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Relevant bibliographies by topics / UHP/HP metamorphism

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Academic literature on the topic 'UHP/HP metamorphism'

Author: Grafiati

Published: 4 June 2021

Last updated: 2 February 2022

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Journal articles on the topic "UHP/HP metamorphism"

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KROHE, A., and E. MPOSKOS. "Structural evolution and exhumation history of the Rhodope UHP-HP metamorphic province (Northern Greece)." Bulletin of the Geological Society of Greece 34, no. 1 (January 1, 2001): 75. http://dx.doi.org/10.12681/bgsg.16945.

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Middle/Early Alpine UHP-HP domain of the Rhodope (N'Greece) show pressures >3.6 Gpa. UHP-HP rocks have been emplaced in three major tectonic pulses: (i) At about 65->48 Ma the UHP Kimi Complex was exhumed at the surface representing the structurally uppermost UHP unit, (ii) Between > 42-30 Ma, the Sidironero, Kardamos and Kechros Complexes were exhumed underlying the Kimi Complex in the central and eastern Rhodope, respectively. They are characterized by HP-metamorphism (some parts by UHP-metamorphism), isothermal decompression and probably rapid exhumation. Exhumation tectonics involves deep level thrusting, synchronous high level extension, and successive post-thrusting extension. The post-thrusting Xanthi low angle normal detachment system extending over a distance of 100 km, from central Rhodope to eastern Rhodope, is interpreted to be responsible for a decrease in recent crustal thickness of about 20 km from central to eastern Rhodope. Lutetian (c. 48-43Ma) to Oligocene marine basins transgressed atop the Kimi Complex representing the upper plate of all detachment generations, (iii) The third exhumation pulse between 26 to 8 Ma, exhumed the Thasos/Pangeon metamorphic core complexes representing the structurally lowermost tectonic units of the Rhodope domain. Their exhumation occurred by displacements on the Miocene Strymon and Thasos detachment systems.

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REBAY, GISELLA, DAVIDE ZANONI, ANTONIO LANGONE, PIETRO LUONI, MASSIMO TIEPOLO, and MARIA IOLE SPALLA. "Dating of ultramafic rocks from the Western Alps ophiolites discloses Late Cretaceous subduction ages in the Zermatt-Saas Zone." Geological Magazine 155, no. 2 (May 3, 2017): 298–315. http://dx.doi.org/10.1017/s0016756817000334.

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AbstractThe Zermatt-Saas Zone was part of the Middle to Late Jurassic Tethyan lithosphere that underwent oceanic metamorphism during Mesozoic time and subduction during Eocene time (HP to UHP metamorphism). In upper Valtournanche, serpentinite, metarodingite and eclogite record a dominant S2 foliation that developed under 2.5±0.3 GPa and 600±20°C during Alpine subduction. Serpentinites contain clinopyroxene and rare zircon porphyroclasts. Clinopyroxene porphyroclasts show fringes within S2 with similar compositions to that of grains defining S2. Zircon cores show zoning typical of magmatic growth and thin fringes parallel to the S2 foliation. These features indicate crystallization of clinopyroxene and zircon fringes during HP syn-D2 metamorphism, related to the Alpine subduction. The U–Pb zircon dates for cores and fringes reveal crystallization at 165±3.2 Ma and 65.5±5.6 Ma, respectively. The Middle Jurassic dates are in agreement with the known ages for the oceanic accretion of the Tethyan lithosphere. The Late Cretaceaous - Paleocene dates suggest that the Zermatt-Saas Zone experienced high-pressure to ultra-high-pressure (HP–UHP) metamorphism at c. 16 Ma earlier than previously reported. This result is in agreement with the evidence that in the Western Alps the continental Sesia-Lanzo Zone reached the subduction climax at least from 70 Ma and was exhumed during ongoing oceanic subduction. Our results are further evidence that the Zermatt-Saas ophiolites diachronically recorded heterogeneous HP–UHP metamorphism.

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Holmberg, Johanna, Michał Bukała, Pauline Jeanneret, Iwona Klonowska, and Jarosław Majka. "Decompressional equilibration of the Midsund granulite from Otrøy, Western Gneiss Region, Norway." Geologica Carpathica 70, no. 6 (December 1, 2019): 471–82. http://dx.doi.org/10.2478/geoca-2019-0027.

