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Dissertations / Theses on the topic 'Fluid inclusion'

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Published: 4 June 2021

Last updated: 25 July 2025

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1

Becker, Stephen Paul. "Fluid Inclusion Characteristics in Magmatic-Hydrothermal Ore Deposits." Diss., Virginia Tech, 2007. http://hdl.handle.net/10919/28318.

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Magmatic-hydrothermal ore deposits are formed in association with aqueous fluids that exsolve from hydrous silicate melts during ascent and crystallization. These fluids are invariably trapped as inclusions in vein-filling minerals associated with hydrothermal fluid flow, and their composition may be modeled based on the H₂O-NaCl system. Thus, if we know the pressure-volume-temperature-composition (PVTX) properties of H₂O-NaCl solutions, it is possible to interpret the PTX trapping conditions, which is important for understanding the processes leading to the generation of the hydrothermal syst

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2

Henderson, Iain Henry Campbell. "Fluid pressure variations in quartz veins, Pyrenees, France : fluid inclusion and cathodoluminescence studies." Thesis, University of Leeds, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.483635.

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3

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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4

Fall, Andras. "Application of fluid inclusions in geological thermometry." Diss., Virginia Tech, 2008. http://hdl.handle.net/10919/30265.

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Many geologic processes occur in association with hydrothermal fluids and some of these fluids are eventually trapped as fluid inclusions in minerals formed during the process. Fluid inclusions provide valuable information on the pressure, temperature and fluid composition (PTX) of the environment of formation, hence understanding PTX properties of the fluid inclusions is required. The most important step of a fluid inclusion study is the identification of Fluid Inclusion Assemblages (FIA) that represent the finest (shortest time duration) geologic event that can be constrained using fluid i

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5

Stoffell, B. "Metal transport and deposition in hydrothermal fluids : insights from laser ablation microanalysis of individual fluid inclusion." Thesis, Imperial College London, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.504926.

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6

Schmatz, Joyce [Verfasser]. "Grain-boundary – fluid inclusion interaction in rocks and analogues / Joyce Schmatz." Aachen : Hochschulbibliothek der Rheinisch-Westfälischen Technischen Hochschule Aachen, 2011. http://d-nb.info/101649324X/34.

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7

Levasseur, Randy. "Fluid inclusion studies of rare element pegmatites, South Platte District, Colorado." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ30962.pdf.

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8

Westerman, Jonathan Mark. "Fluid inclusion planes in selected granitic rocks of the British Isles." Thesis, Kingston University, 1995. http://eprints.kingston.ac.uk/20590/.

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When hydrothermal fluids flow through microfractures in quartz, they effectively heal (anneal) them to produce Fluid Inclusion Planes (FIPs). These FIPs are viewed as a three dimensional plane or array of secondary fluid inclusions and may be used to relate brittle deformation associated with tectonic, thermal and hydraulic stresses to contemporaneous hydrothermal events. In this study, FIPs have been interpreted in granitic quartz from various geological settings. Analysis of the FIPs includes recording their orientation, the morphological characteristics of both the FIPs and the inclusions c

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9

Christoula, Maria. "Fluid inclusion geochemistry of selected epigenetic, low temperature mineralization in the U.K." Thesis, Imperial College London, 2002. http://hdl.handle.net/10044/1/7326.

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10

Ting, Wupao. "A fluid and solid inclusion study of the Sukulu carbonatite complex, Uganda." Thesis, Kingston University, 1994. http://eprints.kingston.ac.uk/20577/.

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The thesis consists of 8 chapters. The first Chapter gives an introduction to carbonatites and outlines the general aims of this study. The general geology of Sukulu, the methodology used in this research, and previous work are presented in Chapter 2. Detailed descriptions and analytical results on the principal minerals are given in Chapter 3. Chapters 4 and 5 focus on aqueous and solid inclusions in apatite, and detailed descriptions, microthermometric results and interpretations are presented. Determination of oxygen and carbon stable isotope compositions and their interpretations are cover

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11

Ferrero, Silvio. "ANATECTIC MELTING IN A METAPELITIC SYSTEM: A FLUID AND MELT INCLUSION STUDY." Doctoral thesis, Università degli studi di Padova, 2010. http://hdl.handle.net/11577/3426976.

