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Dissertations / Theses on the topic 'Schist belt'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Omitogun, Ayotunde Allen. "Métamorphisme et structure de la zone mobile pan-africaine centrale du Nigéria ("Schist belt" d'Igarra)." Toulouse 3, 1991. http://www.theses.fr/1991TOU30275.

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La zone mobile du nigeria comprend dans la partie occidentale, des formations supracristales regroupees en entites bien definies au sein d'un complexe de gneiss et de migmatites: les schist-belts ou ceintures schisteuses. Par l'etude de la ceinture d'igarra s. C. Situee dans la partie centrale de la zone mobile, le metamorphisme pan-africain a ete defini. Dans les formations supracrustales du schist belt c'est un metamorphisme de facies amphibolite caracterise par l'association grenat-andalousite-staurotide dans les metapelites. Les conditions p/t definies par le geothermometre gt-bi et les do

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2

Diener, Johann F. A. "The tectono-metamorphic evolution of the Theespruit Formation in the Tjakastad Schist Belt and surrounding areas of the Barberton Greenstone Belt, South Africa." Thesis, Stellenbosch : University of Stellenbosch, 2004. http://hdl.handle.net/10019.1/16309.

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Thesis (MSc)--University of Stellenbosch, 2004.<br>ENGLISH ABSTRACT: The southern portions of the Early- to Mid-Archaean Barberton granitoid-greenstone terrain of South Africa consists of a high-grade metamorphic granitoid-gneiss terrain that is juxtaposed against the low-grade metamorphic supracrustal sequence of the Barberton Greenstone Belt. The boundary of the two different crustal domains corresponds to the Theespruit Formation, an amphibolite-facies, highly tectonized mélange of metabasites, felsic volcanics and rare, aluminous clastic sediments that occurs along the granitoidgreens

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3

Roberts, Todd M. "GEOCHEMICAL AND STRATIGRAPHIC ANALYSIS OF META-SEDIMENTARY ROCKS OF THE GNEISS DOME BELT, WESTERN CONNECTICUT AND MASSACHUSETTS." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin990633701.

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4

Tünker, Maren Edda. "Mesozoic fold structure of the Otago and alpine schist belt and its implications on the tectonic evolution of South Island, New Zealand." [S.l. : s.n.], 2002. http://deposit.ddb.de/cgi-bin/dokserv?idn=96993856X.

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5

Korkalo, T. (Tuomo). "Gold and copper deposits in Central Lapland, Northern Finland, with special reference to their exploration and exploitation." Doctoral thesis, University of Oulu, 2006. http://urn.fi/urn:isbn:951428108X.

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Abstract At least 30 gold deposits verified by means of one or more notable diamond drill hole results have been discovered in Central Lapland in the last 20 years, and these can be divided spatially into groups, between which the metal composition varies. The deposits contain varying amounts of sulphides and sulpharsenides as well as gold. Pyrite is the most common sulphide mineral in the gold deposits associated with volcanic rocks, and usually pyrrhotite in those associated with sedimentary rocks. The principal sulphide minerals in those connected with banded iron formations are pyrite and

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6

Niebling, Ulf. "Untersuchungen zum Wachstum dünner Schichten organischer Metalle aus (BEDT-TTF) 2 I 3." [S.l. : s.n.], 2001. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB9918598.

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7

Longino, Brando. "Entanglement: dai postulati della meccanica quantistica al teorema di Bell." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2017. http://amslaurea.unibo.it/14595/.

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In questo lavoro di tesi vengono presentati inizialmente i postulati della meccanica quantistica, passando poi alla descrizione di stati tramite vettori in uno spazio di Hilbert e, successivamente, alla descrizione tramite l’operatore densità associato al sistema. Introducendo quindi i concetti di qubit e di decomposizione di Schmidt, si mostra il fenomeno chiamato Entanglement, illustrando alcuni esempi. Nel quinto capitolo viene trattata l’Entropia di Von Neumann come stumento per quantificare l’Entanglement di un sistema, mentre nel sesto si discute il problema del paradosso EPR, acco

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8

Courtot, Hervé. "Les terrains volcaniques paléozoïques et les minéralisations associées dans la série métamorphique de la Brévenne. District de Sain-Bel/Chessy (Rhône)." Paris 6, 1987. http://www.theses.fr/1987PA066321.

