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Rozprawy doktorskie na temat „Rocks, Metamorphic”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 stycznia 2023

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1

Nagurney, Alexandra Bobiak. "Microstructural Controls on the Crystallization and Exhumation of Metamorphic Rocks." Diss., Virginia Tech, 2021. http://hdl.handle.net/10919/103773.

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Microstructural data on the orientation and distribution of minerals can be utilized to better understand the processes controlling mineral crystallization during metamorphism and the extent to which equilibrium versus kinetic factors control the evolution of metamorphic rocks. Four studies in this dissertation address this, finding that: i) garnet crystals crystallize via epitaxial nucleation in which garnet crystallizes by templating on the crystal structure of muscovite; ii) the distribution of grain boundary void space at quartz-quartz and garnet-quartz grain boundaries is a function of th

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2

Huff, Timothy A. "Fluid inclusion evidence for metamorphic fluid evolution in the Black Hills, South Dakota /." free to MU campus, to others for purchase, 2004. http://wwwlib.umi.com/cr/mo/fullcit?p1421144.

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Chan, Heung-ngai. "Igneous and metamorphic rocks from SW Cyprus and NW Syria evidence for Cretaceous microplate collision and subsequent tectonic events in the Eastern Mediterranean /." Click to view the E-thesis via HKUTO, 2004. http://sunzi.lib.hku.hk/hkuto/record/B30711940.

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Cui, Xiaojun. "Numerical modeling of reactive fluid flow in the Notch Peak contact metamorphic aureole, Utah /." free to MU campus, to others for purchase, 2002. http://wwwlib.umi.com/cr/mo/fullcit?p3060092.

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NARUK, STEPHEN JOHN. "KINEMATIC SIGNIFICANCE OF MYLONITIC FOLIATION (METAMORPHIC)." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/184087.

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Geometric analyses of three mylonite zones, including two metamorphic-core-complex SC-mylonite zones, show that the mylonitic foliation surfaces (S-surfaces) are consistently discordant to the margins of the shear zones. Finite-strain analyses show that the foliation surfaces in each zone are consistently oriented parallel to the XY-plane of the finite strain ellipsoid. The shear bands within the mylonites (C-surfaces, C'-surfaces, extensional crenulations, and shear-band cleavages) are uniformly oriented subparallel to the margins of the shear zones. The finite lengths and discontinuous natur

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6

Rougvie, James Russell. "Metamorphism in the northern Park Range of Colorado : fluid-rock interactions and thermobarometry /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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7

Lewerentz, Alexander. "Fluid-induced alteration of metasedimentary rocks in the Scottish Highlands." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-146121.

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Fluids, mainly H2O and CO2, are released from H- and C-bearing phases during prograde metamorphism. Because of the buoyancy of these fluids, they rise within the crust towards the surface of the Earth. Metamorphic fluids take advantage of permeable horizons, shear zones, fold hinges, fractures, and are channelled into high-flux zones. Fluid fluxes for channelized fluid flow may exceed background pervasive fluxes by several orders of magnitude. Metamorphic fluids react with the surrounding rock during fluid flow, and altered zones are commonly observed adjacent to high-flux conduits. Fluid-alte

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8

Mawby, Joanna. "Metamorphic and geochronologic constraints on Palaeozoic tectonism in the eastern Arunta Inlier." Title page, table of contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09PH/09phm462.pdf.

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Appendix 4 and 5 in pocket on back cover. Bibliography: p. 123-130. The isotopic data indicates the Harts Range Metamorphic Complex formed within a previously unrecognized intracratonic tectonic province in Central Australia

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9

Strowbridge, Susan Leah. "Metamorphic evolution of anatectic metapelites from the Gabriel high strain zone, Grenville Province /." Internet access available to MUN users only, 2005. http://collections.mun.ca/u?/theses,62592.

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10

Pressler, Rebecca E. "An integrated petrofabric study of the high-pressure Orlica-Śnieźnik Complex, Czech Republic and Poland." Ohio : Ohio University, 2006. http://www.ohiolink.edu/etd/view.cgi?ohiou1149180445.

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11

Standley, Carl E. "Banda forearc metamorphic rocks accreted to the Australian continental margin : detailed analysis of the Lolotoi Complex of East Timor /." Diss., CLICK HERE for online access, 2007. http://contentdm.lib.byu.edu/ETD/image/etd1696.pdf.

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12

Carswell, Dennis Anthony. "Petrology, whole rock and mineral chemistry, thermobarometry and interpretation of high pressure metamorphic rocks." Thesis, University of Edinburgh, 1988. http://hdl.handle.net/1842/27764.

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13

Baker, Andrew James. "Metamorphic studies in the Scottish Highlands." Thesis, University of Oxford, 1985. http://ora.ox.ac.uk/objects/uuid:0000df07-a390-4b43-af48-31f04ba628ec.