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Abstract In this thesis, a melt and fluid inclusion study was performed to investigate both anatectic melt and fluid phase during anatexis of metapelitic rocks, by studying samples from two different geological settings, the khondalites of the Kerala Khondalite Belt, India, and the granulitic enclaves from El Hoyazo, Neogene Volcanic Province, Spain. In khondalites (garnet-sillimanite-cordierite granulite/gneiss), melt inclusions (MI), interpreted as containing anatectic melt, were found for the first time in peritectic minerals from classic regionally metamorphosed metapelitic migmatites,

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12

Stephenson, Sarah K. Nabelek Peter Igor. "Fluid inclusion evidence for the nature of fluids associated with recrystallization of quartzites in the EJB contact Aureole, California." Diss., Columbia, Mo. : University of Missouri--Columbia, 2009. http://hdl.handle.net/10355/5338.

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The entire thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file; a non-technical public abstract appears in the public.pdf file. Title from PDF of title page (University of Missouri--Columbia, viewed on January 15, 2010). Thesis advisor: Dr. Peter Nabelek. Includes bibliographical references.

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13

Mathieu, Jordan-Paul. "CHARACTERISTICS OF DIAGENETIC FLUIDS AFFECTING TWO MAJOR CAR-BONATE UNITS ON VICTORIA ISLAND, NORTHWEST TERRITORIES." Thesis, Laurentian University of Sudbury, 2014. https://zone.biblio.laurentian.ca/dspace/handle/10219/2134.

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Diagenetic histories of Proterozoic and Paleozoic carbonate strata on Victoria Island, in the Canadian arctic, are poorly understood, and their potential to be associated with base metals or petroleum is unknown. Using fluid inclusion and geochemical techniques, it was determined that the diagenetic fluid compositions of two major carbonate units, the Wynniatt Formation and the “Victoria Island formation”, were largely controlled by fluid-rock reactions in reservoirs and by mixing of multiple fluids. Diagenesis of the Wynniatt Formation resulted from the progression from a shale-dominant fluid

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14

Kar, Adityamoy. "Fluid inclusion and trace element studies of the gem pegmatites of Mt. Antero, Colorado." Thesis, This resource online, 1991. http://scholar.lib.vt.edu/theses/available/etd-02132009-170725/.

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15

Negonga, Lisias. "Geochemistry, stable isotopes and fluid inclusion studies of the Otjikoto gold deposit, Central Namibia." Master's thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/29190.

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The Otjikoto gold deposit is located within the Damara Orogenic Belt which is part of the system of Pan-African mobile belts. The Damara Belt is a northwest trending orogenic belt which formed through sequences of spreading, rifting, subduction and from continental collision between the Congo, Kalahari and Rio Delta Plata Cratons between 900 Ma and 450 Ma. Mineralisation at Otjikoto is hosted by a group of metamorphic rocks which consist of biotite schists from the Okonguarri Formation, albitites from the Oberwasser member and marble units from the Okawayo member. The gold mineralization occur

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16

Guerci, Alain. "Modélisation géochimique des interactions fluides-roches et du comportement de l'uranium : application à des paléo-altérations hydrothermales, et à l'environnement des sites miniers." Vandoeuvre-les-Nancy, INPL, 1998. http://docnum.univ-lorraine.fr/public/INPL_T_1998_GUERCI_A.pdf.

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Les paléo-interactions fluides-roches dans les granites, plus particulièrement la formation des fentes alpines, des épisyénites, des minerais d'U épisyénitiques et leur altération ultérieure, ont été modélisées grâce au code de calcul géochimique EQ3/6. Une version d'EQ3/6 gérant les pressions élevées a servi à modéliser l'évolution des paragenèses dans les fentes alpines intragranitiques en utilisant comme contraintes, la composition chimique détaillée d'inclusions fluides (micro-analyse après écrasement). La minéralogie principale des fentes (quartz-chlorite) a été reproduite après une chute

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17

Guilhaumou, Nicole. "Apport de l'étude des inclusions fluides intracristallines à la diagénèse, l'anchizone et les minéralisations associées." Orléans, 1989. http://www.theses.fr/1989ORLE2010.

