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Dissertations / Theses on the topic 'Alkalic igneous rocks. Petrology'

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Published: 4 June 2021

Last updated: 14 February 2022

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1

Johnson, Geoffrey I. "The petrology, geochemistry and geochronology of the felsic alkaline suite of the eastern Yilgarn Block, Western Australia /." Title page, contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09PH/09phj67.pdf.

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Thesis (Ph. D.)--Dept. of Geology and Geophysics, University of Adelaide, 1992.<br>Typescript (Photocopy). Includes copies of 4 papers by the author as appendix 4 (v. 1). Errata slip inserted. Includes bibliographical references (leaves 170-192 (v. 1)).

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2

Liu, Junsuo. "Pétrogénèse des roches alcalines mafiques d'âge méso-cénozoique dans les provinces de Hunan et Guangxi, Chine septentrionale = petrogenesis of the mesosoic-cenozoic mafic alkaline subvolcanic rocks in Hunan-Guangxi provinces, southern China /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1992. http://theses.uqac.ca.

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3

Potgieter, J. E. "Anorogenic alkaline ring-type complexes of the Damaraland Province, Namibia, and their economic potential." Thesis, Rhodes University, 1987. http://hdl.handle.net/10962/d1001567.

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Anorogenic alkaline ring-type complexes form within continental plate settings. Alkaline magmatism is derived from the upper mantle, in which mantle metasomatism plays an important part, as well as from partial melting of the lower crust. Radial and concentric fractures develop during the ascent of alkaline magma. Extrusion of basic and felsic magma takes place along these fractures with felsic volcanics building-up central volcanoes. As a result of emptying of the magma chamber, the superstructure of the volcano collapses and a caldera is formed. During the caldera stage syenitic and granitic

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4

La, Rocque Cynthia A. "Geochronology and petrology of north-central Gaspe igneous rocks, Quebec." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65499.

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5

Lee, Paula M. "Spatial, temporal, and petrogenetic relationship of basaltic and lamprophyric dikes and sills of the Raton Basin, southern Colorado and northern New Mexico." Diss., Columbia, Mo. : University of Missouri-Columbia, 2005. http://hdl.handle.net/10355/5848.

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Thesis (M.S.)--University of Missouri-Columbia, 2005.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (July 11, 2006) Includes bibliographical references.

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6

Smithies, Robert Hugh. "The geochemical evolution of three alkaline complexes in the Kuboos-Bremen igneous province, southern Namibia." Thesis, Rhodes University, 1992. http://hdl.handle.net/10962/d1005564.

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The Kuboos-Bremen Igneous Province comprises a linear zone of alkaline complexes that intrude Proterozoic and Pan-African rocks and trends in a northeast direction from the northwest of the Cape Province in South Africa into southern Namibia. Of the three most southerly complexes in Namibia. two comprise silicate rocks ranging from nepheline syenite to alkali-granite and are called the Grootpenseiland and Marinkas Kwela Complexes (GPC and MKC). The Marinkas Kwela Carbonatite Complex is the third and most northerly of the complexes. Isotopic age determinations on a number of rock types from bot

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7

Christodoulou, C. "Petrology of the plutonic rocks of the Macquarie Island Complex /." Title page, contents and abstract only, 1990. http://web4.library.adelaide.edu.au/theses/09PH/09phc556.pdf.

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8

Church, Abigail Ann. "The petrology of the Kerimasi carbonatite volcano and the carbonatites of Oldoinyo Lengai with a review of other occurrences of extrusive carbonatites." Thesis, University College London (University of London), 1996. http://discovery.ucl.ac.uk/1349623/.

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Extrusive carbonatites are rare igneous rocks with just 37 known localities. The majority are calciocarbonatites, the principal exception being those of the active volcano, Oldoinyo Lengai, which are strongly alkaline. Unresolved questions concerning extrusive carbonatites include: 1. Why are extrusive carbonatites at Lengai chemically different from all others? 2. Could the extrusive calciocarbonatites originally have had alkaline compositions? In order to address these questions extrusive carbonatites from both Lengai and the adjacent volcano, Kerimasi, were collected and compared. A compila

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9

Lum, Clinton Chew Lun. "Aspects of the petrogenesis of alkali basalts from the Lunar Crater volcanic field, Nevada." Connect to resource, 1986. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1230660431.

