Academic literature on the topic 'Fluid Inclusions'

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Journal articles on the topic "Fluid Inclusions"

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Moritz, Robert P., and Serge R. Chevé. "Fluid-inclusion studies of high-grade metamorphic rocks of the Ashuanipi complex, eastern Superior Province: constraints on the retrograde P–T path and implications for gold metallogeny." Canadian Journal of Earth Sciences 29, no. 10 (1992): 2309–27. http://dx.doi.org/10.1139/e92-180.

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The high-grade metamorphic rocks of the Ashuanipi complex have been the subject of a microthermometric fluid-inclusion study. Four types of fluid inclusions were observed: CO2-rich fluids; low-temperature, high-salinity H2O fluids; CH4 ± N2-rich fluids; and high-temperature, low-salinity H2O fluids. The regionally distributed CO2-rich fluids are the earliest fluids, and their calculated isochores indicate a clockwise post-peak metamorphic P–T–t path for the Ashuanipi complex. The low-temperature, high-salinity aqueous fluid inclusions are also distributed regionally and can be interpreted as l
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RANKIN, ANDREW H. "Fluid inclusions." Geology Today 5, no. 1 (1989): 21–24. http://dx.doi.org/10.1111/j.1365-2451.1989.tb00606.x.

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Cui, Kai, Yunwei Qu, Yuling Xie, Kejun Yang, and Zhaoqiang Huang. "Ore Genesis of the Langcun Porphyry W-Mo Deposit, South China: Constraints from Fluid Inclusion and H-O-S Isotopics." Minerals 15, no. 2 (2025): 109. https://doi.org/10.3390/min15020109.

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The Langcun W-Mo deposit, located in the Zhejiang Province of South China, is a medium-sized porphyry deposit. The ore bodies mainly occur in aplite, granite porphyry, and the contact zone with hornfels of the Nanhua System. Four stages of mineralization are recognized in the Langcun deposit, including the quartz–K-feldspar stage (stage I), quartz–sericite–molybdenite stage (stage II), quartz–chlorite–pyrite stage (stage III), and calcite stage (stage IV). Stages I and II are the main ore-forming stages for wolframite and molybdenite. The petrographic and microthermometric results show that fo
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Zolensky, Michael E., Robert J. Bodnar, Hisayoshi Yurimoto, et al. "The search for and analysis of direct samples of early Solar System aqueous fluids." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 375, no. 2094 (2017): 20150386. http://dx.doi.org/10.1098/rsta.2015.0386.

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We describe the current state of the search for direct, surviving samples of early, inner Solar System fluids—fluid inclusions in meteorites. Meteoritic aqueous fluid inclusions are not rare, but they are very tiny and their characterization is at the state of the art for most analytical techniques. Meteoritic fluid inclusions offer us a unique opportunity to study early Solar System brines in the laboratory. Inclusion-by-inclusion analyses of the trapped fluids in carefully selected samples will, in the immediate future, provide us detailed information on the evolution of fluids as they inter
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Velojić, Miloš, Rade Jelenković, and Vladica Cvetković. "Fluid Evolution of the Čukaru Peki Cu-Au Porphyry System (East Serbia) inferred from a fluid inclusion study." Geologia Croatica 73, no. 3 (2020): 197–209. http://dx.doi.org/10.4154/gc.2020.14.

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Čukaru Peki is a recently discovered copper-gold deposit in the Bor metallogenic zone in east Serbia. Three types of mineralization can be distinguished in this ore deposit: porphyry, high-sulphidation, and transitional epithermal type. This research was focused on fluid inclusion analysis of genetically different veins from the porphyry and the transitional zones of Čukaru Peki with an aim of better understanding the fluid evolution and mineralization processes in this system. Seven types of veins were identified in the porphyry zone of Čukaru Peki and four of these veins contained transparen
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Rosenbaum, Jeffrey M., Alan Zindler, and James L. Rubenstone. "Mantle fluids: Evidence from fluid inclusions." Geochimica et Cosmochimica Acta 60, no. 17 (1996): 3229–52. http://dx.doi.org/10.1016/0016-7037(96)00167-6.

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Srikantappa, C., and L. Venugopal. "Fluid Inclusions in Migmatites from Hunsur, Karnataka." Journal Geological Society of India 49, no. 5 (1997): 503–11. http://dx.doi.org/10.17491/jgsi/1997/490504.

