Articles | Volume 6, issue 1
https://doi.org/10.5194/se-6-49-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-6-49-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
14 Jan 2015
Research article |
| 14 Jan 2015
Magma storage and plumbing of adakite-type post-ophiolite intrusions in the Sabzevar ophiolitic zone, northeast Iran
K. Jamshidi
CORRESPONDING AUTHOR
Faculty of Earth Sciences, Shahrood University, Shahrood, Iran
Department of Earth Sciences, CEMPEG, Uppsala University, Uppsala, Sweden
H. Ghasemi
Faculty of Earth Sciences, Shahrood University, Shahrood, Iran
V. R. Troll
Department of Earth Sciences, CEMPEG, Uppsala University, Uppsala, Sweden
M. Sadeghian
Faculty of Earth Sciences, Shahrood University, Shahrood, Iran
B. Dahren
Department of Earth Sciences, CEMPEG, Uppsala University, Uppsala, Sweden
Related authors
No articles found.
Daniel Müller, Thomas R. Walter, Valentin R. Troll, Jessica Stammeier, Andreas Karlsson, Erica de Paolo, Antonino Fabio Pisciotta, Martin Zimmer, and Benjamin De Jarnatt
Solid Earth, 15, 1155–1184, https://doi.org/10.5194/se-15-1155-2024, https://doi.org/10.5194/se-15-1155-2024, 2024
Short summary
Short summary
We use uncrewed-aerial-system-derived optical and infrared data, mineralogical and geochemical analyses of rock samples, and surface degassing measurements to analyze degassing and hydrothermal alteration at the fumaroles of the La Fossa cone, Vulcano island, Italy. We give a detailed view of associated structures and dynamics, such as local alteration gradients, diffuse active units that significantly contribute to the total activity, or effects of permeability reduction and surface sealing.
Herlan Darmawan, Thomas R. Walter, Valentin R. Troll, and Agus Budi-Santoso
Nat. Hazards Earth Syst. Sci., 18, 3267–3281, https://doi.org/10.5194/nhess-18-3267-2018, https://doi.org/10.5194/nhess-18-3267-2018, 2018
Short summary
Short summary
At Merapi volcano, lava dome failure may generate pyroclastic flow and threaten populations who live on its flanks. Here, we assessed the potential hazard of the Merapi lava dome by using drone photogrammetry and numerical modeling. Results show a weak structural depression that is associated with high thermal imaging in the southern Merapi lava dome sector. The southern lava dome sector may be further destabilized by typical rainfall at the Merapi summit and produce pyroclastic flow up to 4 km.
Related subject area
Petrology
Contribution of carbonatite and recycled oceanic crust to petit-spot lavas on the western Pacific Plate
Interdisciplinary fracture network characterization in the crystalline basement: a case study from the Southern Odenwald, SW Germany
Matrix gas flow through “impermeable” rocks – shales and tight sandstone
Benchmark study using a multi-scale, multi-methodological approach for the petrophysical characterization of reservoir sandstones
First report of ultra-high pressure metamorphism in the Paleozoic Dunhuang orogenic belt (NW China): Constrains from P-T paths of garnet clinopyroxenite and SIMS U-Pb dating of titanite
Yttrium speciation in subduction-zone fluids from ab initio molecular dynamics simulations
Tracing fluid transfers in subduction zones: an integrated thermodynamic and δ18O fractionation modelling approach
Post-entrapment modification of residual inclusion pressure and its implications for Raman elastic thermobarometry
Anatomy of the magmatic plumbing system of Los Humeros Caldera (Mexico): implications for geothermal systems
Alkali basalt from the Seifu Seamount in the Sea of Japan: post-spreading magmatism in a back-arc setting
Magmatic sulfides in high-potassium calc-alkaline to shoshonitic and alkaline rocks
Chemical heterogeneities in the mantle: progress towards a general quantitative description
Deeply subducted continental fragments – Part 1: Fracturing, dissolution–precipitation, and diffusion processes recorded by garnet textures of the central Sesia Zone (western Italian Alps)
Deeply subducted continental fragments – Part 2: Insight from petrochronology in the central Sesia Zone (western Italian Alps)
Interpretation of zircon coronae textures from metapelitic granulites of the Ivrea–Verbano Zone, northern Italy: two-stage decomposition of Fe–Ti oxides
Arrested development – a comparative analysis of multilayer corona textures in high-grade metamorphic rocks
Multi-phase classification by a least-squares support vector machine approach in tomography images of geological samples
Calculating structural and geometrical parameters by laboratory measurements and X-ray microtomography: a comparative study applied to a limestone sample before and after a dissolution experiment
Qualitative and quantitative changes in detrital reservoir rocks caused by CO2–brine–rock interactions during first injection phases (Utrillas sandstones, northern Spain)
Magma mixing enhanced by bubble segregation
The rheological behaviour of fracture-filling cherts: example of Barite Valley dikes, Barberton Greenstone Belt, South Africa
Picroilmenites in Yakutian kimberlites: variations and genetic models
An experimental study of pyroxene crystallization during rapid cooling in a thermal gradient: application to komatiites
Floating stones off El Hierro, Canary Islands: xenoliths of pre-island sedimentary origin in the early products of the October 2011 eruption
Metamorphic history and geodynamic significance of the Early Cretaceous Sabzevar granulites (Sabzevar structural zone, NE Iran)
Kazuto Mikuni, Naoto Hirano, Shiki Machida, Hirochika Sumino, Norikatsu Akizawa, Akihiro Tamura, Tomoaki Morishita, and Yasuhiro Kato
Solid Earth, 15, 167–196, https://doi.org/10.5194/se-15-167-2024, https://doi.org/10.5194/se-15-167-2024, 2024
Short summary
Short summary
Plate tectonics theory is the motion of rocky plates (lithosphere) over ductile zones (asthenosphere). The causes of the lithosphere–asthenosphere boundary (LAB) are controversial; however, petit-spot volcanism supports the presence of melt at the LAB. We conducted geochemistry, geochronology, and geochemical modeling of petit-spot volcanoes on the western Pacific Plate, and the results suggested that carbonatite melt and recycled oceanic crust induced the partial melting at the LAB.