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Conditions of 8kb and 800°C are estimated for sillimanite K feldspar bearing metapelites and garnet-clinopyroxene bearing amnphibolites in Glen Muick. These conditions are inconsistent with the simultaneous nearby presence of equilibrium between andalusite and kyanite. Andalusite in the Glen Muick area is late. The sillimanite zone may have been in part primary. There is a transition without major structural break between Tay Nappe flat belt and the "Banff Nappe". A dataset has been derived for phases in the system KCMASHCO<sub>2</sub>. The MHSRK equation of Kerrick and Jacobs (1981) has been

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14

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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15

Walker, James David. "The structure and metamorphic evolution of the High Himalayan Slab in SE Zanskar and NW Lahaul." Thesis, University of Oxford, 1998. http://ora.ox.ac.uk/objects/uuid:fc8b8fd3-e155-4f2f-9256-3667c2b31f4f.

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This thesis attempts to unravel the complex thermal and structural history of part of the High Himalayan Slab in NW India and combines reconnaissance-style field structural mapping of an area covering ~10,000 km<sup>2</sup> with petrography, microstructural analysis, thermobarometry and geochronology techniques. The results of this work show that the oldest protoliths of the High Himalayan Slab are at least Cambrian in age and that they may have experienced a major pre-Himalayan metamorphism at c.500 Ma. The youngest protoliths are Mesozoic in age (the Tandi Group) and demonstrate that the Hig

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16

Corona, Juan Carlos. "An experimental investigation of the reaction glaucophane + 2 quartz = 2 albite + talc /." Diss., Online access via UMI:, 2005.

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17

Jiang, Yingde, and 蒋映德. "High-grade metamorphic rocks in southern Altai Range, SW Central Asia: their origings, tectonothemal [i.e.tectonothermal] evolution and tectonic implications." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2012. http://hub.hku.hk/bib/B47752567.

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The Central Asian Orogenic Belt (CAOB), the largest accretionary collage on the Earth, has a complicated and prolonged accretionary history which remains being highly debated. High-grade terranes were previously interpreted as Precambrian micro-continents which played a very important role during the evolution of the CAOB. However, some of their presumed old ages are challenged by recent high-resolution dating results which raise questions on their Precambrian origins. The Chinese Altai and Tseel Terrane in the SW CAOB, two typical high-grade terranes occupy vital structural positions, fea

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18

Barboza, Scott A. "Anatexis and metamorphism of crustal rocks during magmatic accretion : field and numerical results /." Thesis, Connect to this title online; UW restricted, 1998. http://hdl.handle.net/1773/6741.

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19

Weiland, Richard John. "Emplacement of the Irian ophiolite and unroofing of the Ruffaer metamorphic belt of Irian Jaya, Indonesia /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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20

Evans, Lesley Jayne. "Low-grade regional metamorphism of Paleozoic rocks in the Midland Valley of Scotland." Thesis, University of St Andrews, 1988. http://hdl.handle.net/10023/15467.

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Low-grade burial metamorphism in the Midland Valley of Scotland, has been investigated with reference to the Silurian sediments and to the Carboniferous volcanics. In the Silurian sediments, facies definitive phyllosilicates are absent. Thin-section examination indicates that cementation was early and despite strong deformation, the lack of cleavage is related to the isotropic dispersal of domains during burial. Scanning electron microscopy and X-ray diffraction define clay mineral assemblages which characterize the transformation of montmorillonite to illite during burial. Illite crystallinit

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21

Chan, Heung-ngai, and 陳向毅. "Igneous and metamorphic rocks from SW Cyprus and NW Syria: evidence for Cretaceous microplate collision andsubsequent tectonic events in the Eastern Mediterranean." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2004. http://hub.hku.hk/bib/B30711940.

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22

Yang, Panseok. "Trace element partitioning between coexisting metamorphic minerals and trace element zoning in metamorphic minerals from Gagnon Terrane, western Labrador /." Internet access available to MUN users only, 2002. http://collections.mun.ca/u?/theses,35173.

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23

Bailey, David Elliott. "Metamorphic evolution of the crust of south-western Norway : an example from Sognefjord." Thesis, University of Oxford, 1989. http://ora.ox.ac.uk/objects/uuid:9c297189-fe46-4d4d-8821-4fce08d5f5cd.

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It is suggested that the Mafic Units and HS are allochthonous and were emplaced onto the WGR during an early stage of the Caledonian Orogeny. All units, including the Basement Gneisses, have suffered retrogression during a late extensional phase which continued into at least the Middle Devonian.

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24

Tollefsen, Elin. "Thermal and chemical variations in metamorphic rocks in Nautanen, Gällivare, Sweden." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-149643.