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9

Kumar, Satish G. "Hydrogeology around Holenarasipur schist belt, Karnataka, India." Thesis, 2003. http://hdl.handle.net/2009/3088.

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10

LIN, MEI-LING, and 林楳嶺. "Petrotectonic study on the Yuli belt of Tananao schist in the Chinshuichi Area, Yuli, Hualien, Taiwan." Thesis, 1986. http://ndltd.ncl.edu.tw/handle/45459536172037368950.

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11

Audet, Marc-Antoine. "Geological study of the Signal Hill Au-As-Sb deposits, Archaean Tati schist belt, Northeast Botswana." Thesis, 2016. http://hdl.handle.net/10539/21332.

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This thesis is submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, for the Degree of Master of Science. January 1995.<br>The Signal Hill Au-As-Sb deposits lie in the uppermost formations of the Archaean Tati Schist belt, located in northwest Botswana. The surface exposures of the potentially economic deposits are confined to three main zones: “A” Zone, “B” Zone and the “F” Zone. The “A” Zone and the “B” Zone are found with the sedimentary assemblage of the Last Hope Formation, while the “F” Zone lies within the underlying volcanic Penhalonga Formation. : [Abbrev

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12

Liu, Cheng-Hao, and 劉丞浩. "Detrital zircon U-Pb age study of the Tailuko belt in the Tananao Schist, eastern Taiwan." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/95632935175248364658.

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碩士<br>國立臺灣大學<br>地質科學研究所<br>101<br>The oldest rocks exposed in Taiwan are the Tananao Schist that exposed along the eastern slope of the Central Range. It mainly consists of schist, marble, and metamorphosed granites. The protolith for marble is supposed to be late Permian, and the protolith for schist is middle Mesozoic. Because of lacking fossils and radiometric dating, the depositional age of schist was difficult to define. U-Pb ages of detrital zircons represent crystallization age of sediment sources (terranes), and the youngest age may be close to or older than the depositional age. There

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13

Kedda, Sean Waugh. "Geochemical and stable isotope studies of gold bearing granitoids in the Murchison Schist Belt, North Eastern Transvaal." Thesis, 2012. http://hdl.handle.net/10539/11161.

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14

Tünker, Maren Edda [Verfasser]. "Mesozoic fold structure of the Otago and alpine schist belt and its implications on the tectonic evolution of South Island, New Zealand / Maren Edda Tünker." 2002. http://d-nb.info/96993856X/34.

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15

LIN, Chii-Wen, and 林啟文. "Structural Styles and Structural Evolution of the Slate and Schist Belts in Northeastern Taiwan." Thesis, 1998. http://ndltd.ncl.edu.tw/handle/06585192257656648629.

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16

Manhica, Antonio dos Santos Tcheco. "The geology of the Mozambique belt and the Zimbabwe craton around Manica, Western Mozambique." Diss., 1998. http://hdl.handle.net/2263/28883.

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The study area comprises the Archaean Manica Greenstone Belt and the Vumba Granite Gneiss, the Proterozoic Messica Granite Gneiss of the Zimbabwe Craton, the possibly allochthonous metasedimentary sequence of the Frontier Formation, the granitoids of the Mozambique Metamorphic Province, which are subdivided into Vanduzi Migmatite Gneiss, the Chimoio Granodiorite Gneiss, the Nhansipfe Granitic Orthogneiss and the Pan-African Tchinhadzandze Granodiorite Gneiss. The rock sequences in the two provinces are cut by mafic intrusions. The greenstone belt comprises mafic to ultramafic and pelitic schis

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17

Huang, Huei-Ting, and 黃會婷. "Metamorphic Evolution and Geologic Implications of In-situ Schists and Mafic Rocks in the Juisui Area, Yuli Belt, Eastern Taiwan." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/36647000320789038882.

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碩士<br>國立東華大學<br>自然資源與環境學系<br>101<br>The Yuli belt of the eastern Taiwan is generally divided into two parts: tectonic (or exotic) blocks and in-situ schists. The former consists mainly of serpentinite and metabasite, whereas the latter is represented by metapelite and metapsammite with subordinate greenschist. The contacts between these two different litho-units tend to contain newly-recrystallized minerals that indicate a possible origin of metasomatism. In the in-situ metapelites, this study found a new type of two-stage garnet zoning with a sharp break in between. Zone I garnet (core) is ov

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