Matthis Frey, Claire Bossennec, Lukas Seib, Kristian Bär, Eva Schill, and Ingo Sass
Solid Earth, 13, 935–955, https://doi.org/10.5194/se-13-935-2022, https://doi.org/10.5194/se-13-935-2022, 2022
Short summary
Short summary
The crystalline basement is considered a ubiquitous and almost inexhaustible source of geothermal energy in the Upper Rhine Graben. Interdisciplinary investigations of relevant reservoir properties were carried out on analogous rocks in the Odenwald. The highest hydraulic conductivities are expected near large-scale fault zones. In addition, the combination of structural geological and geophysical methods allows a refined mapping of potentially permeable zones.
Ernest Rutter, Julian Mecklenburgh, and Yusuf Bashir
Solid Earth, 13, 725–743, https://doi.org/10.5194/se-13-725-2022, https://doi.org/10.5194/se-13-725-2022, 2022
Short summary
Short summary
Underground energy and waste storage require repurposing of existing oil and gas wells for gas storage, compressed air, hydrogen, methane, and CO2 disposal, requiring an impermeable cap rock (e.g. shales) over the porous reservoir. We measured shale permeability over a range of burial pressures and gas pore pressures. Permeability decreases markedly as effective pressure on the rocks is increased. Knowing these relationships is essential to the safe design of engineered gas reservoirs.
Peleg Haruzi, Regina Katsman, Matthias Halisch, Nicolas Waldmann, and Baruch Spiro
Solid Earth, 12, 665–689, https://doi.org/10.5194/se-12-665-2021, https://doi.org/10.5194/se-12-665-2021, 2021
Short summary
Short summary
In this paper, we evaluate a multi-methodological approach for the comprehensive characterization of reservoir sandstones. The approach enables identification of links between rock permeability and textural and topological rock descriptors quantified at microscale. It is applied to study samples from three sandstone layers of Lower Cretaceous age in northern Israel, which differ in features observed at the outcrop, hand specimen and micro-CT scales, and leads to their accurate characterization.
Zhen M. G. Li, Hao Y. C. Wang, Qian W. L. Zhang, Meng-Yan Shi, Jun-Sheng Lu, Jia-Hui Liu, and Chun-Ming Wu
Solid Earth Discuss., https://doi.org/10.5194/se-2020-95, https://doi.org/10.5194/se-2020-95, 2020
Preprint withdrawn
Short summary
Short summary
This manuscript provides the first evidence of ultra-high metamorphism in the Paleozoic Dunhuang orogenic belt (NW China). Though no coesite or diamond was found in the samples or in this orogen, the geothermobarometric computation results and petrographic textures all suggest that the garnet clinopyroxenite experienced ultra-high pressure metamorphism, and SIMS U-Pb dating of titanite indicates that the post peak, subsequent tectonic exhumation of the UHP rocks occurred in the Devonian.
Johannes Stefanski and Sandro Jahn
Solid Earth, 11, 767–789, https://doi.org/10.5194/se-11-767-2020, https://doi.org/10.5194/se-11-767-2020, 2020
Short summary
Short summary
The capacity of aqueous fluids to mobilize rare Earth elements is closely related to their molecular structure. In this study, first-principle molecular dynamics simulations are used to investigate the complex formation of yttrium with chloride and fluoride under subduction-zone conditions. The simulations predict that yttrium–fluoride complexes are more stable than their yttrium–chloride counterparts but likely less abundant due to the very low fluoride ion concentration in natural systems.
Alice Vho, Pierre Lanari, Daniela Rubatto, and Jörg Hermann
Solid Earth, 11, 307–328, https://doi.org/10.5194/se-11-307-2020, https://doi.org/10.5194/se-11-307-2020, 2020
Short summary
Short summary
This study presents an approach that combines equilibrium thermodynamic modelling with oxygen isotope fractionation modelling for investigating fluid–rock interaction in metamorphic systems. An application to subduction zones shows that chemical and isotopic zoning in minerals can be used to determine feasible fluid sources and the conditions of interaction. Slab-derived fluids can cause oxygen isotope variations in the mantle wedge that may result in anomalous isotopic signatures of arc lavas.
Xin Zhong, Evangelos Moulas, and Lucie Tajčmanová
Solid Earth, 11, 223–240, https://doi.org/10.5194/se-11-223-2020, https://doi.org/10.5194/se-11-223-2020, 2020
Short summary
Short summary
In this study, we present a 1-D visco-elasto-plastic model in a spherical coordinate system to study the residual pressure preserved in mineral inclusions. This allows one to study how much residual pressure can be preserved after viscous relaxation. An example of quartz inclusion in garnet host is studied and it is found that above 600–700 °C, substantial viscous relaxation will occur. If one uses the relaxed residual quartz pressure for barometry, erroneous results will be obtained.