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This study focuses on the geology of the Nautanen area. It is part of the SGU-financed project, Metamorphic Map of Sweden, which aims to compile metamorphic data from Sweden and takes the form of a number of Bachelor and Master projects. The main metamorphic event in the Nautanen area is the Svecokarelian Orogeny (1.96 – 1.75 Ga). The samples are metamorphosed sedimentary and volcanic rocks, which were intruded by intermediate to mafic intrusions and a later granite intrusion. The supracrustal rocks are folded and the Nautanen Deformation Zone (NDZ) traverses the area in a NW to SE direction.

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25

Bramwell, M. G. "Crystal growth in some metamorphic rocks from the Lukmanier region, Switzerland." Thesis, Queen's University Belfast, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.372952.

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26

Songul, Gunes. "Archaeometrical Study On Marble Forgery." Master's thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614566/index.pdf.

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This thesis focuses on the detection of marble sculpture forgery made of cultured marble. Cultured marble is a mixture of marble dust, polyester and accelerators. Thus chemical analysis of cultured marble would give declined levels of calcium when compared to authentic sculptures. Since sample removal is a problem when dealing with archaeological heritage, the instrument used was portable X-Ray Fluorescence device which provides in situ analysis of the samples. Device has been used to analyze six authentic and four forgery sculptures. Seven of the sculptures were provided by Anatolian Civiliza

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27

Lawrence, Robert William. "The structure and metamorphism of the Irindina supracrustal assemblage on the western side of the Entia Dome, Harts Range, central Australia /." Title page, contents and summary only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phl4225.pdf.

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Thesis (Ph. D.)--University of Adelaide, Dept. of Geology and Geophysics, 1987.<br>Typescript. Maps in back pocket of v. 1. Microfiches in back pocket of v. 2. Microfiches contain petrographic descriptions, total rock XRF analyses and microprobe analyses. Includes bibliographical references (leaves 160-183 (v. 2)).

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28

Herd, Michelle Erica June. "Continental Extensional Tectonics - The Paparoa Metamorphic Core Complex of Westland, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2007. http://hdl.handle.net/10092/1425.

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Cretaceous continental extension was accommodated by the development of the Paparoa Metamorphic Core Complex, resulting in the separation of New Zealand from Gondwana. High grade (Lower Plate) and low grade (Upper Plate) rocks are separated by the Ohika and Pike Detachment Faults. The two detachment faults have distinctly different histories, with greater exhumation along the Pike Detachment Fault. The onset of crustal extension is proposed to have commenced along the Pike Detachment Fault at 116.2 ± 5.9 Ma (Rb/Sr dating). Both geochemical and geochronological approaches are adopted for this t

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29

Bowman, Dannena Renee Steltenpohl Mark G. "Exhumation history of Caledonia eclogites in Liverpool Land, East Greenland, and comparisons with eclogites in Norway." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Geology_and_Geography/Thesis/Bowman_Dannena_35.pdf.

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30

McDonald, Wayne M. Hames W. "⁴⁰Ar/³⁹Ar ages of muscovite from the western Blue Ridge and Talladega belt, Georgia and North Carolina." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Geology_and_Geography/Thesis/Mcdonald_Wayne_42.pdf.

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31

Haney, Erin Marie. "Pressure-temperature evolution of metapelites within the Anaconda metamorphic core complex, southwestern Montana." CONNECT TO THIS TITLE ONLINE, 2008. http://etd.lib.umt.edu/theses/available/etd-07252008-111800/.

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32

Tam, Pui-yuk, and 譚佩玉. "Ages and tectonic nature of the high-pressure metamorphosed pelitic and mafic rocks in eastern Shandong, North China Craton." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hub.hku.hk/bib/B49799526.

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The Paleoproterozoic Jiao-Liao-Ji Belt (JLJB) is a NNE-SSW trending continental belt lying in the Eastern Block of the North China Craton, with its southern segment extending across Bohai Sea into the Jiaobei massif. Little work has been done in the southern segment of the belt, and thus the timing for metamorphism and tectonic nature of the JLJB are still controversial, with models ranging from those invoking continent-arc-continent collision to those advocating rifting closure. The presence of the high-pressure pelitic and mafic rocks of the Jiaobei massif (Eastern Shandong) located in the

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33

Labadie, Julia E. Schermer Elizabeth. "The structural and tectonic history of the Mt. Formidable region, North Cascades, Washington /." Online version, 2010. http://content.wwu.edu/cdm4/item_viewer.php?CISOROOT=/theses&CISOPTR=333&CISOBOX=1&REC=14.

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34

Miller, Martin Gregg. "Structural and kinematic evolution of the Badwater Turtleback, Death Valley, California /." Thesis, Connect to this title online; UW restricted, 1992. http://hdl.handle.net/1773/6716.

