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Relevant bibliographies by topics / Granulite facies metamorphism

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Academic literature on the topic 'Granulite facies metamorphism'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 January 2023

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Journal articles on the topic "Granulite facies metamorphism"

1

ENGVIK, A. K., and B. BINGEN. "Granulite-facies metamorphism of the Palaeoproterozoic – early Palaeozoic gneiss domains of NE Mozambique, East African Orogen." Geological Magazine 154, no. 3 (2016): 491–515. http://dx.doi.org/10.1017/s0016756816000145.

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AbstractGranulite-facies metamorphism recorded in NE Mozambique is attributed to three main tectonothermal events, covering more than 1400 Ma from Palaeoproterozoic – early Palaeozoic time. (1) Usagaran–Ubendian high-grade metamorphism of Palaeoproterozoic age is documented in the Ponta Messuli Complex by Grt-Sil-Crd-bearing metapelites, estimated to pressure (P) 0.75 ± 0.08 GPa and temperature (T) 765 ± 96°C. The post-peak P-T path is characterized by decompression followed by near-isobaric cooling. (2) Irumidian medium- to high-pressure granulite-facies metamorphism is evident in the Unango

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Timmermann, Hilke, Rebecca A. Jamieson, Randall R. Parrish, and Nicholas G. Culshaw. "Coeval migmatites and granulites, Muskoka domain, southwestern Grenville Province, Ontario." Canadian Journal of Earth Sciences 39, no. 2 (2002): 239–58. http://dx.doi.org/10.1139/e01-076.

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We present new field observations and petrologic and geochronological data from the Muskoka domain in the southwestern Grenville Province of Ontario in an attempt to constrain the relationship between amphibolite-facies and granulite-facies gneisses in areas of transitional metamorphic grade, and to examine their implication for tectonometamorphic models for the Grenville Province of Ontario. The predominant medium-grained amphibolite-facies migmatitic orthogneisses of the Muskoka domain contain several generations of leucosome, some of which are related to southeast-directed extensional struc

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Campos, José C. S., Maurício A. Carneiro, and Miguel A. S. Basei. "U-Pb evidence for late Neoarchean crustal reworking in the Southern São Francisco Craton (Minas Gerais, Brazil)." Anais da Academia Brasileira de Ciências 75, no. 4 (2003): 497–511. http://dx.doi.org/10.1590/s0001-37652003000400008.

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The Passa Tempo Metamorphic Complex is one of several metamorphic complexes that form the Archean sialic crust of the southern São Francisco Craton. It encompasses hypersthene-bearing gneissic rocks, with subordinateNW- or EW-trending mafic-ultramafic bodies and granodioritic to alkali-granitic, weakly foliated, and light-colored granitoids. These granitoids are the product of generalized migmatization that followed granulite-facies metamorphism. To determine the ages of the granulite-facies metamorphism and granitoid genesis, we obtained U-Pb ages on zircon extracted from the mesosome and leu

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Dasgupta, Somnath, Pulak Sengupta, A. Mondal, and M. Fukuoka. "Mineral chemistry and reaction textures in metabasites from the Eastern Ghats belt, India and their implications." Mineralogical Magazine 57, no. 386 (1993): 113–20. http://dx.doi.org/10.1180/minmag.1993.057.386.11.

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AbstractThree types of mafic granulites, namely two pyroxene-plagioclase granutite (MG), two pyroxeneplagioclase-garnet granulite (GMG) and spinel-olivine-plagioclase-two pyroxene granulite (SMG) are exposed at Sunkarimetta, Eastern Ghats belt, India. The marie granulites exhibit a foliation concordant with that in associated granulite facies quartzofeldspathic gneisses. Textural characteristics and mineral chemical data suggest the following mineral reactions: olivine + plagioclase = spinel + orthopyroxene + clinopyroxene (SMG), orthopyroxene + plagioclase = garnet + quartz (GMG), clinopyroxe

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PRAKASH, DIVYA, DEEPAK, PRAVEEN CHANDRA SINGH, et al. "Reaction textures and metamorphic evolution of sapphirine–spinel-bearing and associated granulites from Diguva Sonaba, Eastern Ghats Mobile Belt, India." Geological Magazine 152, no. 2 (2014): 316–40. http://dx.doi.org/10.1017/s0016756814000399.