Federico Lucci, Gerardo Carrasco-Núñez, Federico Rossetti, Thomas Theye, John Charles White, Stefano Urbani, Hossein Azizi, Yoshihiro Asahara, and Guido Giordano
Solid Earth, 11, 125–159, https://doi.org/10.5194/se-11-125-2020, https://doi.org/10.5194/se-11-125-2020, 2020
Short summary
Short summary
Understanding the anatomy of active magmatic plumbing systems is essential to define the heat source(s) feeding geothermal fields. Mineral-melt thermobarometry and fractional crystallization (FC) models were applied to Quaternary volcanic products of the Los Humeros Caldera (Mexico). Results point to a magmatic system controlled by FC processes and made of magma transport and storage layers within the crust, with significant implications on structure and longevity of the geothermal reservoir.
Tomoaki Morishita, Naoto Hirano, Hirochika Sumino, Hiroshi Sato, Tomoyuki Shibata, Masako Yoshikawa, Shoji Arai, Rie Nauchi, and Akihiro Tamura
Solid Earth, 11, 23–36, https://doi.org/10.5194/se-11-23-2020, https://doi.org/10.5194/se-11-23-2020, 2020
Short summary
Short summary
We report a peridotite xenolith-bearing basalt dredged from the Seifu Seamount (SSM basalt) in the northeast Tsushima Basin, southwest Sea of Japan, which is one of the western Pacific back-arc basin swarms. An 40Ar / 39Ar plateau age of 8.33 ± 0.15 Ma (2 σ) was obtained for the SSM basalt, indicating that it erupted shortly after the termination of back-arc spreading. The SSM basalt was formed in a post-back-arc extension setting by the low-degree partial melting of an upwelling asthenosphere.
Ariadni A. Georgatou and Massimo Chiaradia
Solid Earth, 11, 1–21, https://doi.org/10.5194/se-11-1-2020, https://doi.org/10.5194/se-11-1-2020, 2020
Short summary
Short summary
We study the petrographical and geochemical occurrence of magmatic sulfide minerals in volcanic rocks for areas characterised by different geodynamic settings, some of which are associated with porphyry (Cu and/or Au) and Au epithermal mineralisation. The aim is to investigate the role of magmatic sulfide saturation processes in depth for ore generation in the surface.
Massimiliano Tirone
Solid Earth, 10, 1409–1428, https://doi.org/10.5194/se-10-1409-2019, https://doi.org/10.5194/se-10-1409-2019, 2019
Short summary
Short summary
The prevalent assumption in solid Earth science is that if we have different lithologies in the mantle they are separately in chemical equilibrium and together in chemical disequilibrium; this is the condition that at the moment defines a chemically heterogeneous mantle. The main contribution of this study is to show that this may not be the case. We can have (partial) chemical equilibration between the two and still observe a chemically heterogeneous mantle.
Francesco Giuntoli, Pierre Lanari, and Martin Engi
Solid Earth, 9, 167–189, https://doi.org/10.5194/se-9-167-2018, https://doi.org/10.5194/se-9-167-2018, 2018
Short summary
Short summary
Continental high-pressure terranes in orogens offer insight into deep recycling and transformation processes that occur in subduction zones. These remain poorly understood, and currently debated ideas need testing. We document complex garnet zoning in eclogitic mica schists from the Sesia Zone (western Italian Alps). These retain evidence of two orogenic cycles and provide detailed insight into resorption, growth, and diffusion processes induced by fluid pulses under high-pressure conditions.
Francesco Giuntoli, Pierre Lanari, Marco Burn, Barbara Eva Kunz, and Martin Engi
Solid Earth, 9, 191–222, https://doi.org/10.5194/se-9-191-2018, https://doi.org/10.5194/se-9-191-2018, 2018
Short summary
Short summary
Subducted continental terranes commonly comprise an assembly of subunits that reflect the different tectono-metamorphic histories they experienced in the subduction zone. Our challenge is to unravel how, when, and in which part of the subduction zone these subunits were juxtaposed. Our study documents when and in what conditions re-equilibration took place. Results constrain the main stages of mineral growth and deformation, associated with fluid influx that occurred in the subduction channel.
Elizaveta Kovaleva, Håkon O. Austrheim, and Urs S. Klötzli
Solid Earth, 8, 789–804, https://doi.org/10.5194/se-8-789-2017, https://doi.org/10.5194/se-8-789-2017, 2017
Short summary
Short summary
This is a study of unusual coronae textures formed by zircon in granulitic metapelites, Ivrea–Verbano Zone (northern Italy). Zircon coronas occur in two generations: (1) thick (5–20 µm) crescent-shaped aggregates and (2) thin (≤ 1 µm) thread-shaped and tangled coronae. Both are found in the same petrological context, so that the difference between two generations is very conspicuous. Formation of zircon coronae is attributed to the two-stage decomposition of Fe–Ti oxides, a rich source of Zr.
Paula Ogilvie and Roger L. Gibson
Solid Earth, 8, 93–135, https://doi.org/10.5194/se-8-93-2017, https://doi.org/10.5194/se-8-93-2017, 2017
Short summary
Short summary
Coronas are vital clues to the presence of arrested reaction in metamorphic rocks. We review formation mechanisms of coronas and approaches utilized to model their evolution in P–T–X space. Forward modelling employing calculated chemical potential gradients allows a far more nuanced understanding of the intricacies that govern metamorphic reaction. These models have critical implications for the limitations and opportunities coronas afford in interpreting the evolution of metamorphic terranes.