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35

Zack, Thomas. "Trace element mineral analysis in high pressure metamorphic rocks from Trescolmen, Central Alps." [S.l. : s.n.], 1999. http://deposit.ddb.de/cgi-bin/dokserv?idn=963753924.

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36

Dean, Andrew. "Upper Palaeozoic palynomorphs from the low grade metamorphic rocks of Devon and Cornwall." Thesis, University of Exeter, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303917.

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37

Moore, John Michael. "A comparative study of metamorphosed supracrustal rocks from the western Namaqualand metamorphic complex." Doctoral thesis, University of Cape Town, 1986. http://hdl.handle.net/11427/22585.

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Bibliography: pages 346-370.<br>A regional study of highly metamorphosed supracrustal rocks was undertaken in the western portions of the Namaqualand Metamorphic Complex. The study area was essentially restricted to a north-south section some 50 kilometres wide and 220 kilometres long. Eight east-west-trending belts of supracrustal rocks were examined, together with several smaller paragneiss remnants, in an area dominated by quartzo-feldspathic gneisses of granitic composition. The supracrustal rocks were classified into seven major lithological groups: quartzitic rocks, metapelitic and metap

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38

Sigler, Joshua T. "The metamorphic and structural evolution of the Davis Peak area, northern Park Range, Colorado." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1798480831&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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39

Kassos, Gabriel Philip Steltenpohl Mark G. "Structural, isotropic, and kinematic analysis of eclogite-facies shear zones and associated structures, Lofoten, North Norway." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SUMMER/Geology_and_Geography/Thesis/Kassos_Gabriel_39.pdf.

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40

Layfield, Nathan Timothy Hames W. "Permian to Cretaceous evolution of the Piedmont along the Alabama - Georgia coastal plain unconformity." Auburn, Ala, 2009. http://hdl.handle.net/10415/1731.

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41

Holness, Marian Barbara. "Experimental and petrological studies of textural equilibrium and fluid flow in metacarbonate rocks : the Beinn an Dubhaich Aureole, Skye." Thesis, University of Cambridge, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.385419.

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42

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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43

Parkinson, Christopher David. "The petrology, structure and geologic history of the metamorphic rocks of Central Sulawesi, Indonesia." Thesis, Royal Holloway, University of London, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.361396.

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44

Dransfield, Malcolm. "Extensional exhumation of high-grade metamorphic rocks in western Norway and the Zanskar Himalaya." Thesis, University of Oxford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387017.

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45

Tadesse, Tarekegn. "A stratigraphic, structural and metamorphic analysis of Dalradian Rocks west of Ballater, northeast Scotland." Thesis, Queen's University Belfast, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.241492.

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46

Buchanan, John Wesley Steltenpohl Mark G. "Tectonic evolution of a Caledonian-aged continental basement eclogite terrane in Liverpool Land, East Greenland." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Geology_and_Geography/Thesis/Buchanan_John_21.pdf.

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47

Kleine, Barbara. "How do fluids move through rocks? : High fluxes of CO2 in the Earth's crust." Licentiate thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-84007.

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Metamorphic hydrous, CO2-bearing fluids play a critical role in the global carbon cycle. However, how big this influence is on the global carbon cycle and therefore on global climatic processes, is unknown. The actual amount of CO2 which is released into the atmosphere due to metamorphic processes is still debated. For this purpose, fluid-driven reactions in metamorphic rocks must be studied by tracking fluid-rock interactions along pathways of ancient fluids. In the study presented in this thesis, we study fluid-rock interaction in the southeastern part of the Greek island Syros in the Cyclad

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48

Evans, Thomas P. "The proterozoic metamorphic evolution of rocks exposed in the White Range Nappe, Central Australia : polymetamorphism and an unconformity in the Southern Strangways metamorphic complex /." Adelaide, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbe92.pdf.

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49

Lalonde, André E. "The intrusive rocks of the Hepburn metamorphic-plutonic zone of the central Wopmay Orogen, N.W.T. /." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=76906.

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50

Bugdaycioglu, Cagri. "Tectono-metamorphic Evolution Of The Northern Menderes Massif: Evidence From The Horst Between Gordes And Demirci Basins (west Anatolia, Turkey)." Master's thesis, METU, 2004. http://etd.lib.metu.edu.tr/upload/12605378/index.pdf.

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The Menderes Massif forms a large metamorphic culmination in western Turkey &amp<br>#8211<br>an extensional province where continental lithosphere has been stretching following Palaeogene crustal thickening. Northern sector of the Massif on the horst between G&ouml<br>rdes and Demirci Basins was chosen for structural analysis aimed to study the tectono-metamorphic evolution of the northern Menderes Massif. Within the study area, four groups of rocks are recognized: (1) the metamorphic rocks &amp<br>#8211<br>orthogneisses and metasediments<br>(2) pegmatoids<br>(3) Neogene sedimentary rocks<br>

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