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Etudes methodologiques concernant l'analyse non destructive des fractions volatiles et des hydrocarbures liquides pieges dans les inclusions fluides par des methodes ponctuelles et non destructives comme la microspectrometrie infra-rouge et raman et la microfluorometrie, et d'autre part la mesure des changements de volume et de composition lors de surchauffes sous pression de confinement dans les inclusions de la fluorine. Les apports originaux des etudes d'inclusions fluides a la connaissance des circulations de fluides dans les bassins sedimentaires et pour la definition des conditions de de

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18

Cloete, Maret. "Modelling of non-Newtonian fluid flow through and over porous media with the inclusion of boundary effects." Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/80240.

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Thesis (PhD)--Stellenbosch University, 2013.<br>ENGLISH ABSTRACT: Different generalized Newtonian fluids (where the normal stresses were neglected) were considered in this study. Analytical expressions were derived for time independent, fully developed velocity profiles of Herschel-Bulkley fluids (including the simplifications thereof: Newtonian, power law and Bingham plastic fluids) and Casson fluids through open channel sections. Both flow through cylindrical pipes (Hagen-Poiseuille flow) and parallel plates (plane Poiseuille flow) were brought under consideration. Equations were deriv

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19

Siljeström, Sandra. "Single fluid inclusion analysis using ToF-SIMS : Implications for ancient Earth biodiversiy and paleoenvironment studies." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-54909.

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When and how life first emerged on the Earth is an area of intense research. Signs of the first life on Earth, including morphological fossils, are scarce and hard to interpret. An alternative approach is to study organic biomarkers, which are molecular fossils commonly considered as bona fide biosignatures. The main objective of the project is to develop an approach for analysis of single oil-bearing fluid inclusions and most importantly the detection of organic biomarkers in these inclusions. Analysis of oil-bearing fluid inclusions is advantageous since the inclusions may provide an unconta

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20

Ellershaw, Angus. "Fluid inclusion, petrographic and sulphur isotope investigations into Luxemburg mineral deposits, Curnamona Province, South Australia /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbe457.pdf.

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21

Markham, Jennifer Lynn. "Fluid History of the Peach Bottom Slate and Adjacent Units, Southeastern Pennsylvania." Bowling Green State University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1245726188.

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22

OGLIALORO, EDUARDO. "“THE MAGMA PLUMBING SYSTEM OF THE RIFT VOLCANISM ACTIVITY IN EL HIERRO, CANARY ISLANDS: FLUID INCLUSION, AND PETROLOGICAL STUDIES”." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2017. http://hdl.handle.net/10281/153284.

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i) L’eterogeneità geochimica della litosfera al di sotto di El Hierro Studi geochimica dei basalti di isola oceanica (OIB) offrono I mezzi principali per la comprensione dell’etogeneità del mantello attraverso la segnatura di isotopi di Sr-Nd-Pb a lungo termine (> 1 Ga) e definiscono i relativi arricchimenti di elementi incompatibili dei basalti medio oceanici. Precedenti studi riportano dati relativi a isotopi radiogenici per basalti alcalini delle isole di La Palma ed El Hierro, e più in generale delle isole Canarie. I dati raccolti con caratterizzazione petrografica, spettroscopia Raman e

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23

Anderson, Michael Richard. "A fluid inclusion and isotopic study of gold-bearing veins in the Transvaal Sequence, South Africa." Thesis, Imperial College London, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321197.

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24

Bradley, Mark Alan 1958. "Vein mineralogy, paragenetic sequence and fluid inclusion survey of the Silver district, La Paz Co., Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/558062.

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25

Henry, Adam T. "Petrologic and Fluid Inclusion Constraints on the Tectonic Evolution of the Manhattan Prong, Southeastern New York." Thesis, Virginia Tech, 1997. http://hdl.handle.net/10919/36855.