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10

Perry, Anna F. Parker Donnie Franklin. "Petrology of Cascade Head Basalt, Oregon Coast Range, USA." Waco, Tex. : Baylor University, 2007. http://hdl.handle.net/2104/5079.

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11

Wilt, Jan Carol. "Geochemical patterns of hydrothermal mineral deposits associated with calc-alkalic and alkali-calcic igneous rocks as evaluated with neural networks." Diss., The University of Arizona, 1993. http://hdl.handle.net/10150/186500.

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Six alkalinity and oxidation classes of fresh igneous rocks were correlated with trace elements in rock chip samples from temporally and spatially associated ore deposits. Learning vector quantization and back-propagation artificial neural networks correctly classified 100 percent of whole rock oxides and 99 percent of mineralized samples; discriminant analysis correctly classified 96 and 83 percent, respectively. The high degree of correlation between chemistries of igneous rocks and related mineralization implies genetic links between magmatic processes or sources and the ore deposits studie

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12

Grosser, Benjamin. "Petrology and geochemistry of the Wildcat Gulch syenite, Gunnison County, Colorado /." Electronic version (PDF), 2005. http://dl.uncw.edu/etd/2005/grosserb/benjamingrosser.pdf.

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13

Buick, Ian S. "The petrology and geochemistry of granitic rocks from the Entia domal structure, Harts Range, eastern Arunta Block, Central Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09SM/09smb932.pdf.

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14

Florence, Frank P., and Frank P. Florence. "Petrology of mantle xenoliths in the Sloan kimberlite, Larimer County, Colorado." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558046.

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15

Mainville, Michèle. "Les komatiites et tholéiites à la base du groupe de baby, Témiscamingue /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1994. http://theses.uqac.ca.

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16

Ipekgil, Ceren. "Geology And Petrology Of Beypazari-oymaagac Granitoids." Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/2/12605846/index.pdf.

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The purpose of this study is to investigate the origin, source characteristics, evolution petrogenesis and emplacement mechanisms of Beypazari-Oymaaga&ccedil<br>granitoids. These granitoids are intruded into a metamorphic basement and nonconformably overlain by Neogene clastic rocks. Field work, petrographical and geochemical studies are carried out to determine the petrologic features and tectonic setting of the granitoid body. The Beypazari-Oymaaga&ccedil<br>pluton is a composite pluton with its host batholith, enclaves, aplite dykes and a pegmatite. The batholith is generally composed of q

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17

Raymond, Anne Charlotte. "Carboniferous rocks of the eastern and central Midland Valley of Scotland : organic petrology, organic geochemistry and effects of igneous activity." Thesis, University of Newcastle Upon Tyne, 1991. http://hdl.handle.net/10443/315.

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An integrated organic petrological and geochemical approach has been adopted to evaluate the variation in the type of organic materials contributing to the Carboniferous succession in the eastern and central Midland Valley and to assess the extent to which both extrusive and intrusive igneous activity have modified the optical and geochemical properties of organic matter in this province. The type investigation reveals that the succession is extremely rich in organic matter, much of which originated from the vascular tissues of higher plants. The profound influence of terrestrial sedimentation

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18

Péloquin, Alice Shirley. "The petrographic and geochemical variations in archean meta-basaltic pillows from the Kinojevis Group of the Abitibi Greenstone Belt, Rouyn-Noranda, Québec = Les variations pétrographiques en géochimiques des coussins basaltiques archéens du groupe de Kinojevis, sous-province de l'Abitibi, Rouyn-Noranda, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1990. http://theses.uqac.ca.

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19

Côté, Denis. "Pétrographie, pétrologie et étude géochimique du dyke de diorite, de l'intrusion troctolitique et des deux petits massifs anorthositiques de Canton Taché /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1986. http://theses.uqac.ca.

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Mémoire (M.Sc.A.)--Université du Québec à Chicoutimi, 1986.<br>"Mémoire présenté à Chicoutimi en vue de l'obtention d'une maîtrise en science appliquée (géologie)" CaQCU Bibliogr.: p. 129-134. Document électronique également accessible en format PDF. CaQCU

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20

McMullin, David William Augustine. "Thermobarometry of pelitic rocks using equilibria between quartz-garnet-aluminosilicate-muscovite-biotite, with application to rocks of the Quesnel Lake area, British Columbia." Thesis, University of British Columbia, 1990. http://hdl.handle.net/2429/31043.

