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Dissertations / Theses on the topic 'Granulite facies metamorphism'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 January 2023

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Taylor, Jeanne. "The anatectic history of Archaean metasedimentary granulites from the Ancient Gneiss Complex, Swaziland." Thesis, Stellenbosch : Stellenbosch University, 2011. http://hdl.handle.net/10019.1/20311.

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Thesis (DSc)--Stellenbosch University, 2012<br>ENGLISH ABSTRACT: This study is an investigation of the anatectic history of high-grade paragneisses from the Ancient Gneiss Complex (AGC) in Swaziland. The work involved an integrated field, metamorphic, geochemical, geochronological and structural study of metasedimentary granulites from three separate, but spatially related areas of outcrop in south-central Swaziland, which were subjected to multiple high-grade partial melting events throughout the Meso- to Neoarchaean. The project has aimed to constrain the age(s) and conditions of metamo

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12

Baars, Franciscus Jacobus, and Franciscus Jacobus Baars. "Geologic and petrologic evidence for granulite facies partial melting in the Garies-Platbakkies supracrustal gneiss belt, Namaqualand metamorphic complex, South Africa." Master's thesis, University of Cape Town, 1990. http://hdl.handle.net/11427/23148.

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The Namaqua Province of southwestern Africa is comprised of a number of distinct tectonostratigraphic subprovinces and terranes, which have in common a 1100-1200Ma structural and metamorphic imprint. In the western Bushmanland Subprovince, E-Wtrending belts of supracrustal gneisses are intruded by and infolded with granitic gneisses of varying ages. A central zone of rocks metamorphosed in the granulite facies is bordered to the north and south by amphibolite facies rocks. A portion of the Garies-Platbakkies supracrustal gneiss belt has been mapped on a 1:15 000 scale. The supracrustal success

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13

Palamountain, Robert. "Metamorphic petrology of the Winnecke Domain, central Australia : P-T-t constraints on the granulite-to lower amphibolite-facies terrane /." Title page, table of contents and abstract, 1996. http://web4.library.adelaide.edu.au/theses/09SB/09sbp1541.pdf.

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14

St-Jean, J. Alger. "Evolution of the granulite-facies Hart-Jaune Terrane in the context of the Grenville of eastern Quebec : structural and metamorphic indicators of late-stage normal faulting." Thesis, McGill University, 1995. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=22809.

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The granulite-facies Hart-Jaune Terrane is the structurally lowermost tectonic assemblage in the Allochthonous Belt of the Grenville province exposed along the Manicouagan Reservoir transect in eastern Quebec.<br>The Hart-Jaune Terrane is composed of interbanded two-pyroxene/plagioclase mafic granulites and quartzofeldspathic gneisses, which are probably supracrustal, and of granulitic gabbros. Gneissic banding generally trends NNE with moderately steep southerly dips, and contains a SSW-plunging pyroxene mineral lineation that is parallel to the axes of intrafolial folds. These structures are

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15

Nicollet, Christian. "METABASITES GRANULITIQUES, ANORTHOSITES ET ROCHES ASSOCIEES DE LA CROUTE INFERIEURE - Exemples pris à Madagascar et dans le Massif Central français - ARGUMENTS EN FAVEUR D'UN METAMORPHISME ASSOCIE A L'EXTENSION LITHOSPHERIQUE." Phd thesis, Université Blaise Pascal - Clermont-Ferrand II, 1988. http://tel.archives-ouvertes.fr/tel-00787525.

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Ce travail regroupe un ensemble de chapitres traitant de différents aspects des granulites, en mettant l'accent sur les compositions basiques. Ces chapitres sont indépendants, mais sont reliés entre eux par des renvois de l'un à l'autre. La première approche pour l'étude des granulites est géochimique: il est montré, dans un article en collaboration avec Andriambololona D., que les éléments de transition, peu affectés par le métamorphisme, peuvent être utilisés pour caractériser les métabasites. La suite du travail est consacrée à une étude pétrologique des formations granulitiques de Madagasc

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16

Palamountain, R. "Metamorphic petrology of the Winneke domain, Central Australia: P-T-t constraints on the granulite to lower amphibole facies terrain." Thesis, 1996. http://hdl.handle.net/2440/97272.