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Abstract Fluid inclusion studies in migmatites around Hunsur document the presence of a) CO2-CH4, CO2 and CO2-H2O inclusions in paleosome, b) predominantly CO2 inclusions in leucosome and c) CO2 and low salinity aqueous inclusions in late pink granite. Chronological studies of CO2 inclusions in quartz grains from migmatites and their densities corresponding to Th maxima plus mineral P-T data for the regional metamorphism indicate that they are syn-migmatitic fluids. An internal origin of CO2 inclusions during the process of migmatization is envisaged.
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Huang, Wenqing, Pei Ni, Jungui Zhou, et al. "Fluid Inclusion and Titanite U-Pb Age Constraints on the Yuanjiang Ruby Mineralization in the Ailao Shan-Red River Metamorphic Belt, Southwest China." Canadian Mineralogist 60, no. 1 (2022): 3–28. http://dx.doi.org/10.3749/canmin.2100009.

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ABSTRACT The Yuanjiang marble-hosted ruby deposit lies in the central segment of the Ailao Shan metamorphic massif of the Ailao Shan-Red River metamorphic belt. The mineralizing fluid and age were characterized by detailed petrography, Raman spectroscopy, microthermometry, and in situ titanite laser ablation-inductively coupled plasma-mass spectrometry dating. Some fluid inclusions in the corundum show an interesting morphology with a diaspore crystal fully separating the whole inclusion into two smaller inclusions. This morphological feature can be explained by morphological ripening and subs
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Thankan, Silpa, V. Nandakumar, and S. Shivapriya. "Raman Spectroscopic Technique to Distinguish Constituents of Hydrocarbon-Bearing Fluid Inclusions of Kerala-Konkan Basin, Western offshore, India." Journal of Geosciences Research 8, no. 1 (2023): 1–6. http://dx.doi.org/10.56153/g19088-022-0096-21.

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Fluid inclusion studies have a great diversity of applications in exploration geology and are necessary tools in the determination of palaeotemperature and nature of fluids associated with the rocks in a basin. Using various fluid inclusion techniques such as petrography, microthermometry and Laser Raman Spectroscopy of fluid inclusions with Hydrocarbon fluid inclusions (HCFIs) help us to understand the generation potential of the basin. The representative micron sized fluid inclusions that intruded into the different geological formations of the KK-4C-A1well drilled by Oil and Natural Gas Cor
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Rabiei, M., G. Chi, E. G. Potter, et al. "Fluid evolution along the Patterson Lake corridor in the southwestern Athabasca Basin: constraints from fluid inclusions and implications for unconformity-related uranium mineralization." Geochemistry: Exploration, Environment, Analysis 21, no. 3 (2021): geochem2020–029. http://dx.doi.org/10.1144/geochem2020-029.

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The Patterson Lake corridor (PLC) in the southwestern margin of the Athabasca Basin hosts several high-grade uranium deposits. These deposits are located in the basement up to 900 m below the unconformity surface, raising questions about their affiliation with typical unconformity-related uranium (URU) deposits elsewhere in the basin. Based on cross-cutting relationships four pre- and three syn- to post-mineralization quartz generations were identified. Fluid inclusion analyses indicate that pre-mineralization fluids have salinities ranging from 0.2 to 27.2 wt% NaCl equiv. (avg. 9.0 wt%), wher
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Dissertations / Theses on the topic "Fluid Inclusions"

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Bigge, M. Ashley. "Investigations of petroleum-bearing fluid inclusions." Thesis, University of Newcastle Upon Tyne, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364805.

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Sterner, Steven Michael. "Geological applications of synthetic fluid inclusions." Diss., Virginia Polytechnic Institute and State University, 1989. http://hdl.handle.net/10919/54434.

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Vapor-saturated solubility relationships in the system NaCl-KCl-H₂0 have been determined by experimentally synthesizing fluid inclusions in quartz in the presence of known brine compositions and then measuring the dissolution temperatures of halite and/or sylvite daughter crystals within the inclusions using a microscope equipped with a heating stage. These data, along with other literature values have been used in a regression routine to generate a series of equations describing vapor-saturated solubility relations within the halite, sylvite and hydrohalite stability fields. These equations,
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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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Kelly, Jason. "Fluid flow through low permeability successions : the application of fluid inclusions." Thesis, University of Aberdeen, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.401364.