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Rocks of the Quesnel Lake area are divided into three units: unit 1, a continental margin sequence; unit 2, The Crooked Amphibolite (an ocean-floor sequence); and unit 3, the Quesnel sedimentary and volcanic sequence. Two conglomerate localities within unit 3 contain clasts identified as being derived from deformed rocks of units 1 and 2. Deformation of the combined package of units 1 and 2 must have accompanied the emplacement of unit 2 onto unit 1 sometime between the deposition of unit 2 (Mississippian - Permian) and the deposition of unit 3 (Triassic - Jurassic). Rocks of unit 1 have been

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21

Lefebvre, Christian. "Étude de la genèse des pépérites et de leur contexte volcano-sédimentaire, formation de Blondeau, Chibougamau, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1991. http://theses.uqac.ca.

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Mémoire (M.Sc.T.)-- Université du Québec à Chicoutimi, 1991.<br>"Mémoire présenté en vue de l'obtention de la maîtrise en sciences de la terre" CaQCU Bibliogr.: f. 166-171. Document électronique également accessible en format PDF. CaQCU

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22

Terracin, Matthew Theodore. "Petrography, geochemistry and origin of atypical sedimentary-igneous contact relationships at the base of the Hotazel Formation around Middelplaats, Northern Cape Province, RSA." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1012985.

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In the Middelplaats mine area of the Kalahari manganese field, two drill holes (MP53 and MP54) intersected anomalously high-grade manganese ore sitting stratigraphically just above an igneous body (likely a dike or sill). Manganese ore located within approximate 5 meters of the contact with the underlying igneous rocks has been substantially metasomatically upgraded from 25 percent manganese, to over 40 percent whilst the dominant manganese species within the ore has been altered to hausmannite. This report demonstrates the metasomatic alteration is related to devolatilization (removal and/or

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23

Fackir, Sanaâ. "Origine des ségrégations leucocrates et des biotitites dans une intrusion felsique-mafique syntectonique : exemple de la région de Baie-Comeau (Tadoussac) /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2005. http://theses.uqac.ca.

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24

BESSER, Marcell Leonard. "Sequência vulcânica ácida da região de São Joaquim-SC: reoignimbritos ou lavas?" reponame:Repositório Institucional da CPRM, 2017. http://rigeo.cprm.gov.br/jspui/handle/doc/18194.

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Submitted by Teresa Cristina Rosenhayme (teresa.rosenhayme@cprm.gov.br) on 2017-10-17T14:25:49Z No. of bitstreams: 1 Tese Marcell L. Besser.pdf: 26010964 bytes, checksum: a9834adf566ddb70c42cc10b3dc9c6b8 (MD5)<br>Approved for entry into archive by Jéssica Gonçalves (jessica.goncalves@cprm.gov.br) on 2017-10-18T07:58:09Z (GMT) No. of bitstreams: 1 Tese Marcell L. Besser.pdf: 26010964 bytes, checksum: a9834adf566ddb70c42cc10b3dc9c6b8 (MD5)<br>Approved for entry into archive by Jéssica Gonçalves (jessica.goncalves@cprm.gov.br) on 2017-10-18T08:18:10Z (GMT) No. of bitstreams: 1 Tese Marcell L.

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25

Dillet, Brigitte. "Petrography and mineralogy of the granitic rocks associated with questa caldera (new mexico, u. S. A. )." Clermont-Ferrand 2, 1987. http://www.theses.fr/1989CLF21051.

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L'etude petrographique des neuf plutons granitiques associes a la caldera de questa (nouveau mexique) a permis de mettre en evidence l'existence d'une lignee alcaline et d'une lignee calcoalcaline granodioritique a monzonitique l'existence de ces deux series peut etre reliee a l'evolution geodynamique regionale a l'epoque de leur mise en place. Les donnees geochimiques confirment les resultats de l'etude petrographique. Les relations ilmenite-magnetite-sphene et la composition de l'ilmenite, de la magnetite, de la biotite et de l'amphibole ont permis de mettre en evidence des conditions de cri

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26

Couture, Jean-François. "Géologie de la formation de Gilman dans la partie centrale du canton de Roy, Chibougamau, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1986. http://theses.uqac.ca.