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AbstractThe Diguva Sonaba area (Vishakhapatnam district, Andhra Pradesh, South India) represents part of the granulite-facies terrain of the Eastern Ghats Mobile Belt. The Precambrian metamorphic rocks of the area predominantly consist of mafic granulite (±garnet), khondalite, leptynite (±garnet, biotite), charnockite, enderbite, calc-granulite, migmatic gneisses and sapphirine–spinel-bearing granulite. The latter rock type occurs as lenticular bodies in khondalite, leptynite and calc-granulite. Textural relations, such as corroded inclusions of biotite within garnet and orthopyroxene, resorbe

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BHATTACHARYA, S., RAJIB KAR, S. MISRA, and W. TEIXEIRA. "Early Archaean continental crust in the Eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite." Geological Magazine 138, no. 5 (2001): 609–18. http://dx.doi.org/10.1017/s0016756801005702.

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The Eastern Ghats granulite belt of India has traditionally been described as a Proterozoic mobile belt, with probable Archaean protoliths. However, recent findings suggest that synkinematic development of granulites took place in a compressional tectonic regime and that granulite facies metamorphism resulted from crustal thickening. The field, petrological and geochemical studies of a charnockite massif of tonalitic to trondhjemitic composition, and associated rocks, document granulite facies metamorphism and dehydration partial melting of basic rocks at lower crustal depths, with garnet gran

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ROY, A. B., ALFRED KRÖNER, P. K. BHATTACHAYA, and SANJEEV RATHORE. "Metamorphic evolution and zircon geochronology of early Proterozoic granulites in the Aravalli Mountains of northwestern India." Geological Magazine 142, no. 3 (2005): 287–302. http://dx.doi.org/10.1017/s0016756805000804.

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Granulites including a charnockite suite, mafic granulites, pelitic granulites, metanorite dykes and their retrograde varieties occur as discontinuous shear zone-bounded bodies within the Archaean basement comprising a granite gneiss–amphibolite–metasedimentary rock association in the central part of the Aravalli Mountains, northwest India. The entire suite, named the Sandmata Complex, preserves a complex history of tectonothermal evolution. Except for their strongly foliated margins, the granulite bodies are largely massive. Partial melting in the ‘country rocks’ led to the development of mig

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Kepezhinskas, Nikita. "Fluid-induced metamorphism and anatexis of refractory Ni-Co-Cu sulphides in subduction-related rocks." E3S Web of Conferences 98 (2019): 08008. http://dx.doi.org/10.1051/e3sconf/20199808008.

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The role of metamorphism on refractory sulfides is not well constrained. Although experiments have displayed the effectiveness of high grade metamorphism, namely granulite facies metamorphism, on sulfide anatexis, its role in the presence of other variables is still poorly understood. Rocks from the Bay Islands Accretionary Complex in Honduras and the Ildeus-Lucha Complex in Russia exhibit extensive metamorphism. Sulfide mineralization is prolific in these rocks suggesting that metamorphism has played an important role in re-concentrating these sulfides during amphibolite and granulite facies

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Skublov, Sergey G., Aleksey V. Berezin, and Laysan I. Salimgaraeva. "Comment on Volodichev et al. Archean Zircons with Omphacite Inclusions from Eclogites of the Belomorian Province, Fennoscandian Shield: The First Finding. Minerals 2021, 11, 1029." Minerals 12, no. 2 (2022): 141. http://dx.doi.org/10.3390/min12020141.

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Volodichev et al. (Volodichev et al., 2021) reported on the first finding of omphacite (23%–25% Jd) inclusions in 2.68 Ga metamorphic zircons from Gridino eclogites and presented it as evidence for Archean eclogite-facies metamorphism in the Belomorian Mobile Belt. We believe that the Archean age of the garnets referred to by the above authors was estimated incorrectly. Our interpretation is that omphacite origin is related to Archean high-pressure granulite-facies metamorphism.