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Smith, Evan Mathew. "Fluid inclusions in fibrous and octahedrally-grown diamonds." Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/46301.

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My thesis puts forth new models for diamond formation that explain the difference between octahedral and fibrous diamond growth, as well as the difference between octahedral diamond growth in the lithospheric and the sublithospheric mantle. Diamond growth in the mantle involves reactions between carbon-bearing fluid and the host rocks it infiltrates. This fluid is sometimes included in diamond. Fluids in dendritically-grown, fibrous diamonds from Wawa, Superior craton, were analysed in a novel way, using transmission X-ray diffraction. The technique allows bulk analysis of daughter minerals w
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Lamadrid, De Aguinaco Hector M. "Geochemistry of fluid-rock processes." Diss., Virginia Tech, 2016. http://hdl.handle.net/10919/71350.

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When these fluids interact with the surrounding rocks, small aliquots of these fluids are trapped as imperfections in the crystal lattice and fractures of minerals. These microscopic features are called fluid and melt inclusions, and are one of the best tools available to probe, measure and determine the chemical and physical properties of crustal fluids. In the present study we examine new developments into our understanding of fluid-rock interactions using fluid and melt inclusion as tools to provide insights into the evolution of the Earth's crust from the deep continental crust to the surf
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Yue, Zhongqi Carleton University Dissertation Engineering Civil. "Mechanics of rigid disc inclusions in fluid saturated poroelastic media." Ottawa, 1992.

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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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Bobo, Emilie. "Contribution on the formation and the behaviors of fluid inclusions in crystals." Rouen, 2016. http://www.theses.fr/2016ROUES022.

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Ce manuscrit porte sur la caractérisation et l’étude de la formation des inclusions qui sont les impuretés principales restantes dans les cristaux après leur purification par cristallisation en solution. Le cas du Perchlorate d’Ammonium obtenu en solution aqueuse a été particulièrement étudié notamment sous différentes atmosphères (CO2, N2, O2). La formation des poches de solution dans les monocristaux a été directement observée au moyen d’un microscope. Les expériences ont mis en évidence la relation étroite entre la forte croissance de certaines faces des cristaux et la formation d’inclusion
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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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Books on the topic "Fluid Inclusions"

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M, Santosh, and Geological Society of India, eds. Fluid inclusions. Geological Society of India, 1988.

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Gostyayeva, Natalya. Implications of the fluid-inclusion motions in the Elder Creek porphyry copper system, Battle Mountain Mining District, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Gostyayeva, Natalya. Implications of the fluid-inclusion motions in the Elder Creek porphyry copper system, Battle Mountain Mining District, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Gostyayeva, Natalya. Implications of the fluid-inclusion motions in the Elder Creek porphyry copper system, Battle Mountain Mining District, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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G, Theodore Ted, Lowenstern Jacob B, and Geological Survey (U.S.), eds. Implications of fluid-inclusion motions in the Elder Creek porphyry copper system, Battle Mountain Mining District, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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G, Theodore Ted, Lowenstern Jacob B, and Geological Survey (U.S.), eds. Implications of fluid-inclusion motions in the Elder Creek porphyry copper system, Battle Mountain Mining District, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Rowan, E. Lanier. Homogenization temperatures and salinities of fluid inclusions from the Viburnum Trend, southeast Missouri, and the northern Arkansas zinc distict. U.S. Dept. of the Interior, U.S. Geological Survey, 1987.

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United States. National Aeronautics and Space Administration., ed. P-T conditions of deformation from fluid inclusions in mylonites. Dept. of Geology, University of Maryland, 1990.

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Goldstein, Robert H. Systematics of fluid inclusions in diagenetic minerals. SEPM, 1994.

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Rowan, E. Lanier. Stretching of fluid inclusions in fluorite at confining pressures up to one kilobar. U.S. Dept. of the Interior, Geological Survey, 1985.

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Book chapters on the topic "Fluid Inclusions"

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J. Bodnar, Robert. "Fluid Inclusions." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-39193-9_225-1.

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J. Bodnar, Robert. "Fluid Inclusions." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_225.

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Philippot, Pascal. "Fluid Inclusions." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_579-4.

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Philippot, Pascal. "Fluid Inclusions." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_579.