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Mémoire (M.Sc.A.)-- Université du Québec à Chicoutimi ; 1986.<br>"Mémoire présenté pour l'obtention du grade de maîtrise es sciences appliquées" CaQCU Document électronique également accessible en format PDF. CaQCU

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27

Carrazana, Di Lucia Ariana. "El volcanismo calcoalcalino y peralcalino del suroeste de Cerdeña (Italia) y mineralizaciones asociadas." Doctoral thesis, Universitat de Barcelona, 2020. http://hdl.handle.net/10803/672411.

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El volcanismo oligo-mioceno del Sulcis, SO de Cerdeña (Italia) presenta la particularidad de contener rocas peralcalinas y alcalinas de un ambiente geodinámico anorogénico posterior a la actividad orogénica relacionada con la subducción de una placa oceánica durante la migración antihoraria del bloque Sardo-Corso y la sincrónica creación de la cuenca Liguro-Provençal. La geocronología 40Ar/39Ar (feldespatos), marca el final de la actividad magmática calcoalcalina a 16.18±0.04 Ma (Burdigaliense) y el inicio del episodio anorogénico a 15.96±0.04 Ma (Langhiniense inferior). La duración del evento

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28

BOISSON, DOMINIQUE. "Etude geologique du massif du nord d'haiti (hispaniola - grandes antilles)." Paris 6, 1987. http://www.theses.fr/1987PA066771.

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Le massif du nord est un edifice cretace et tertiaire polyphase appartenant a la bordure nord de l'orogene caraibe. Son etude stratigraphique et petrographique permet d'y distinguer : une logique de depot post-danienne caracterisee par : une sedimentation neogene essentiellement detritique : deux cycles de plate-forme carbonatee (l'un a l'eocene et l'autre au miocene inferieur) separes par une discordance fini-eocene et une lacune locale de sedimentation oligocene. Tous ces terrains sont supportes par l'ensemble volcano-sedimentaire de l'arc cretace recoupe par plusieurs generations d'intrusif

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29

Laporte, Didier. "Un exemple d'intrusion syntectonique : l'intrusion d'Ile-Rousse, Corse du nord-ouest : étude pétrographique, minéralogique et géochimique, analyse structurale." Saint-Etienne, 1987. http://www.theses.fr/1987STET4001.

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L'intrusion d'Ile Rousse est une association intime de granitoïdes aux caractéristiques plus ou moins fortement contrastées, juxtaposés en lames subméridiennes à fort pendage. On y distingue des granitoïdes calcoalcalins magnésio-potassiques et des granitoïdes n'appartenant pas à l'association magnésiopotassiques dont les mieux types sont les granodivrités de Corbara. Analyse statistique de la sous-fabrique des mégacristaux de Feldspath potassique accompagnée d'une modélisation mathématique

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30

Dupont, Pierre-Luc. "Pétrologie et géochimie des ensembles magmatiques pharusien I et II, dans le rameau oriental de la chaîne pharusienne (Hoggar, Algérie) : Implications géodynamiques pour l'évolution d'une chaîne mobile au protérozoïque supérieur." Nancy 1, 1987. http://www.theses.fr/1987NAN10332.

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Au pharusien I, la série de timesselarsine révèle l'épanchement de basaltes, d'affinité transitionnelle a faiblement alcaline dont le site géodynamique serait celui d'un "rift" en domaine continental. Vient ensuite une série ultrabasique/basique dont le site le plus probable est celui d'arc insulaire ou de bassin marginal. Le troisième épisode est représenté par deux ensembles : un lié à un domaine de type arc insulaire, l'autre montrant une évolution vers une marge continentale active. Au pharusien II, la série d'anded est intrudée par des dolérites et des roches volcaniques en liaison avec u

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31

Dissler, Eric. "Evolution geodynamique cadomienne du nord-cotentin (massif armoricain)." Caen, 1987. http://www.theses.fr/1987CAEN2048.

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La structuration actuelle des terrains brioveriens resulte en grande partie de l'evolution tectono-metamorphique varisque. La chaine cadomienne accuse une vergence nord-ouest. L'identification geochimique des series volcaniques brioveriennes revele une affinite tholeitique generalisee. Une tendance calcoalcaline s'exprime en revanche au sein du batholite de la hague. L'enchainement des premieres etapes de l'evolution geodynamique cadomienne est ainsi etablie, le magmatisme du brioverien inferieur traduisant le fonctionnement d'un dispositif arcs insulaires-bassins marginaux de type marge ouest

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32

Mboungou-Kongo, Jean-Baptiste. "Les formations metamorphiques devono-dinantiennes et les roches plutoniques de la region sud-ouest de clermont-ferrand (massif central francais) : etudes petrographique, geochimique et structurale." Clermont-Ferrand 2, 1987. http://www.theses.fr/1987CLF21027.