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The results of a combined mineral equilibria and fluid inclusion study show that the Manhattan Prong, southeastern New York, has experienced multiple metamorphic events. Two episodes of intrusion, separated by approximately 100 million years, have superimposed contact aureoles on the Taconic regional metamorphic gradient in the northeastern Manhattan Prong and have modified the regional assemblage to different degrees. The assemblage Sil-Bt-Grt-Qtz-Pl+Ksp+Ms in regionally metamorphosed Manhattan Schist records P-T conditions of 4-5 kbar and 650-700 oC. Garnet porphyroblasts, homogenous with

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26

Wang, Can Sheng. "The Jianfengling granite complex and the associated polymetallic mineralisation, Hunan Province, P.R. China." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.241274.

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27

Castles, Megan Erin. "Determining the Geometry and Former Extent of the North Mountain Thrust from Fluid Inclusion and Microstructural Analysis." Bowling Green State University / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1269223700.

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28

Zhu, Lichun. "An isotopic and fluid inclusion study of the Rock Canyon Creek, fluorite-REE deposit, southeastern British Columbia." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0015/MQ52689.pdf.

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29

Stevens, Kirk. "Fluid inclusion and geological studies on the Zn-Pb-Cu vein system at Lemieux Dome, Gaspe, Quebec." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65412.

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30

Siseho, Kamwi Rector. "Constraints on the genesis of the Sandamap gold prospect, Namibia: fluid inclusion, geochronology and stable isotope studies." University of the Western Cape, 2020. http://hdl.handle.net/11394/7246.

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Philosophiae Doctor - PhD<br>The Sandamap gold prospect is a metaturbidite shear zone-hosted gold mineralization located in the Neoproterozoic Damara Orogen 30 km northwest of the town of Usakos in Namibia with an estimated gold content of 240 000 t at 3.6 g/t up to 40 m below surface. This research project was aimed at constraining the age, crustal level of formation, pressure-temperature conditions during formation, sources of the mineralizing fluids, and by implication, the metal sources of the Sandamap gold mineralization. Fluid inclusion, geochronological and isotopic studies were carried

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31

Proctor, Briony. "The tectonic evolution of the Cape Fold Belt: constraints from fluid inclusion characteristics in syntectonic quartz veins." Thesis, Rhodes University, 2017. http://hdl.handle.net/10962/8019.

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Syn-tectonic quartz veins formed along faults, folds and tension gashes in rocks of the Cape Supergroup (CSG) of the central Cape Fold Belt (CFB) comprise mainly hydrous saline fluids. These veins may also contain CO₂ Syn-tectonic quartz veins formed along faults, folds and tension gashes in rocks of the Cape Supergroup CO₂ , or CH4 and CO₂, or neither CO₂ nor CH4. The majority of inclusions are two-phase and fluid rich, and the most common fluid composition is H2O-NaCl. The final melting temperature, and therefore salinity, differs very little across different structures (fluids in all struct

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32

Lacek, William Joseph. "Fluid History of the Sideling Hill Syncline, Hancock County, Maryland." Bowling Green State University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1435009185.

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33

Zajacz, Zoltán. "Mass transfer during volatile exsolution in magmatic systems : insights trough methodological developments in melt and fluid inclusion analysis /." Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17254.

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34

Laurent, Dimitri. "Marqueurs de la dynamique des fluides associée à l'enfouissement des bassins sédimentaires : Exemples du Bassin Permien de Lodève (France) et du North Viking Graben (Mer du Nord)." Thesis, Montpellier, 2015. http://www.theses.fr/2015MONTS170/document.

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Ce travail porte sur la caractérisation de la source et de la dynamique des fluides de bassin au cours de leur chargement à travers deux exemples complémentaires de demi-grabens tardi-orogéniques pétroliers : Le Bassin Permien de Lodève, aujourd'hui à l'affleurement et un bassin jurassique enfouis dans le North Viking Graben (Mer du Nord). Le cœur de la thèse concerne le Bassin de Lodève où, à partir d'une approche pluridisciplinaire intégrée, nous avons caractérisé l'architecture des minéralisations (Ba, F, Cu, Pb) piégées dans un réseau paléokarstique alimenté par les failles syn-rift, dans

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35

Renard, Stéphane. "Rôle des gaz annexes sur l'évolution géochimique d'un site de stockage de dioxyde de carbone : application à des réservoirs carbonatés." Thesis, Vandoeuvre-les-Nancy, INPL, 2010. http://www.theses.fr/2010INPL025N/document.