Faisal Khan, Frieder Enzmann, and Michael Kersten
Solid Earth, 7, 481–492, https://doi.org/10.5194/se-7-481-2016, https://doi.org/10.5194/se-7-481-2016, 2016
Short summary
Short summary
X-ray microtomography image processing involves artefact reduction and image segmentation. The beam-hardening artefact is removed, applying a new algorithm, which minimizes the offsets of the attenuation data points. For the segmentation, we propose using a non-linear classifier algorithm. Statistical analysis was performed to quantify the improvement in multi-phase classification of rock cores using and without using our advanced beam-hardening correction algorithm.
Linda Luquot, Vanessa Hebert, and Olivier Rodriguez
Solid Earth, 7, 441–456, https://doi.org/10.5194/se-7-441-2016, https://doi.org/10.5194/se-7-441-2016, 2016
Short summary
Short summary
To evaluate oil and gas production, accurate characterization (usually based on laboratory experiments) of reservoir rock properties needs to be performed. X-ray scanning samples enable obtaining 3-D images of the rock inner structure from which those properties can be obtained using images processing. This article shows that these two approaches are complementary and yield consistent results. Moreover, image-based calculations allow to save a huge amount of time compared to lab-based measures.
E. Berrezueta, B. Ordóñez-Casado, and L. Quintana
Solid Earth, 7, 37–53, https://doi.org/10.5194/se-7-37-2016, https://doi.org/10.5194/se-7-37-2016, 2016
Short summary
Short summary
The aim of this article is to describe and interpret qualitative and quantitative changes at the rock matrix scale of Cretaceous sandstones (northern Spain) exposed to supercritical CO2 and brine. Experimental CO2-rich brine injection was performed in a reactor chamber under realistic conditions of deep saline formations (P ≈ 7.8 MPa, T ≈ 38 °C and 24 h exposure time). SEM and optical microscopy, aided by optical image processing and chemical analyses were used to study the rock samples.
S. Wiesmaier, D. Morgavi, C. J. Renggli, D. Perugini, C. P. De Campos, K.-U. Hess, W. Ertel-Ingrisch, Y. Lavallée, and D. B. Dingwell
Solid Earth, 6, 1007–1023, https://doi.org/10.5194/se-6-1007-2015, https://doi.org/10.5194/se-6-1007-2015, 2015
Short summary
Short summary
We reproduced in an experiment the mixing of two different magmas by bubbles. Bubbles form filaments when dragging portions of one magma into another and thus mingle both magmas. Bubble mixing must be an accelerating process in nature, because formed filaments are channels of low resistance for subsequently rising bubbles. In natural gas-rich magmas, this may be an important mechanism for magma mixing. Natural samples from Axial Seamount show evidence for bubble mixing.
M. Ledevin, N. Arndt, A. Davaille, R. Ledevin, and A. Simionovici
Solid Earth, 6, 253–269, https://doi.org/10.5194/se-6-253-2015, https://doi.org/10.5194/se-6-253-2015, 2015
Short summary
Short summary
We investigate the composition, physical and rheological properties of fluids at the origin of Palaeoarchean chert dikes in South Africa. The dikes formed by repetitive hydraulic fracturing as overpressured oceanic fluids were released at low temperatures as a siliceous slurry. The gelation capacity of silica conferred the chert precursor a viscoelastic, probably thixotrope behaviour. It is an additional step to understand fluid circulations towards the ocean floor, the habitat of early life.
I. V. Ashchepkov, N. V. Alymova, A. M. Logvinova, N. V. Vladykin, S. S. Kuligin, S. I. Mityukhin, H. Downes, Yu. B. Stegnitsky, S. A. Prokopiev, R. F. Salikhov, V. S. Palessky, and O. S. Khmel'nikova
Solid Earth, 5, 915–938, https://doi.org/10.5194/se-5-915-2014, https://doi.org/10.5194/se-5-915-2014, 2014
S. Bouquain, N. T. Arndt, F. Faure, and G. Libourel
Solid Earth, 5, 641–650, https://doi.org/10.5194/se-5-641-2014, https://doi.org/10.5194/se-5-641-2014, 2014
V. R. Troll, A. Klügel, M.-A. Longpré, S. Burchardt, F. M. Deegan, J. C. Carracedo, S. Wiesmaier, U. Kueppers, B. Dahren, L. S. Blythe, T. H. Hansteen, C. Freda, D. A. Budd, E. M. Jolis, E. Jonsson, F. C. Meade, C. Harris, S. E. Berg, L. Mancini, M. Polacci, and K. Pedroza
Solid Earth, 3, 97–110, https://doi.org/10.5194/se-3-97-2012, https://doi.org/10.5194/se-3-97-2012, 2012
M. Nasrabady, F. Rossetti, T. Theye, and G. Vignaroli
Solid Earth, 2, 219–243, https://doi.org/10.5194/se-2-219-2011, https://doi.org/10.5194/se-2-219-2011, 2011
Cited articles
Agard, P., Omrani, J., Jolivet, L., and Mouthereau, F.: Convergence history across Zagros (Iran): Constraints from collisional and earlier deformation, Int. J. Earth. Sci., 94, 401–419, 2005.
Agard, P., Omrani, J., Jolivet, L., Whitechurch, H., Vrielynck, B., Spakman, W., Monie, P., Meyer, B., and Wortel, R.: Zagros orogeny: a subduction-dominated process, Geol. Mag., 148, 692–725, 2011.
Allegre, C. J., Provost, A., and Jaupart, C.: Oscillatory zoning: a pathological case of crystal growth, Nature, 294, 223–-228, 1981.
