615-6, 2003.
Nirta, G., Moratti, G., Piccardi, L., Montanari, D., Catanzariti, R.,
Carras, N., and Papini, M.: The boeotian flysch revisited: New constraints on
ophiolite obduction in central Greece, Ofioliti, 40, 107–123,
https://doi.org/10.4454/ofioliti.v40i2.438, 2015.
Nirta, G., Moratti, G., Piccardi, L., Montanari, D., Carras, N.,
Catanzariti, R., Chiari, M., and Marcucci, M.: From obduction to continental
collision: New data from Central Greece, Geol. Mag., 155, 377–421,
https://doi.org/10.1017/S0016756817000942, 2018.
Papanikolau, D.: Are the medial crystalline massifs of the Eastern
Mediterranean drifted Gondwanian fragments?, Geol. Soc. Greece Spec. Publ.,
1, 63–90, 1989.
Papanikolaou, D.: The tectonostratigraphic terranes of the Hellenides, Annales géologiques des pays Helléniques, 37, 495–514,
1997.
Papanikolaou, D.: Timing of tectonic emplacement of the ophiolites and
terrane paleogeography in the Hellenides, Lithos, 108, 262–280,
https://doi.org/10.1016/j.lithos.2008.08.003, 2009.
Papanikolaou, D. J. and Royden, L. H.: Disruption of the Hellenic arc: Late
Miocene extensional detachment faults and steep Pliocene-Quaternary normal
faults – Or what happened at Corinth?, Tectonics, 26, 1–16,
https://doi.org/10.1029/2006TC002007, 2007.
Picotti, V., Cobianchi, M., Luciani, V., Blattmann, F., Schenker, T.,
Mariani, E., Bernasconi, S. M., and Weissert, H.: Change from rimmed to ramp
platform forced by regional and global events in the Cretaceous of the
Friuli-Adriatic Platform (Southern Alps, Italy), Cretaceous Res., 104, https://doi.org/10.1016/j.cretres.2019.07.007, 104177, 2019.
Reiners, P. W. and Brandon, M. T.: Using Thermochronology To Understand
Orogenic Erosion, Annu. Rev. Earth Planet. Sci., 34, 419–466,
https://doi.org/10.1146/annurev.earth.34.031405.125202, 2006.
Ricou, L.-E. and Godfriaux, I.: Mise au point sur la fenêtre multiple du
Paikon et la structure du Vardar en Grèce, Comptes rendus l'Académie
des Sci. Série 2, Sci. la terre des planètes, 321, 601–608,
1995.
Ricou, L. E., Dercourt, J., Geyssant, J., Grandjacquet, C., Lepvrier, C., and Biju-Duval, B.: Geological constraints on the alpine evolution of the Mediterranean Tethys, Tectonophysics, 123, 83–86, doi:10.1016/0040-1951(86)90194-0, 1986.
Ricou, L. E., Burg, J. P., Godfriaux, I., and Ivanov, Z.: Rhodope and Vardar: The metamorphic and the olistostromic paired belts related to the Cretaceous subduction under Europe, Geodin. Acta, 11, 285–309, doi:10.1016/S0985-3111(99)80018-7, 1998.
Riding, R.: Microbial carbonates: The geological record of calcified bacterial-algal mats and biofilms, Sedimentology, 47, 179–214, doi:10.1046/j.1365-3091.2000.00003.x, 2000.
Ring, U., Glodny, J., Will, T., and Thomson, S.: The Hellenic subduction
system: high-pressure metamorphism, exhumation, normal faulting, and
large-scale extension, Annu. Rev. Earth Planet. Sci., 38, 45–76, 2010.
Robertson, A. H. F. and Dixon, J. E.: Introduction: aspects of the
geological evolution of the Eastern Mediterranean, Geol. Evol. East.
Mediterr., 17, 1–74, https://doi.org/10.1144/GSL.SP.1984.017.01.02, 1984.
Sanders, D.: Upper Cretaceous “Rudist” formations, Geol. Mitteilungen
Innsbruck, 23, 37–59, 1998.
Sanders, D. and Höfling, R.: Carbonate deposition in mixed-siliciclastic-carbonate environments on top of an orogenic wedge (Late Cretaceous,
Northern Calcareous Alps, Austria), Sed. Geol., 137, 127–146, 2000.
Sanders, D. and Pons, J. M.: Rudist formations in mixed
siliciclastic-carbonate depositional environments, Upper Cretaceous,
Austria: Stratigraphy, sedimentology, and models of development,
Palaeogeogr. Palaeocl., 148, 249–284,
https://doi.org/10.1016/S0031-0182(98)00186-2, 1999.
Schenker, F. L.: Thermo-mechanical evolution of the Pelagonian Gneiss Dome (Greece): Insights from numerical modeling and new geological and geochronological data, Ph. D thesis, ETH Zurich, Switzerland, 186 pp., 2013.