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Pan, Y., M. E. Fleet, and F. J. Longstaffe. "Melt-related metasomatism in mafic granulites of the Quetico subprovince, Ontario: constraints from O-Sr-Nd isotopic and fluid inclusion data." Canadian Journal of Earth Sciences 36, no. 9 (1999): 1449–62. http://dx.doi.org/10.1139/e99-041.

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Mafic granulites in the Archean Quetico subprovince, north of Manitouwadge, Ontario, occur as isolated lenses or discontinuous layers in spatial association with tonalitic leucosomes in metasedimentary rocks and exhibit concentric zoning from a biotite-rich margin to an orthopyroxene-rich outer zone and a clinopyroxene-rich central zone, with internal orthopyroxene-bearing leucosomes and, rarely, patches of relict amphibolites within the clinopyroxene-rich zone. Microstructural and microchemical evidence suggests that the mafic granulites formed from amphibolites by combined infiltration-diffu

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Dissertations / Theses on the topic "Granulite facies metamorphism"

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SUZUKI, Kazuhiro, Setsuo YOGO, and Masahiro ITO. "Cambrian granulite to upper amphibolite facies metamorphism of post-797 Ma sediments in Madagascar." Dept. of Earth and Planetary Sciences, Nagoya University, 1997. http://hdl.handle.net/2237/2837.

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Redler, Charlotte [Verfasser]. "Granulite facies metamorphism and partial melting processes in the Ivrea Zone, Northern Italy / Charlotte Redler." Mainz : Universitätsbibliothek Mainz, 2012. http://d-nb.info/1019231149/34.

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McStay, Jonathan Hugh. "Granulite-facies metamorphism, fluid buffering and partial melting in the Buffels River area of the Namaqualand metamorphic complex, South Africa." Doctoral thesis, University of Cape Town, 1991. http://hdl.handle.net/11427/18280.

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The Buffels River area of central Namaqualand comprises a sequence of Proterozoic volcano-sedimentary gneisses intruded by granitoid orthogneisses. This study concentrates on the mechanisms of granrilite-facies metamorphism in a small area of isofacial rocks. Particular emphasis is placed on the role of partial melting and the infiltration and buffering of metamorphic fluid is examined.

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Daczko, Nathan Robert. "The Structural and Metamorphic evolution of cretaceous high-P granulites, Fiordland, New Zealand." University of Sydney. Geosciences, 2002. http://hdl.handle.net/2123/822.

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Fiordland is located southwest of South Island of New Zealand. The field area of this thesis is in northern Fiordland, at the boundary of pristine arc rocks (Median Tectonic Zone) and a belt of Paleozoic paragneisses and orthogneisses of variable age that represent the metamorphosed paleo-Pacific Gondwana margin.

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Zulbati, Petrillo Fabio. "P-T-fluid conditions of an end-Archaean granulite-facies metamorphism in the Vestfold Hills, East Antartica." Thesis, University of Edinburgh, 2002. http://hdl.handle.net/1842/13259.

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Guilmette, Carl. "High-P Granulite facies metamorphism from the tibetan plateau and the Himalaya: Metamorphic history and geochemistry of lower crustal and early subduction metamorphic rocks." Thesis, Université Laval, 2010. http://www.theses.ulaval.ca/2010/27631/27631.pdf.

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Garlick, Sarah R. "Granulite- to amphibolite-facies metamorphism and penetrative deformation in a disrupted ophiolite, Kangaroo Mountain area, Klamath Mountains, California a deep view into the basement of an accreted, oceanic island arc /." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1317326781&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Krauss, Jason B. "High-pressure (HP), granulite-facies thrusting in a thick-skinned thrust system in the eastern Grenville Province, central Labrador /." Internet access available to MUN users only, 2002. http://collections.mun.ca/u?/theses,42716.