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Abstract The Western Gneiss Region (WGR) of the Scandinavian Caledonides is an archetypal terrain for high-pressure (HP) and ultrahigh-pressure (UHP) metamorphism. However, the vast majority of lithologies occurring there bear no, or only limited, evidence for HP or UHP metamorphism. The studied Midsund HP granulite occurs on the island of Otrøy, a locality known for the occurrence of the UHP eclogites and mantle-derived, garnet-bearing ultramafics. The Midsund granulite consists of plagioclase, garnet, clinopyroxene, relict phengitic mica, biotite, rutile, quartz, amphibole, ilmenite and titanite, among the most prominent phases. Applied thermodynamic modelling in the NCKFMMnASHT system resulted in a pressure–temperature (P–T) pseudosection that provides an intersection of compositional isopleths of XMg (Mg/Mg+Fe) in garnet, albite in plagioclase and XNa (Na/Na+Ca) in clinopyroxene in the stability field of melt + plagioclase + garnet + clinopyroxene + amphibole + ilmenite. The obtained thermodynamic model yields P–T conditions of 1.32–1.45 GPa and 875–970 °C. The relatively high P–T recorded by the Midsund granulite may be explained as an effect of equilibration due to exhumation from HP (presumably UHP) conditions followed by a period of stagnation under HT at lower-to-medium crustal level. The latter seems to be a more widespread phenomenon in the WGR than previously thought and may well explain commonly calculated pressure contrasts between neighboring lithologies in the WGR and other HP–UHP terranes worldwide.

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Liou, J. G., W. G. Ernst, S. G. Song, and B. M. Jahn. "Tectonics and HP–UHP metamorphism of northern Tibet – Preface." Journal of Asian Earth Sciences 35, no. 3-4 (July 2009): 191–98. http://dx.doi.org/10.1016/j.jseaes.2009.03.001.

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Zhang, Lifei, Zeming Zhang, Hans-Peter Schertl, and Chunjing Wei. "HP–UHP metamorphism and tectonic evolution of orogenic belts: introduction." Geological Society, London, Special Publications 474, no. 1 (2019): 1–4. http://dx.doi.org/10.1144/sp474.15.

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Asano, Kouhei, Katsuyoshi Michibayashi, and Tomohiro Takebayashi. "Rheological Contrast between Quartz and Coesite Generates Strain Localization in Deeply Subducted Continental Crust." Minerals 11, no. 8 (August 4, 2021): 842. http://dx.doi.org/10.3390/min11080842.

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Deformation microstructures of peak metamorphic conditions in ultrahigh-pressure (UHP) metamorphic rocks constrain the rheological behavior of deeply subducted crustal material within a subduction channel. However, studies of such rocks are limited by the overprinting effects of retrograde metamorphism during exhumation. Here, we present the deformation microstructures and crystallographic-preferred orientation data of minerals in UHP rocks from the Dabie–Shan to study the rheological behavior of deeply subducted continental material under UHP conditions. The studied samples preserve deformation microstructures that formed under UHP conditions and can be distinguished into two types: high-strain mafic–ultramafic samples (eclogite and garnet-clinopyroxenite) and low-strain felsic samples (jadeite quartzite). This distinction suggests that felsic rocks are less strained than mafic–ultramafic rocks under UHP conditions. We argue that the phase transition from quartz to coesite in the felsic rocks may explain the microstructural differences between the studied mafic–ultramafic and felsic rock samples. The presence of coesite, which has a higher strength than quartz, may result in an increase in the bulk strength of felsic rocks, leading to strain localization in nearby mafic–ultramafic rocks. The formation of shear zones associated with strain localization under HP/UHP conditions can induce the detachment of subducted crustal material from subducting lithosphere, which is a prerequisite for the exhumation of UHP rocks. These findings suggest that coesite has an important influence on the rheological behavior of crustal material that is subducted to coesite-stable depths.

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Hart, Emma, Craig Storey, Emilie Bruand, Hans-Peter Schertl, and Bruce D. Alexander. "Mineral inclusions in rutile: A novel recorder of HP-UHP metamorphism." Earth and Planetary Science Letters 446 (July 2016): 137–48. http://dx.doi.org/10.1016/j.epsl.2016.04.035.

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Kirst, Frederik, Sascha Sandmann, Thorsten Nagel, Nikolaus Froitzheim, and Marian Janák. "Tectonic evolution of the southeastern part of the Pohorje Mountains (Eastern Alps, Slovenia)." Geologica Carpathica 61, no. 6 (December 1, 2010): 451–61. http://dx.doi.org/10.2478/v10096-010-0027-y.