Schenker, F. L., Burg, J. P., Kostopoulos, D., Moulas, E., Larionov, A., and
Von Quadt, A.: From mesoproterozoic magmatism to collisional cretaceous
anatexis: Tectonomagmatic history of the Pelagonian Zone, Greece, Tectonics,
33, 1552–1576, https://doi.org/10.1002/2014TC003563, 2014.
Schenker, F. L., Fellin, M. G., and Burg, J.-P.: Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data, Solid Earth, 6, 285–302, https://doi.org/10.5194/se-6-285-2015, 2015.
Schenker, F. L., Burg, J.-P., Kostopoulos, D., Baumgartner, L. P., and
Bouvier, A.-S.: Carbonatitic dykes during Pangaea transtension (Pelagonian
Zone, Greece), Lithos, 302/303, 329–340, https://doi.org/10.1016/j.lithos.2018.01.011,
2018.
Schermer, E. R.: Geometry and kinematics of continental basement deformation
during the Alpine orogeny, Mt. Olympos region, Greece, J. Struct. Geol.,
15, 571–591, https://doi.org/10.1016/0191-8141(93)90149-5, 1993.
Schermer, E. R., Lux, D. R., and Clark Burchfiel, B.: Temperature-time
history of subducted continental crust, Mount Olympus region, Greece,
Tectonics, 9, 1165–1195, 1990.
Schmid, S. M., Bernoulli, D., Fügenschuh, B., Matenco, L., Schefer, S.,
Schuster, R., Tischler, M., and Ustaszewski, K.: The
Alpine-Carpathian-Dinaridic orogenic system: Correlation and evolution of
tectonic units, Swiss J. Geosci., 101, 139–183,
https://doi.org/10.1007/s00015-008-1247-3, 2008.
Schmid, S. M., Fügenschuh, B., Kounov, A., Maţenco, L., Nievergelt,
P., Oberhänsli, R., Pleuger, J., Schefer, S., Schuster, R., and
Tomljenović, B.: Tectonic units of the Alpine collision zone between
Eastern Alps and western Turkey, Gondwana Res., 78, 308–374, 2020.
Scott, R. W.: Evolution of Late Jurassic and Early Cretaceous Reef Biotas,
Palaios, 3, 184–193, 1988.
Sharp, I. R. and Robertson, A. H. F.: Tectonic-sedimentary evolution of the
western margin of the Mesozoic Vardar Ocean: evidence from the Pelagonian
and Almopias zones, northern Greece, Geol. Soc. London, Spec. Publ., 260,
373–412, https://doi.org/10.1144/GSL.SP.2006.260.01.16, 2006.
Smith, A. G., Hynes, A. J., Menzies, M., Nisbet, E. G., Price, I., Welland,
M. J., and Ferrière, J.: The stratigraphy of the Othris Mountains,
eastern central Greece: a deformed Mesozoic continental margin sequence,
Eclogae Geol. Helv., 68, 463–481, 1975.
Ustaszewski, K., Schmid, S. M., Lugović, B., Schuster, R., Schaltegger,
U., Bernoulli, D., Hottinger, L., Kounov, A., Fügenschuh, B., and
Schefer, S.: Late Cretaceous intra-oceanic magmatism in the internal
Dinarides (northern Bosnia and Herzegovina): Implications for the collision
of the Adriatic and European plates, Lithos, 108, 106–125,
https://doi.org/10.1016/j.lithos.2008.09.010, 2009.
Van Hinsbergen, D. J. J., Hafkenscheid, E., Spakman, W., Meulenkamp, J. E.,
and Wortel, R.: Nappe stacking resulting from subduction of oceanic and
continental lithosphere below Greece, Geology, 33, 325–328, 2005.
Vergély, P. and Mercier, J.-L.: New data concerning thrusting subsequent to
the Late Cretaceous in the Paikon massif (Axios-Vardar zone, Macedonia,
Greece): A new structural model [Données nouvelles sur les
chevauchements d'âge post-Crétacé supérieur dans le massif
du Paikon (zone de l'Axios-Vardar, Macédoine, Grèce): Un nouveau
modèle structural], Comptes Rendus de l'Académie de Sciences –
Série IIa: Sciences de la Terre et des Planètes, 330, 555–561, 2000
Vermeesch, P.: On the visualisation of detrital age distributions, Chem.
Geol., 312/313, 190–194, https://doi.org/10.1016/j.chemgeo.2012.04.021, 2012.
Voigt, S., Hay, W. W., Höfling, R., and DeConto, R. M.: Biogeographic
distribution of late early to Late Cretaceous rudist-reefs in the
mediterranean as climate indicators, Spec. Pap. Geol. Soc. Am., 332,
91–103, https://doi.org/10.1130/0-8137-2332-9.91, 1999.
Zimmerman, J. J. J. and Ross, J. J. V.: Structural evolution of the Vardar
root zone, northern Greece, Geol. Soc. Am. Bull., 87, 1547–1550,
https://doi.org/10.1130/0016-7606(1976)87<1547:SEOTVR>2.0.CO;2, 1976.
Short summary
The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar...
Special issue