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Rocha, Brenda Chung da. "Evolução metamórfica dos metassedimentos da Nappe Lima Duarte e rochas associadas do Complexo Mantiqueira, sul da Faixa Brasília (MG)." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-27072011-180118/.

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A Nappe Lima Duarte está situada no sudeste do Orógeno Brasília. É constituída por paragnaisses migmatíticos com granada, sillimanita, biotita e muscovita, e ortoquartzitos grossos, com intercalações esparsas de gnaisses calciossilicáticos e de anfibolitos. O Complexo Mantiqueira, infraestrutura alóctone da nappe, ocorre na forma de lascas tectonicamente imbricadas na mesma. É constituído por ortognaisses migmatíticos e polimetamórficos, tipo TTG, com intercalações de rochas metabásicas granulíticas, na forma de enclaves máficos alongados e boudins, geralmente concordantes com a foliação princ

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Müller, Mario. "The Mavuradonha layered complex neoproterozoic emplacement and Pan-African granulite facies metamorphism in the Zambezi Allochthonous Terrane of the Mt. Darwin Area, Zambezi belt, NE-Zimbabwe /." [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=971950113.

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Books on the topic "Granulite facies metamorphism"

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Nijland, Teunis Gerrit. The Bamble amphibolite to granulite facies transitions zone, Norway. Faculteit Aardwetenschappen der Rijksuniversiteit Utrecht, 1993.

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Peterson, Jonathan William. Experimental investigation on the melting of biottle-quartz-feldspar assemblages and its potential role in granulite facies metamorphism. 1989.

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Book chapters on the topic "Granulite facies metamorphism"

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Newton, R. C. "Fluids of Granulite Facies Metamorphism." In Advances in Physical Geochemistry. Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4896-5_2.

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Schiøtte, L., and D. Bridgwater. "Multi Stage Late Archaean Granulite Facies Metamorphism in Northern Labrador, Canada." In Granulites and Crustal Evolution. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2055-2_9.

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3

Hensen, B. J., and S. L. Harley. "Graphical analysis of P—T—X relations in granulite facies metapelites." In High-temperature Metamorphism and Crustal Anatexis. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-3929-6_2.

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Rumble, D., C. P. Chamberlain, P. K. Zeitler, and B. Barreiro. "Hydrothermal Graphite Veins and Acadian Granulite Facies Metamorphism, New Hampshire, USA." In Fluid Movements — Element Transport and the Composition of the Deep Crust. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_11.

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Schumacher, Renate, Volker Schenk, Peter Raase, and P. W. Vitanage. "Granulite facies metamorphism of metabasic and intermediate rocks in the Highland Series of Sri Lanka." In High-temperature Metamorphism and Crustal Anatexis. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-3929-6_10.

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Vernon, R. H., G. L. Clarke, and W. J. Collins. "Local, mid-crustal granulite facies metamorphism and melting: an example in the Mount Stafford area, central Australia." In High-temperature Metamorphism and Crustal Anatexis. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-3929-6_11.

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Harley, S. L., and B. J. Hensen. "Archaean and Proterozoic high-grade terranes of East Antarctica (40–80°E): a case study of diversity in granulite facies metamorphism." In High-temperature Metamorphism and Crustal Anatexis. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-3929-6_12.

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Newton, Robert C. "Temperature, Pressure and Metamorphic Fluid Regimes in the Amphibolite Facies to Granulite Facies Transition Zones." In The Deep Proterozoic Crust in the North Atlantic Provinces. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_6.

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Touret, J. L. R., and T. G. Nijland. "Prograde, Peak and Retrograde Metamorphic Fluids and Associated Metasomatism in Upper Amphibolite to Granulite Facies Transition Zones." In Lecture Notes in Earth System Sciences. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-28394-9_11.

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Sengupta, Sudipta. "A Comprehensive Study of the Structural Geology of the Schirmacher Hills." In Geoscientific Investigations From the Indian Antarctic Program. IGI Global, 2022. http://dx.doi.org/10.4018/978-1-6684-4078-0.ch003.