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Tectonic evolution of the southeastern part of the Pohorje Mountains (Eastern Alps, Slovenia)Field relations and deformation structures in the southeastern part of the Pohorje Mountains constrain the tectonic evolution of the Austroalpine high-pressure/ultrahigh pressure (HP/UHP) terrane. The Slovenska Bistrica Ultramafic Complex (SBUC) forms a large (ca. 8 × 1 km size) body of serpentinized harzburgite and dunite including minor garnet peridotite and is associated with partly amphibolitized eclogite bodies. The SBUC occurs in the core of an isoclinal, recumbent, northward closing antiform and is mantled by metasedimentary rocks, mostly gneisses and a few marbles, including isolated eclogite/amphibolite lenses. Before this folding, the SBUC formed the deepest part of the exposed terrane. We interpret the SBUC to be derived from near-MOHO, uppermost mantle which was intruded by gabbros in the subsurface of a Permian rift zone. During Cretaceous intracontinental subduction, the SBUC was most likely part of the footwall plate which experienced HP to UHP metamorphism and was folded during exhumation. In the Miocene, the Pohorje Pluton intruded and, subsequently, the metamorphic rocks together with the pluton were deformed probably due to east-west extension and contemporaneous north-south shortening, thus forming an antiformal metamorphic core complex.

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Chen, Zhen-Yu, Li-Fei Zhang, Zeng Lü, and Jin-Xue Du. "Episodic Fluid Action in Chinese Southwestern Tianshan HP/UHP Metamorphic Belt: Evidence from U–Pb Dating of Zircon in Vein and Host Eclogite." Minerals 9, no. 12 (November 25, 2019): 727. http://dx.doi.org/10.3390/min9120727.

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Fluid plays a key role in metamorphism and magmatism in subduction zones. Veins in high-pressure (HP) to ultrahigh-pressure (UHP) rocks are the products of fluid–rock interactions and can thus provide important constraints on fluid processes in subduction zones. In this study, we present an integrated study of zircon in situ U–Pb dating, trace element and mineral inclusion analysis for a complex vein and its host eclogite in the southwestern Tianshan UHP terrane, aiming to decipher the episodic fluid action during slab subduction and exhumation. Both zircon in eclogite and vein have euhedral, prismatic morphology similar to those crystallized from metamorphic fluid. Zircon in eclogite shows core–rim structures with distinct bounds and mineral inclusions. Zircon in the vein shows sector zoning or weak zoning, with bright rims around most zircon grains, which suggests recrystallization of the zircon crystals after their formation and multiple evolution of the vein. Eclogite zircon rims yield a weighted mean of 311 ± 3 Ma and cores yield a range from 413 ± 4 to 2326 ± 18 Ma, respectively. Vein zircon yields four groups of age (~355 Ma, ~337 Ma, ~315 Ma, and ~283 Ma), which date four episodes of fluid flow involving zircon growth. The first two groups of age may represent prograde epidote–amphibolite facies and amphibolite/blueschist facies metamorphism stage, respectively. The third group is similar to that of eclogite zircon rims, which is thought to date the eclogitic facie metamorphism (320–305 Ma), and the fourth group dates a later retrograde metamorphism after greenschist facies. The vein-forming fluid system was supposed to be an open system indicated by trace element of vein zircon and mineral assemblage of the vein. The coexistence of rutile, zircon, and garnet in prograde vein and the heavy rare earth elements (HREE) enrichment characteristic of vein zircon suggest that the vein-forming fluid are enriched in high field strength elements (HFSE) and HREE, and such fluid could be formed under low P–T conditions.

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Brueckner, H. K. "Dunk, Dunkless and Re-dunk Tectonics: A Model for Metamorphism, Lack of Metamorphism, and Repeated Metamorphism of HP/UHP Terranes." International Geology Review 48, no. 11 (November 2006): 978–95. http://dx.doi.org/10.2747/0020-6814.48.11.978.

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Dissertations / Theses on the topic "UHP/HP metamorphism"

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Xiao, Yilin. "Fluid histories during HP and UHP metamorphism in Dabie Shan, China constraints from trace elements, fluid inclusions, and stable isotopes /." [S.l.] : [s.n.], 2000. http://webdoc.sub.gwdg.de/diss/2001/xiao/diss.pdf.

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Tan, Zhou. "P-T-deformation-time evolution of the Akeyasi HP/UHP complex (SW-Tianshan, China) and implications for subduction dynamics." Thesis, Sorbonne université, 2018. http://www.theses.fr/2018SORUS185/document.