Andrews, B. J., Gardner, J. E., and Housh, T. B.: Repeated recharge, assimilation, and hybridization in magmas erupted from El Chichón as recorded by plagioclase and amphibole phenocrysts, J. Volcanol. Geoth. Res., 175, 415–426, 2008.
Annen, C., Blundy, J. D., and Sparks, R. S. J.: The genesis of intermediate and silicic magmas in deep crustal hot zones, J. Petrol., 47, 505–539, 2006.
Arvin, M. and Robinson, P. T.: The petrogenesis and tectonic setting of lava from Baft ophiolitic melange, SW Kerman, Iran, Can. J. Earth Sci., 31, 824–834, 1994.
Azizi, H. and Moinevaziri, H.: Review for tectonic setting for Cretaceous to Quaternary volcanism in NW Iran, J. Geodyn., 47, 167–179, 2009.
Babazadeh, S. A and De Wever, P.: Early Cretaceous radiolarian assemblages from radiolarites in the Sistan Suture (eastern Iran), Geodiversitas, 26, 185–206, 2004.
Baroz, J., Macaudière, J., Montigny, R., Noghreyan, M., Ohnen stetter, M., and Rocci, G. A.: Ophiolites and related formations in the central part of the Sabzevar (Iran) and possible geotectonic reconstructions, Geodynamic Project (Geotraverse) in Iran: GSI, Report no. 51, 51–68, 1983.
Behrens, H. and Gaillard, F.: Geochemical aspects of melts: volatiles and redox behavior, Elements, 2, 275–280, 2006.
Berberian, F. and Berberian, M.: Tectono-plutonic episodes in Iran, in Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Geodynamics, 3, 5–32, 1981.
Berberian, F., Muir, I. D., Pankhurst, R. J., and Berberian, M.: Late Cretaceous and early Miocene Andean type plutonic activity in northern Makran and central Iran, J. Geol. Soc. London, 139, 605–614, 1982.
Berberian, M. and King, G.C.P.: Towards a paleogeography and tectonic evolution of Iran, Can. J. Earth Sci., 18, 210–265, 1981.
Bina, M. M., I. Bucur, I., Pervot, M., Meyerfeld, Y., Daly, L., Cantagrel, J. M., and Mergoil, J.: Palaeomagnetism petrology and geochronology of Tertiary magmatic and sedimentary units from Iran, Tectonophysics, 121, 303–329, 1986.
Blundy, J. D. and Holland T. J. B.: Calcic amphibole equilibria and a new amphiboleplagioclase geothermometer, Contrib. Mineral. Petr., 104, 208–224, 1990.
Bottinga, Y. Kudo, A., and Weill, D.: Some observation on oscillatory zoning and crystallization of magmatic plagioclase, Am. Mineral., 51, 792–806, 1966.
Castillo, P. R.: An overview of adakite petrogenesis, Chinese Sci. Bull., 51, 257–268, 2006.
Castillo, P. R.: Adakite petrogenesis., Lithos, 134, 304–316, 2012.
Chang, Z. and Meinert, L. D.: The magmatic–hydrothermal transition- evidence from quartz phenocryst textures and endoskarn abundance in Cu–Zn skarns at the Empire Mine, Idaho, USA. Chem. Geol., 210, 149–171, 2004.
Chaussard, E. and Amelung, F.: Regional controls on magma ascent and storage in volcanic Arcs, Geochem. Geophys. Geosyst., 1407–1418, 2014.
Chiaradia, M., Müntener, O., Beate, B., and Fontignie, D.: Adakite-like volcanism of Ecuador: lower crust magmatic evolution and recycling, Contrib. Mineral. Petr., 158, 563–588, 2009.
Danyushevsky, L. V., Falloon, T. J., Crawford, A. J., Tetroeva, S. A., Leslie, R. L., and Verbeeten, A.: High-Mg adakites from Kadavu Island Group, Fiji, southwest Pacific: evidence for the mantle origin of adakite parental melts, Geology, 36, 499–502, 2008.
Davidson, J., Turner, S., Handley, H., Mcpherson, C., and Dosseto, A.: Amphibole "sponge" in arc crust?, Geology, 35, 787–790, 2007.
Deer, W. A., Howie, R. A., and Sussman, J. Z.: An introduction to rock- forming minerals, Longman Ltd, 528 pp., 1986.
Defant, M. J. and Drummond, M. S.: Derivation of some modern arc magmas by melting of young subducted lithosphere, Nature, 347, 662–665, 1990.
Donaldson, C. H. and Henderson, C. M. B.: A new interpretation of round embayments quartz crystals, Mineral. Mag., 52, 27–33, 1988.
Foley, F., Norman, J., Pearson, N. J., Rushmer, T., Turner, S., and Adam, J.: Magmatic evolution and magma mixing of Quaternary adakites at Solander and little Solander Islands, New Zealand, J. Petrol., 54, 1–42, 2013.
Garcia, M. O. and Jacobson, S. S.: Crystal clots, amphibole fractionation and the evolution of calc-alkaline magmas, Contrib. Mineral. Petrol., 69, 319–327, 1979.
Ghasemi, H., Sadeghian, M., Khanalizadeh, A., and Tanha, A.: Petrography, geochemistry and radiometric ages of high-silica adakitic domes of Neogene continental arc, South of Quchan, Iranian J. Crystal. Mineral., 3, 347–370, 2010.