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La capture et le stockage géologique du CO2 constituent une option importante de limitation des émissions de gaz à effet de serre au niveau des pôles industriels et des centrales de production d’énergie. Les gaz capturés à l’issu de ces chaînes de production ne sont pas constitués de CO2 pur mais contiennent une fraction (jusqu’à 10 %) de gaz annexes qui sont essentiellement Ar, N2, SOx et NOx. Ces gaz étant pour la plupart très réactifs il est essentiel de connaître leur impact sur les conditions physico-chimiques du réservoir géologique d’accueil, ainsi que sur l’environnement dans le cas d’

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36

Majidi, Seyyed Hojjat. "Modeling of air entrainment and oxide inclusion formation during pouring of metal castings." Diss., University of Iowa, 2018. https://ir.uiowa.edu/etd/6611.

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Oxide inclusions are among the most commonly reported defects in ferrous and non-ferrous castings. They affect the surface quality, machinability, and mechanical performance of a cast part. Air entrainment during mold filling is the main source of the oxygen that is consumed in inclusion formation. A quantitative understanding of the formation mechanisms or the prediction of final amounts and locations of oxide inclusions in metal castings is not available. Ductile iron experiments are conducted to study the formation of oxide inclusions during pouring. Oxide inclusions are measured by serial

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37

ESPOSITO, ROSARIO. "Geochemical study of the Solchiaro (Procida Island, Campi Flegrei) eruptive products by microthermometry and microanalysis of fluid and melt inclusions." Doctoral thesis, Università degli Studi di Napoli Federico II, 2010. http://hdl.handle.net/10281/349383.

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In this study is presented the work I have done during the 4 years of a PhD program that was part of the internationalization programme of the Italian research system approved by the Ministero della Ricerca e dell’Università (MIUR) between the Università degli Studi di Napoli “Federico II”, (Dipartimento di Scinze della Terra) and the Virginia Polytechnic Institute and State University (Department of Geosciences). 107 selected MI, 77 open glasses, 80 olivines and 7 bulk rocks (from 4 representative samples of Solchiaro eruption) were analyzed for major/trace element and volatiles. Mostly, oli

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38

Cattalani, Sergio 1960. "A fluid inclusion and stable isotopic study of the St. Robert, W-Ag-Bi vein deposit, Eastern Townships, Quebec /." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63786.

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39

Penhall, John Lachlan. "A fluid inclusion and sulphur isotope study of epigenetic copper mineralisation in the Bimbowrie area, Olary Domain, South Australia /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbp399.pdf.

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Cline, Jean Schroeder 1948. "The sixteen-to-one epithermal silver-gold deposit, Esmeralda County, Nevada: a wall rock alteration and fluid inclusion study." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558052.

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41

Bergström, Sara. "Fluid inclusions and geochemistry of the Peña del Seo W-deposit, northwest Spain : Controlling mechanisms for tungsten deposition." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-78194.

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The Peña del Seo tungsten deposit in northwestern Spain is situated in the tin (Sn)-tungsten (W) metallogenic province of Europe − one of the richest tin-tungsten (tantalum-lithium) mineral provinces in the world. The European Union’s current goal is to become self-sufficient of these commodities in the near future and the iTARG3T project was launched in order to improve the understanding and provide innovative exploration methods of these types of deposits. This master thesis will contribute to the iTARG3T project. The aim was to determine which physico-chemical conditions (temperature, press

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42

Curti, Enzo. "Isotope geochemistry and fluid inclusion studies on the late metamorphic gold-quartz veins of the Monte Rosa area, northwestern alps, Italy : the origin of metals and fluids /." Zurich : E.T.H, 1987. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=8263.