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This item is only available electronically.<br>The Winnecke Gorge-Two Mile Bore region (Winnecke Domain) of the Arunta Block, central Australia, contains a highly condensed geological section from greenschist-facies Amadeus Basin cover sequences (Heavitree Quartzite and Bitter Springs Formation), through amphibolite-grade assemblages (Ankala gneiss), to granulite-facies mafic, felsic and calc-silicate lithologies (Strangways Metamorphic Complex). Juxtaposition of these blocks of widely varying metamorphic grade has been facilitated via the activation (and probable reactivation in many cases) o

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17

Müller, Mario [Verfasser]. "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 / Mario Müller." 2004. http://d-nb.info/971950113/34.

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18

Elsenheimer, Donald William. "Development and application of laser microprobe techniques for oxygen isotope analysis of silicates and, fluid/rock interaction during and after granulite-facies metamorphism, Highland Southwestern Complex, Sri Lanka." 1992. http://catalog.hathitrust.org/api/volumes/oclc/28654261.html.

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19

Brandt, Sönke. "Metamorphic evolution of ultrahigh-temperature granulite facies and upper amphibolite facies rocks of the Epupa Complex, NW Namibia." Doctoral thesis, 2003. https://nbn-resolving.org/urn:nbn:de:bvb:20-opus-10930.

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The high-grade metamorphic Epupa Complex (EC) of north-western Namibia constitutes the south-western margin of the Archean to Proterozoic Congo Craton. The north-eastern portion of the EC has been geochemically and petrologically investigated in order to reconstruct its tectono-metamorphic evolution. Two distinct metamorphic units have been recognized, which are separated by ductile shear zones: (1) Upper amphibolite facies rocks (Orue Unit) and (2) ultrahigh-temperature (UHT) granulite facies rocks (Epembe Unit). The rocks of the EC are transsected by a large anorthosite massif, the Kunene In

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20

Alessio, Kiara Louise. "The effects of high temperature metamorphic and melting processes on granulite-facies rocks." Thesis, 2019. http://hdl.handle.net/2440/122416.

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This thesis presents research on high-temperature metamorphic processes. A recent development in petrological modelling of granulite facies rocks is reintegration of melt generated and lost during metamorphism. The aim of melt reintegration is to create bulk compositions suitable for modelling prograde subsolidus evolution. Melt reintegration methodology was applied to a low-pressure granulite assemblage containing unambiguous textural evidence for subsolidus andalusite. Melt reintegration methodology resulted in a bulk composition that stabilised subsolidus and modally correct andalusite, pro

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21

Brandt, Sönke [Verfasser]. "Metamorphic evolution of ultrahigh-temperature granulite facies and upper amphibolite facies rocks of the Epupa Complex, NW Namibia / vorgelegt von Sönke Brandt." 2004. http://d-nb.info/974403253/34.

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22

Saunders, Brenton Mark. "Fluid-induced charnockite formation post-dating prograde granulite facies anatexis in southern Natal metamorphic province, South Africa." Thesis, 2014. http://hdl.handle.net/10210/10370.

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M.Sc. (Geology)<br>The Proterozoic Namaqua-Natal Mobile Belt of southern Africa represents a succession of high grade metamorphosed igneous and sedimentary rocks rimming the southern and western extents of the Kaapvaal craton. Different petrological processes associated with the onset of granulite facies metamorphism were investigated with the emphasis on the processes on anatexis and migmatitization and the influence of the fluid phase on these processes. The investigation took place in the Margate Terrane of the Southern Natal Metamorphic Province. The Umzimkulu and Louisiana Quarries near P

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23

Sriramguru, K. "Chemistry and metamorphic history of Granulite facies lithologies and associated rock types, south west of Rajapalaiyam, Tamil Nadu." Thesis, 2002. http://hdl.handle.net/2009/1487.

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24

Millonig, Leo Jakob [Verfasser]. "The neoarchean and palaeoproterozoic metamorphic evolution of the Limpopo Belt's Central Zone in southern Africa : new insights from petrological investigations on amphibolite to granulite facies rocks / vorgelegt von Leo Jakob Millonig." 2009. http://d-nb.info/1003787878/34.

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