Ghasemi, H., Barahmand, M., and Sadeghian, M.: The Oligocene basaltic lavas of east and southeast of Shahroud: Implication for back-arc basin setting of Central Iran Oligo-Miocene basin, Petrol. J., 2, 77–94, 2011 (in Persian).
Gill, J. B.: Orogenic andesites and plate tectonics. Springer, New York, Springer-Verlag, 390 pp., 1981.
Ginibre, C., Gerhard Wörner, G., and Kronz, A.: Minor- and trace-element zoning in plagioclase: implications for magma chamber processes at Parinacota volcano, northern Chile, Contrib. Mineral. Petrol., 143, 300–315, 2002.
Guan, Q., Zhu, D. C., Zhao, Z. D., Zhang, L. L., Liu, M., Li, X. W., Yu, F., Liu, M. H., and Mo, X. X.: Late Cretaceous adakites from the eastern segment of the Gangdese Belt, Southern Tibet: products of Neo-Tethyan mid-ocean ridge subduction, Acta Petrol. Sin., 26, 2165–2179, 2010 (in Chinese with English abstract).
Guo, F., Nakamuru, E., Fan, W., Kobayoshi, K., and Li, C.: Generation of Paleocene adakitic andesites by magma mixing: Yanji area, NE China, J. Petrol., 48, 661–692, 2007.
Holland T. J. B. and Blundy, J. D.: Non-ideal interactions in calcic amphiboles and their bearing on amphibole-plagioclase thermometry, Contrib. Mineral. Petrol., 116, 433–447, 1994.
Houseman, G. A., McKenzie, D. P., and Molnar, P. J.: Convective instability of a thickened boundary layer and its relevance for the thermal evolution of continental convergent belts, J. Geophys. Res., 86, 6115–6132, 1981.
Housh, T. B. and Luhr, J. F.:Plagioclase-melt equilibria in hydrous system, Am. Mineral., 76, 477–492, 1991.
Humphreys, M. C. S., Blundy, J. D., and Sparks, R. S. J.: Magma evolution and open-system processes at Shiveluch volcano: insights from phenocrysts zoning, J. Petrol., 47, 2303–2334, 2006.
Humphreys, M. C. S., Christopher, T., and Hards, V.: Microlite transfer by disaggregation of mafic inclusions following magma mixing at Soufrie're Hills volcano, Montserrat, Contrib. Mineral. Petrol., 157, 609–624, 2009.
Irvine, T. N. and Baragar, W. R. A.: A guide to the chemical classification of the common volcanic rocks, Can. J. Earth Sci., 8, 523–548, 1971.
Jahangiri, A.: Post-collisional Miocene adakitic volcanism in NW Iran: Geochemical and geodynamic implications, J. Asian Earth Sci., 30, 433–447, 2007.
Jamshidi, K., Ghasemi, H., and Sadeghian, M.: Petrology and geochemistry of the Sabzevar post-ophiolitic high silica adakitic rocks, J. Petrol., 5, 51–68, 2014 (in Persian).
Keskin, M., Pearce, J. A., and Mitchell, J. G.: Volcano-stratigraphy and geochemistry of collision-related volcanism on the Erzurum-Kars Plateau, North Eastern Turkey, J. Volcanol. Geoth. Res., 85, 355–404, 1998.
Khalatbari Jafari, M., Babaie, H. A., and Gani, M.: Geochemical evidence for Late Cretaceous marginal arc-to-back arc transition in the Sabzevar ophiolitic extrusive sequence, northeast Iran, J. Asian Earth Sci., 70, 209–230, 2013.
Kohn, M. J. and Parkinson, C. D.: Petrologic case for Eocene slab break off during the Indo-Asian collision, Geology, 30, 591–594, 2002.
Le Bas, M. J., Le Maitre, R. W., Streckeisen, A., and Zanettin, B.: A chemical classification of volcanic rocks based on the total alkali-silica diagram, J. Petrol., 27, 745–750, 1986.
Leake, B. E.: Nomenclature of amphiboles. Am. Mineral., 63, 1023–1052, 1978.
Leake, B. E., Woolley, A. R., Arps, C. E. S., Birch, W. D., Gilbert, M. C., Grice, J. D., Hawthorne, F. C., Kato, A., Kisch, H. J., Krivovichev, V. G., Linthout, K., Laird, J., Mandarino, J. A., Maresch, W. V., Nickel, E. H., Rock, N. M. S., Schumacher, J. C., Smith, D. C., Stephenson, N. C. N., Ungaretti, L., Whittaker, E. J. W., and Youzhi, G.: Nomenclature of amphiboles: Report of the Subcommittee on Amphiboles of the International Mineralogical Association, Commission on New Minerals and Mineral Names, Am. Mineral., 82, 1019–1037, 1997.
Leake, B. E., Wooley, A. R., Birch, W. D., Burke, E. A. J., Ferraris, G, Grice, J. D., Hawthorne, F. C., Kisch, H. J., Krivovichev, V. G., Schumacher, J. C., Stephenson, N. C. N., and Whittaker, E. J. W.: Nomenclature of amphiboles: Additions and revisions to the International Mineralogical Associations amphibole nomenclature, Am. Mineral., 89, 883–887, 2004.
Le Maitre, R. W.: Some Problems of the Projection of Chemical Data into Mineralogical Classifications, Contrib. Mineral. Petrol., 56, 181–189, 1976.
Lensch, G.: Major element geochemistry of the ophiolites in north-eastern Iran, in: "Ophiolites, Proceedings Intern. Ophiolite Symposium, Cyprus 1979", edited by: Panayotou, A., Geological Survey Department, Cyprus, 398–401, 1980.