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The Precambrian basement of the Schirmacher Hills records multiple episodes of deformation, metamorphism, migmatization, and emplacement of successive generations of mafic and felsic bodies. The earliest tectono-thermal event (D1/M1), preserved in some mafic and ultramafic enclaves, indicates deformation at great crustal depth. The mineralogical assemblage of these enclaves indicates early high temperature (900o C) and high-pressure (10 Kbar) granulite facies conditions. The second tectono-thermal event also showed deformation under granulite facies metamorphism (D2/M2) under 800-850oC and 8 Kbar. The third group of events (D3/M3) is the most dominant in this region and involved deformation under amphibolite facies conditions with synchronous emplacement of granites and mafic dykes and culminated in regional thrusting, producing a regional inversion where the granulates were emplaced over the amphibolite facies rocks. The later events created upright folds and vertical shear zones under amphibolite facies conditions.

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Conference papers on the topic "Granulite facies metamorphism"

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Weimer, Joshua J., and Benjamin W. Hallett. "CHARACTERIZING GRANULITE FACIES METAMORPHISM OF THE PICURIS OROGENY, TAOS RANGE, NEW MEXICO." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348215.

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Yakymchuk, Chris, Christopher L. Kirkland, Julie Hollis, Jillian L. Kendrick, Nicolas J. Gardiner, and Kristoffer Szilas. "ACCRETION OR STAGNATION? ARCHEAN GRANULITE-FACIES METAMORPHISM IN THE AKIA TERRANE, WEST GREENLAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334306.

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Cutts, Kathryn, Lucas Eduardo Araujo, Talitta Nunes Manoel, Monica Heilbron, and Claudio Valeriano. "Metamorphic evolution of the Juiz de Fora Complex: Rhyacian and Ediacaran granulite facies metamorphism records two supercontinent amalgamation events." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7390.

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Schwartz, Joshua J., John A. Wiesenfeld, and Jade Star Lackey. "CRETACEOUS BATHOLITH CONSTRUCTION DURING EPISODIC GARNET GRANULITE-FACIES METAMORPHISM IN THE SAN GABRIEL MOUNTAINS, SOUTHERN CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274738.

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Yoshida, Kenta, Sota Niki, Hikaru Sawada, et al. "Simultaneous P-T-t estimation of ultrahigh-temperature high-pressure granulite facies metamorphism recorded in titanite." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.4227.

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Du, Kaiyang, and Hao Cheng. "Long-Lived Granulite-Facies Metamorphism in the North China Craton Constrained by Combined Garnet and Zircon Geochronology." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.614.

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Walters, Jesse, Steven Spreitzer, Edward S. Grew, et al. "CAMBRIAN GRANULITE-FACIES METAMORPHISM OF THE LARSEMANN HILLS, PRYDZ BAY, ANTARCTICA: USING THERMODYNAMIC MODELING TO INFORM MONAZITE PETROCHRONOLOGY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302124.

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Adsit, Aaron, Matthew Carter, William O. Nachlas, and Earl R. Verbeek. "INTERDIFFUSION OF ZN-MN-FE IN PYROXENE, SPINEL, AND GARNET DURING GRENVILLE GRANULITE FACIES METAMORPHISM AT STERLING HILL, NJ." In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-375208.

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Baker, Lindsey K., Sara V. Stotter, Christopher L. Andronicos, and Christopher G. Daniel. "TESTING MODELS OF MAZATZAL (1650 MA) AND PICURIS AGE (1400 MA) METAMORPHISM IN NEAR–GRANULITE FACIES METAMORPHIC ROCKS OF THE NORTHERN TAOS RANGE, NEW MEXICO." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320328.

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Southworth, Scott, John N. Aleinikoff, and Thomas A. Johnson. "SEDIMENTATION, GRANULITE-FACIES METAMORPHISM, DEFORMATION, AND IGNEOUS INTRUSIONS DEFINE MULTIPLE TECTONIC EVENTS ASSOCIATED WITH THE OTTAWAN-RIGOLET OROGENIES IN PROTEROZOIC ROCKS OF THE APPALACHIAN BLUE RIDGE." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-343303.

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