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Le socle hercynien au sud-ouest de clermont-ferrand comporte une serie volcano-sedimentaire. Des corps plutoniques y sont intrusifs et la metamorphisent. Diorites et gabbros resultent d'une lignee de differenciation calco-alcaline, avec des facies de cumulats. Les etudes geochimiques soulignent le contraste entre le cortege gabbro-dioritique essentiellement mantellique, et les granites crustaux. L'analyse structurale de la serie volcano-sedimentaire montre deux phases de deformation

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Costarella, René. "Le complexe annulaire alcalin de Combeynot ( Massifs cristallins externes, Alpes françaises), témoin d'un magmatisme en régime distensif. Pétrogéochimie et signification géodynamique." Phd thesis, Grenoble 1, 1987. http://tel.archives-ouvertes.fr/tel-00539879.

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Le massif de Combeynot, sur la bordure nord-orientale du massif du Haut-Dauphiné (massifs cristallins externes, Alpes Françaises) est constitué de deux unités fondamentales (1) un socle, déformé et métamorphisé, représenté par un ensemble migmatitique et un orthogneiss oeillé ; ce socle se rattache aux formations du noyau du massif du Haut-Dauphiné, (2) un complexe annulaire subvolcanique, intrusif dans le socle, composé de formations volcaniques et volcano-détritiques, d'un réseau filonien microgranitique et rhyolitique très dense, de deux unités granitiques disposées de manière concentrique

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Benzakour, Abderrahim. "Le volcanisme permien des Vosges du Nord : un témoin d'une évolution dans le cycle orogénique varisque de l'Europe occidentale." Nancy 1, 1988. http://www.theses.fr/1988NAN10252.

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Cette thèse présente une étude pétrographique et géochimique des roches volcaniques (diabases, trachy-andésites, rhyodacites, rhyolites, ignimbrites) permienne des Vosges du Nord en vue de connaître les relations pétrogénétiques entre les différents faciès et le cadre géodynamique de leur mise en place. Deux séries calcoalcalines sont distinguées et l'enrichissement en K::(2)O qui représente un caractère généralisé de ces roches est discuté

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35

Pivin, Marjorie. "La suite complexe des mégacristaux des kimberlites de Mbuji-Mayi en République Démocratique du Congo: témoins du métasomatisme dans le manteau lithosphérique sous-continental archéen du craton du Congo-Kasaï." Doctoral thesis, Universite Libre de Bruxelles, 2012. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209701.

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L’origine des suites de mégacristaux des kimberlites est sujette à d’intenses débats depuis de nombreuses années. La suite complexe de mégacristaux (grenat, clinopyroxène, zircon, baddeleyite, ilménite, rutile et nodules d’intercroissances rutile-silicates) des kimberlites diamantifères de Mbuji-Mayi (Kasaï Oriental), mises en place au Crétacé dans le craton archéen du Congo-Kasaï, a été étudiée en détails dans le but d’établir les relations entre les différents minéraux de la suite, leur relation au magma kimberlitique-hôte et au manteau lithosphérique cratonique archéen. L’étude des mégacris

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Bassahak, Jean. "Le complexe plutonique du Massif de Kogue (Poli-nord Cameroun) : Pétrologie, géochimie, pétrologie structurale, sa place dans le plutonisme de la chaîne panafricaine au Nord Cameroun." Nancy 1, 1988. http://www.theses.fr/1988NAN10017.

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L'architecture, la mise en place et la pétrogénèse du Massif du Kogue (Poli, Nord Cameroun) s'intègrent dans l'évolution tectonique et plutonique de la zone mobile panafricaine du Nord Cameroun. Intrusion dans les formations métamorphiques de Poli, le complexe plutonique de Kogue est formé de deux unités constituées par deux lignées de différenciation magmatique, d'affinité calco-alcaline. L'agencement et l'analyse des trajectoires des fluidalités planaires soulignent une mise en place syntectonique sous forme de dome diapir dans un couloir de cisaillement. L'état rhéologique des magmas granit

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Johnson, Geoffrey I. (Geoffrey Ian). "The petrology, geochemistry and geochronology of the felsic alkaline suite of the eastern Yilgarn Block, Western Australia / Geoffrey I. Johnson." 1991. http://hdl.handle.net/2440/19697.