Lensch, G., Mihn, A., and Alavi-Tehrani, N.: Petrography and geology of the ophiolite belt north of Sabzevar/ Khorasan (Iran), Neues Jahrb. Geol. P-M., 131, 156–178, 1977.
L'Heureux, I.: Oscillatory zoning in plagioclase: thermal effects, Physica A, 239, 137–146, 1997.
Majidi, J.: Sabzevar Geological Map and Report, 1:100 000. Geological Survey and Mining Exploration of Iran, 1999.
Maniar, P. D. and Piccoli, P. M.: Tectonic discrimination of granitoids. Geol. Soc. Am. Bull., 101, 635–643, 1989.
Martel, C., Pichavant, M., Holtz, F., Scaillet, B., Bourdier, J. L. and Traineau, H.: Effects of fO2 and H2O on andesite phase relation between 2 and 4 kbar, J. Geophys. Res., 104, 29453–29470, 1999.
Martin, H., Smithies, R. H., Rapp, R., Moyen, J. F., and Champion, D.: An overview of adakite, tonalite–trondhjemite–granodiorite (TTG), and sanukitoid: relationships and some implications for crustal Evolution, Lithos, 79, 1–24, 2005.
Mohamadi Gorchi, E., Ghorbani, G., and Shafaii Moghadam, H.: The Origin of high-SiO2 adakites in southwestern part of the Sabzevar ophiolites, 1st National Conferences on the Iranian Plateau Geology, 2013 (in Persian).
Motaghi, K., Tatar, M., Shomali, Z. H., Kaviani, K., and Priestley, K.: High resolution image of uppermost mantle beneath NE Iran continental collision zone, Phys. Earth Planet. In., 208, 38–49, 2012.
Müntener, O., Kelemen, P. B., and Grove, T. L.: The role of H2O during the crystallization of primitive arc magmas under uppermost mantle conditions and genesis of igneous pyroxenites: an experimental study, Contrib. Mineral. Petrol., 141, 643–658, 2001.
Murphy, J. B., Blais, S. A., Tubrett, M., McNeil, D., and Middleton, M.: Microchemistry of amphiboles near the roof of a mafic magma chamber: Insights into high level melt evolution, Lithos, 148, 162–175, 2012.
Noghreyan, M. K.: Evolution geochimique, mineralogique, et structurale d'un edifice ophiolitique singulier: Le massif de Sabzevar (Partie Central), NE d'Iran. These Sci, Univ. de Nancy I, France, 239 pp., 1982.
O'Neill, H. S. C. and Pownceby, M. L.: Thermodynamic data from redox reactions at high temperatures, I. An experimental and theoretical assessment of the electrochemical method using stabilized zirconia electrolytes, with revised values for the Fe-"FeO", Co-CoO, Ni-NiO, and Cu-Cu2O oxygen buffers, and new data for the W-WO2 buffer, Contrib. Mineral. Petrol., 114, 296–314, 1993.
Pearce, T. H. and Kolisnik, A. M.: Observations of plagioclase zoning using interference imaging, Earth-Sci. Rev., 29, 9–26, 1990.
Petford, N. and Atherton, M.: Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru, J. Petrol., 37, 1491–1521, 1996.
Putirka, K. D.: Thermometers and barometers for volcanic systems, in: Minerals, inclusions and volcanic processes, edited by: Putrika, K. and Tepley, F., Rev. Mineral. Geochem., 69, 61–120, 2008.
Putirka, K. D., Mikaelian, Ryerson, H., F., and Shaw, H.: New clinopyroxene-liquid thermobarometers for mafic, evolved, and volatile-bearing lava compositions, with applications to lavas from Tibet and the Snake River Plain, Idaho, Am. Mineral., 88, 1542–1554, 2003.
Ramos, F. C., Wolff, J. A., and Tollstrup, D. L.: Sr isotope disequilibrium in Columbia River flood basalts: evidences for rapid shallow-level open-system processes, Geology, 33, 457–460, 2005.
Reilinger, R., McClusky, S., Vernant, P., Lawrence, S., Semih Ergintav, S., Cakmak, R., Haluk Ozener, H., Kadirov, F., Guliev, I., Stepanyan, R., Nadariya, M., Hahubia, G., Mahmoud, S., Sakr, K., ArRajehi, A., Paradissis, D., Al-Aydrus, A., Prilepin, M., Guseva, T., Evren, E., Dmitrotsa, A., Filikov, S. V., Gomez, F., Riad Al-Ghazzi, R., and Karam, G.: GPS constraints on continental deformation in the Africa-Arabia-Eurasia continental collision zone and implications for the dynamics of plate interactions, J. Geophys. Res., 111, B05411, https://doi.org/10.1029/2005JB004051, 2006.
Ridolfi, F. and Renzulli, A.: Calcic amphiboles in calc-alkaline and alkaline magmas: thermobarometric and chemometric empirical equations valid up to 1130 °C and 2.2 GPa, Contrib. Mineral. Petrol., 163, 877–895, 2012.
Ridolfi, F., Renzulli, A., and Puerini, M.: Stability and chemical equilibrium of amphibole in calc-alkaline magmas: an overview, new thermobarometric formulations and application to subduction-related volcanoes, Contrib. Mineral. Petrol., 160, 45–66, 2010.
Rooney, T. O., Franceschi, P., and Hall, C. M.: Water-saturated magmas in the Panama Canal region: a precursor to adakite-like magma generation, Contrib. Mineral. Petrol., 161, 373–388, 2010.