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Cette étude vise à caractériser des fragments clés d’une interface de subduction fossile affleurant dans la Ceinture Métamorphique du Sud-Tianshan (Chine). Nous étudions les processus de subduction au travers de la profondeur critique de ~80 km, au-delà de laquelle la géophysique et les modèles prévoient un changement du couplage mécanique, et les roches océaniques ne sont normalement pas exhumées. Ce travail s’intéresse au Complexe Métamorphique Akeyazi (AMC), un épais empilement de roches métavolcanoclastiques enveloppant des écailles éclogitiques, exposé sur ~30 km dans la vallée de Kebuerte, et préservant de nombreuses reliques de coésites. L’étude structurale révèle que l’AMC est un dôme métamorphique consistant de plusieurs nappes cohérentes d’ampleur kilométrique avec des histoire P-T-t-d distinctes. 4 unités sur 6, i.e. UH (2.75 GPa/480-560°C), EB (2.1/505), MU (1.45/485) et GT (>0.7-1.0/470-520) ont été subduites à des profondeurs de ~85, 65, 45 et 30 km respectivement. La déformation rétrograde des unités, liée à leur exhumation, est caractérisée par des bandes de cisaillement top vers le Nord au faciès schiste bleu. Le pic d’enfouissement de ces unités a eu lieu à 320±1, 332±2, 359±2 et 280-310 Ma pour les unités UH, EB, MU et schiste vert, indiquant plusieurs courts épisodes de détachement de matériel de la plaque plongeante. L’évolution tectono-métamorphique de ~12 à 5-7°C/km au cours du temps peut refléter le refroidissement progressif de la subduction. La juxtaposition et l’exhumation à 1-3 mm/an de ces 4 unités à des profondeurs crustales a eu lieu autour de 290-300 Ma
This study attempts to characterize key fossil fragments of material equilibrated along subduction plate boundary, now exposed in Chinese SW-Tianshan Metamorphic Belt (STMB). We herein elucidate some subduction zone processes across a critical depth range of ~80km, beyond which geophysicist and modeler infer a change in mechanical coupling and oceanic rocks are usually not recovered. It focuses on an unusually thick pile of HP/UHP metavolcanoclastics, wrapping eclogite slices and preserving pervasive coesite relics, along a ~30km-long transect across the Akeyazi metamorphic complex (AMC) in the Kebuerte valley. Structural studies reveal the current geometry of the AMC is a metamorphic dome with evidence of internal nappe stacking and should be subdivided into several coherent, km-scale tectonic units with distinct P-T-time-deformation histories. At least 4 of 6 sub-units identified here, i.e., the UH (2.75 GPa/480-560°C), EB (2.1/505), MU (1.45/485) and GT units (>0.7-1.0/470-520) were subducted and buried to depths of ~85, 65, 45 and 30 km respectively. Deformation following EC/BS-EC peak burial is marked by pervasive BS facies exhumation-related shear senses with a top to North component. Radiometric constraints yield peak burial ages of 320±1, 332±2, 359±2 and 280-310 Ma, respectively, for the UH, EB, MU and GS facies units, indicating several short-lived detachment episodes of material from the downgoing plate. The tectono-metamorphic evolution from ~12 to 5-7°C/km with time may reflect progressive cooling of the subduction system. Juxtaposition & exhumation of those 4 units to mid-crustal depth, at rates on the order of 1-3 mm/yr, was accomplished around 290-300Ma

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TEDESCHI, Mahyra. "Geodynamic evolution of the Southern Brasilia orogen, SE Brazil: new petrochronological insights from UHT and HP metamorphic rocks." reponame:Repositório Institucional da CPRM, 2018. http://rigeo.cprm.gov.br/jspui/handle/doc/19382.

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Albrecht, Nina [Verfasser], Gerhard [Akademischer Betreuer] [Gutachter] Wörner, and Andreas [Gutachter] Pack. "Metamorphic fluids at extreme pressure conditions and their significance for element transfer in subduction zones : A multidisciplinary study on metamorphic veins in UHP/HP eclogites from Dabieshan, China / Nina Albrecht ; Gutachter: Gerhard Wörner, Andreas Pack ; Betreuer: Gerhard Wörner." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2017. http://d-nb.info/1132717515/34.