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Typescript (Photocopy)<br>Includes copies of 4 papers by the author as appendix 4 (v. 1)<br>Errata slip inserted<br>Bibliography: leaves 170-192 (v. 1)<br>2 v. : ill., maps ; 30 cm.<br>Title page, contents and abstract only. The complete thesis in print form is available from the University Library.<br>Thesis (Ph.D.)--Dept. of Geology and Geophysics, University of Adelaide, 1992

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Shamberger, Patrick J. "Leucocratic & gabbroic xenoliths from Hualālai Volcano, Hawaiʻi /". 2004. http://hdl.handle.net/10125/10461.

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Scogings, Andrew John. "Alkaline intrusives from the Tugela terrane, Natal metamorphic province." Thesis, 1991. http://hdl.handle.net/10413/11162.

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Three gneissose alkaline granitoid intrusives at Ngoye, Bulls Run and Wangu are described. They are located within the Nkomo Nappe of the Tugela Terrane, near the northern margin of the Natal Metamorphic Province. The Ngoye Complex comprises alkaline granites, with minor syenite and monzodiorite phases. According to modal am geochemical criteria the Ngoye granites range from peraluminous (muscovite-bearing), through metaluminous (biotite- and/or hornblende-bearing), to peralkaline (riebeckite-, aegirine- and magnetite-bearing). The granites are A-types according to their modal and geochemical

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Schrader, Christian Michael. "Geochronology and geology of the Pebble Cu-Au-Mo porphyry and the sill Au-Ag epithermal deposits, southwest Alaska." 2001. http://purl.galileo.usg.edu/uga%5Fetd/schrader%5Fchristian%5Fm%5F200112%5Fms.

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Slagel, Matthew M. "Experimental melting of phlogopite-calcite assemblages : applications to the evolution and emplacement of silicocarbonatite magmas in the crust /." 1999. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:9943118.

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Quelhas, Pedro Moniz. "Petrology and geochemistry of the igneous rocks from Macao (South China) : Tectono-magmatic implications." Doctoral thesis, 2019. http://hdl.handle.net/10451/44158.

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The territory of Macao is composed of several granitic intrusions belonging to one of the biggest granite provinces in the world, the Southeast China Magmatic Belt (SCMB), located in the southeast (SE) area of the Cathaysia Block. The SCMB is known by the occurrence of large volumes of Mesozoic magmatic rocks (over 90% are granitic rocks and equivalent volcanic rocks with minor basalts), occupying a total outcrop area of nearly 200.000 km2. The geology of Macao (~30 Km2) is dominated by granitic rocks displaying a wide range of textural, mineralogical and chemical features, making it an ideal

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Chaoka, Thebeyame R. "The geology, petrology and geochemistry of the Kanye volcanics and Nnywane Formation : Ramotswa area, southeast Botswana /." 1988. http://collections.mun.ca/u?/theses,146773.

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Christodoulou, C. (Constaninos). "Petrology of the plutonic rocks of the Macquarie Island Complex / C. Christodoulou." 1990. http://hdl.handle.net/2440/19657.

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Maps on 2 folded leaves in pocket<br>Includes bibliography (25 leaves)<br>ca 400 leaves in various foliations : ill. (some col.), maps ; 31 cm.<br>Title page, contents and abstract only. The complete thesis in print form is available from the University Library.<br>Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1992

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Freeman, Lauren Anne. "The nature of hydrothermal fluids associated with granite-hosted, polymetallic mineralisation in the Eastern lobe of the bushveld complex." Thesis, 1998. https://hdl.handle.net/10539/24747.

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A thesis submitted in fulfilment of the requirements for the degree of PhD in Geology< University of the Witwatersrand.<br>Numerous small base-metal deposits occur in the acidic rocks of the Bushveld Complex, and modern exploration programs are currently re-examining this metallotect in an attempt to refine the current working hypothesis for mineralisation in these granites. The hypothesis proposed for the origin of mineralisation is multifaceted, encompassing both spatial and temporal relationships between at least three episodes of ore formation. The first episode of mineralisation (typified

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Rahilly, Kristen Elizabeth. "The Forsterite-Anorthite-Albite system at 5 kb pressure." 2010. http://hdl.handle.net/10090/15194.

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