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43

Mosser, Kevin Lynn. "Mineralogy, paragenesis, and fluid inclusion relationships of the hydrothermal ore deposits at Florida Mountain, Carson mining district, Owyhee County, Idaho." Thesis, The University of Arizona, 1991. http://hdl.handle.net/10150/144647.

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Exploration on Florida Mountain in southwestern Owyhee County, Idaho has defined four separate Au-Ag-Se orebodies. These deposits differ greatly in size, shape, grade, and metal ratios. However, all four are related to the same episode of epithermal vein mineralization. Ore deposition was associated with an active geothermal field related to a series of Mid-Miocene (15.2 to 16.6 m.y.a.) silicic domes and flows. Hydrothermal fluids of meteoric origin were localized along NW-trending faults and leached their constituents from the surrounding rocks. Metals were transported as complexes of sulfur

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44

Fadipe, Oluwaseun Adejuwon. "Reservoir quality, structural architecture, fluid evolution and their controls on reservoir performance in block 9, F-O gas field, Bredasdorp Basin, offshore South Africa." Thesis, University of the Western Cape, 2012. http://hdl.handle.net/11394/4005.

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Philosophiae Doctor - PhD<br>The use of integrated approach to evaluate the quality of reservoir rocks is increasingly becoming vital in petroleum geoscience. This approach was employed to unravel the reason for the erratic reservoir quality of sandstones of the F-O gas field with the aim of predicting reservoir quality, evaluate the samples for presence, distribution and character of hydrocarbon inclusions so as to gain a better understanding of the fluid history. Information on the chemical conditions of diagenetic processes is commonly preserved in aqueous and oil fluid inclusion occu

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45

Buckroyd, Clara Catherine. "Development of the 213nm UV laser ablation ICP-MS technique for fluid inclusion microanalysis and application to contrating magamtic-hydrothermal systems." Thesis, Imperial College London, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.497941.

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46

Arkadakskiy, Serguey Viktorov. "Fluid inclusion and stable isotopic study of precious and base metal veins from the Coeur d'Alene Ag-Pb-Zn district, Idaho, USA." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0002/MQ59773.pdf.

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47

Pyanoe, Dominic. "Fluid inclusion and metal ratio analysis of cordilleran Pb-Zn-Cu-(Ag-Au) veins of the Montezuma district| Summit County Colorado, USA." Thesis, Colorado State University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=1606517.

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<p> Evidence from fluid inclusion microthermometry in Pb-Zn-Cu-(Ag-Au) veins and district scale metal ratio zonation analysis indicate that the Cordilleran veins of the Montezuma mining district Summit County, Colorado, USA are indicative of subepithermal setting about a central hydrothermal source. Cordilleran-type polymetallic mineralization is a class of ore deposits that are spatially and temporally related to felsic igneous centers and can also be genetically related to porphyry mineralization (Fontboté and Bendezú, 2009). At Montezuma, the Teritary-aged Montezuma Stock is c

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48

Baker, Robin Masuko. "Study of the chronology and regional character of mineralization in veins of the bonanza area, Saguache County, Colorado, using fluid inclusion microscopy." The Ohio State University, 1987. http://rave.ohiolink.edu/etdc/view?acc_num=osu1406628783.

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49

Yoshida, Kenta. "Deep fluid characteristics in the subduction zone: A window from metamorphic quartz veins." 京都大学 (Kyoto University), 2015. http://hdl.handle.net/2433/199115.

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Ding, Junying. "The pH determination of palaeofluids : experimental and thermodynamic approach." Thesis, Nancy 1, 2010. http://www.theses.fr/2010NAN10106/document.

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Abstract:

Le but de cette étude est de développer une méthodologie permettant d'obtenir le pH des paléofluides du système H2O-CO2-HCO3--NaCl dans leurs conditions P-T de circulation. Ceci combine une approche expérimentale pour le calibrage d'une méthode analytique, la spectrométrie Raman et une modélisation numérique pour l'interprétation quantitative des équilibres de phase ou d'espèces chimiques. Les techniques analytiques utilisées en routine pour l'étude des inclusions fluides, comme la microthermométrie et la micro-spectrométrie Raman sont utilisées pour la détermination des concentrations. Les ex

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