Rossetti, F., Nasrabady, M., Vignaroli, G., Theye, T., Gerdes, A., Razavi, S. M. H., and Moin Vaziri, H.: Early Cretaceous migmatitic mafic granulites from the Sabzevar range (NE Iran): Implications for the closure of the Mesozoic peri-Tethyan oceans in central Iran, Terra Nova, 22, 26–34, 2010.
Rossetti, F., Nasrabady, M., Theye, T., Gerdes, A., Monié, P., Lucci, F., and Vignaroli, G.: Adakite differentiation and emplacement in a subduction channel: The late Paleocene Sabzevar magmatism (NE Iran), Geol. Soc .Am. Bull. 126, 317–343, 2014.
Peccerillo, R. and Taylor, S. R.: Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey, Contrib. Mineral. Petrol., 58, 63–81, 1976.
Salehinejad, H.: Petrological and geochemical investigation of subvolcanic domes of Bashtin area (SW of Sabzevar), MSc thesis, Shahrood University of Technology, Shahrood, Iran, 2008 (in Persian).
Shabanian, E., Acocella, V., Gioncada, A., Ghasemi, H. and Bellier, O.: Structural control on volcanism in intraplate post collisional settings: Late Cenozoic to Quaternary examples of Iran and Eastern Turkey. Tectonics, 31, 3013-3042, 2012.
Shafaii Moghadam, H. S., Whitechurch, H., Rahgoshay, M., and Monsef, I.: Significance of Nain-Baft ophiolitic belt (Iran): Short-lived, transtensional Cretaceous back-arc oceanic basins over the Tethyan subduction zone, C. R. Geosci., 341, 1016–1028, 2009.
Shafaii Moghadam, S. H., Zaki Khedr, M., Arai, S., Stern, R. J., Ghorbani, G., Tamura, A., and Ottley, C.: Arc-related harzburgite-dunite-chromitite complexes in the mantle section of the Sabzevar ophiolite, Iran: a model for formation of podiform chromitites, Gondwana Res., 27, 575–593, https://doi.org/10.1016/j.gr.2013.09.007, 2015.
Shojaat, B., Hassanipak, A. A., Mobasher, K., and Ghazi, A. M.: Petrology, geochemistry and tectonics of the Sabzevar ophiolite, North Center Iran, J. Asian Earth Sci., 21, 1053–1067, 2003.
Sisson, T. W. and Grove, T. L.: Experimental investigations of the role of H2O in calc-alkaline differentiation and subduction zone magmatism. Contrib. Mineral. Petrol., 113, 143–166, 1993.
Slaby, E. and Götze, J.: Feldspar crystallization under magma-mixing conditions shown by cathodoluminescence and geochemical modeling- a case study from the Karkonosze pluton (SW Poland), Mineral. Mag., 68, 561–577, 2004.
Spies, O., Lensch, G., and Mihem, A.: Geochemistry of the post-ophiolitic Tertiary volcanics between Sabzevar and Quchan (NE Iran), GSI, Report no. 51, 247–266, 1983.
Stampfli, G. M. and Borel, G. D.: A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrones, Earth Planet. Sc. Lett., 196, 17–33, 2002.
Stewart, D. C.: Crystal clots in calc-alkaline andesites as breakdown products of high-Al amphiboles, Contrib. Mineral. Petrol., 53, 195–204, 1975.
Sun, S.S. and McDonough, W. F.: Chemical and isotopic systematics of oceanic of basalts: implication for mantle composition and processes, in: Magmatism in oceanic basins, edited by: Saunders, A. D. and Norry, M. J., Geol. Soc. London, 42, 313–345, 1989.
Tepley, F. J., Davidson, J., Tilling, R. I., and Arth, J. G.: Magma mixing, recharge and eruptive histories recorded in plagioclase phenocrysts from El Chichón Volcano, Mexico, J. Petrol., 41, 1397–1411, 2000.
Troll, V. R. and Schmincke, H.-U.: Magma mixing and crustal recycling recorded in ternary feldspar from compositionally zoned peralkaline ignimbrite "A", Gran Canaria, Canary Islands, J. Petrol., 43, 243–270, 2002.
Troll, V. R., Donaldson, C. H., and Emeleus, C. H.: Pre-eruptive magma mixing in ash-flow deposites of the Tertisry Rum Igneous Centre, Scotland, Contrib. Mineral. Petrol., 147, 722–739, 2004.
Turner, S., Arnaud, N., Liu, J., Rogers, N., Hawkesworth, C., Harris, N., Kelley, S., van Calsteren, P., and Deng, W.: Post-collisional, shoshonitic volcanism on the Tibetean plateau: implications for convective thinning of the lithosphere and the source of ocean island basalts, J. Petrol., 37, 45–71, 1996.
Wang, Q., Wyman, D. A., Xu, J.-F., Zhao, Z. H., Jian, P., Xiong, X. L., Bao, Z. W., Li, C. F., and Bai, Z. H.: Petrogenesis of Cretaceous adakitic and shoshonitic igneous rocks in the Luzong area, Anhui Province (Eastern China): implications for geodynamics and Cu-Au mineralization, Lithos, 89, 424–446, 2006.
Wang, X. L., Shu, X. J., Xu, X., Tang, M., and Gaschnig, R.: Petrogenesis of the Early Cretaceous adakite-like porphyries and associated basaltic andesites in the eastern Jiangnan orogen, southern China, J. Asian Earth Sci., 61, 243–256, 2012.