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Xiao, Yilin. "Fluid Histories During HP and UHP Metamorphism in Dabie Shan, China: Constraints from Trace Elements, Fluid Inclusions, and Stable Isotopes." Doctoral thesis, 2001. http://hdl.handle.net/11858/00-1735-0000-0006-B257-5.

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Xiao, Yilin [Verfasser]. "Fluid histories during HP and UHP metamorphism in Dabie Shan, China : constraints from trace elements, fluid inclusions, and stable isotopes / vorgelegt von Yilin Xiao." 2000. http://d-nb.info/961823224/34.

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Albrecht, Nina. "Metamorphic fluids at extreme pressure conditions and their significance for element transfer in subduction zones." Doctoral thesis, 2017. http://hdl.handle.net/11858/00-1735-0000-0023-3E42-C.

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Book chapters on the topic "UHP/HP metamorphism"

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Krogh, E. J., and D. A. Carswell. "HP and UHP eclogites and garnet peridotites in the Scandinavian Caledonides." In Ultrahigh Pressure Metamorphism, 244–98. Cambridge University Press, 1995. http://dx.doi.org/10.1017/cbo9780511573088.009.

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Yang, Jingsui, Zhiqin Xu, Paul T. Robinson, Jianxin Zhang, Zeming Zhang, Fulai Liu, and Cailai Wu. "HP–UHP Metamorphic Belts in the Eastern Tethyan Orogenic System in China." In Ultrahigh-Pressure Metamorphism, 459–99. Elsevier, 2011. http://dx.doi.org/10.1016/b978-0-12-385144-4.00014-x.

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Fedkin, Valentin V., Theodore D. Burlick, Mary L. Leech, Andrey A. Shchipansky, Peter M. Valizer, and W. G. Ernst. "Petrotectonic origin of mafic eclogites from the Maksyutov subduction complex, south Ural Mountains, Russia." In Plate Tectonics, Ophiolites, and Societal Significance of Geology: A Celebration of the Career of Eldridge Moores. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2552(09).

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ABSTRACT The Maksyutov complex is a mid- to late-Paleozoic high- to ultrahigh-pressure (HP-UHP) eclogite-bearing subduction zone terrane in the south Ural Mountains. Previous reports of radial fractures emanating from quartz inclusions in garnet, omphacite, and glaucophane, cuboid graphite pseudomorphs after matrix diamond, and microdiamond aggregates preserved in garnet identified by Raman spectroscopy indicate that parts of the complex were subjected to physical conditions of ∼600 °C and >2.8 GPa for coesite-bearing rocks, and >3.2 GPa for diamond-bearing rocks. Peak UHP eclogite-facies metamorphism took place at ca. 385 Ma, and rocks were exhumed through retrograde blueschist-facies conditions by ca. 360 Ma. Bulk analyses of 18 rocks reflect the presence of mid-oceanic-ridge basalt (MORB), oceanic-island basalt (OIB), and island-arc tholeiite (IAT) basaltic and andesitic series plus their metasomatized equivalents. To more fully constrain the petrotectonic evolution of the complex, we computed isochemical phase equilibria models for representative metabasites in the system Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2 based on our new bulk-rock X-ray fluorescence (XRF) data. Both conventional Fe-Mg exchange thermometry and phase equilibrium modeling result in higher peak equilibrium temperatures than were previously reported for the complex. Pseudosection analysis provides minimum P-T conditions of 650–675 °C and 2.4–2.6 GPa for peak assemblages of the least retrogressed Maksyutov eclogites, whereas Fe-Mg exchange thermometry yields temperatures of 750 ± 25 °C for a pressure of 2.5 GPa. We interpret our new P-T data to reflect a thermal maximum reached by the eclogites on their initial decompression-exhumation stage, that defines a metamorphic field gradient; the relict coesite and microdiamond aggregates previously reported testify to pressure maxima that define an earlier prograde subduction zone gradient. The eclogitic Maksyutov complex marks underflow of the paleo-Asian oceanic plate and does not represent subduction of the Siberian cratonal margin.

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Eide, E. A. "A model for the tectonic history of HP and UHPM regions in east central China." In Ultrahigh Pressure Metamorphism, 391–426. Cambridge University Press, 1995. http://dx.doi.org/10.1017/cbo9780511573088.012.

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Conference papers on the topic "UHP/HP metamorphism"

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Zhang, Lijuan, and Lifei Zhang. "Massive Production of Abiotic Methane during Subduction Zone HP-UHP Metamorphism in SW Tianshan, China." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3110.

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