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Philippot, Pascal. "Fluid Inclusions." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_579.

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Philippot, Pascal. "Fluid Inclusions." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_579.

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Barker, Andy J. "Veins and fluid inclusions." In Introduction to Metamorphic Textures and Microstructures. Springer US, 1998. http://dx.doi.org/10.1007/978-1-4615-7291-6_11.

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Okrusch, Martin, and Hartwig E. Frimmel. "Fluid Inclusions in Minerals." In Springer Textbooks in Earth Sciences, Geography and Environment. Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-57316-7_12.

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Touret, J., and Sakiko N. Olsen. "Fluid inclusions in migmatites." In Migmatites. Springer US, 1985. http://dx.doi.org/10.1007/978-1-4613-2347-1_8.

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Crawford, M. L., and L. S. Hollister. "Metamorphic Fluids: The Evidence from Fluid Inclusions." In Advances in Physical Geochemistry. Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4896-5_1.

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Conference papers on the topic "Fluid Inclusions"

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Chen, Wei, Helmuth Sarmiento Klapper, and John Stevens. "Effects of Pitting and Inclusions on the Corrosion Fatigue of a CrMnN Stainless Steel." In CORROSION 2014. NACE International, 2014. https://doi.org/10.5006/c2014-4070.

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Abstract Pitting corrosion plays an important role in corrosion fatigue crack initiation and growth in austenitic stainless steels that are subject to dynamic loading in an aqueous corrosive environment. Non-metallic inclusions such as sulfides can lead to preferential dissolution and pit formation. Consequently, the cleanliness of austenitic stainless steels, as measured by levels of sulfides and other types of inclusions, strongly influences the material's susceptibility to pitting corrosion, and correspondingly, its corrosion fatigue performance. However, the synergistic effect of dynamic l
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Ye, Rong, and Youmin Bai. "Characteristics of Bayern Fluid Inclusions." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3024.

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Maffeis, Andrea, Simona Ferrando, Daniele Castelli, Chiara Groppo, and Maria Luce Frezzotti. "Evaluating Fluid-Host Post Entrapment Interaction in UHP Fluid Inclusions." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1697.

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Robbes, Anne-Sophie, Mona Pierrette Moret, and Carl Henderson. "EPMA ANALYSIS OF FLUID INCLUSIONS IN VOLCANIC ROCKS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318468.

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Abudayeh, Ahmad, and Tibor Guzmics. "Fluid and melt inclusions study from Jacupiranga carbonatite." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.20388.

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Rabiei, Morteza, Guoxiang Chi, Eric Potter, and Renfei Feng. "Tracking ore fluid pathways by in situ synchrotron-XRF analysis of fluid inclusions." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.3613.

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Klyukin, Yury I., and Robert J. Bodnar. "REVIEW OF FLUID AND MELT INCLUSIONS IN GEM MINERALS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281851.

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Li, Rongxi, Bangsheng Zhao, and Ahmed Khaled. "Correlation of Geochemistry of Gas between Fluid Inclusions and Reservoir." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1510.

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Moncada, Daniel. "Fluid Inclusions from Active and Fossil Hydrothermal System in Chile." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1829.

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Taylor, Sandra, Daniel Perea, Libor Kovarik, John Cliff, Daniel D. Gregory, and Timothy W. Lyons. "Ancient Seawater Compositions Recorded in Nanoscale Fluid Inclusions in Pyrite?" In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2575.

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Reports on the topic "Fluid Inclusions"

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Kingston, A. W., and O. H. Ardakani. Diagenetic fluid flow and hydrocarbon migration in the Montney Formation, British Columbia: fluid inclusion and stable isotope evidence. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330947.

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The Montney Formation in Alberta and British Columbia, Canada is an early Triassic siltstone currently in an active diagenetic environment at depths greater than 1,000 m, but with maximum burial depths potentially exceeding 5,000 m (Ness, 2001). It has undergone multiple phases of burial and uplift and there is strong evidence for multiple generations of hydrocarbon maturation/migration. Understanding the origin and history of diagenetic fluids within these systems helps to unravel the chemical changes that have occurred since deposition. Many cores taken near the deformation front display abu
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Kontak, D. J., S. Paradis, Z. Waller, and M. Fayek. Petrographic, fluid inclusion, and secondary ion mass spectrometry stable isotopic (O, S) study of Mississippi Valley-type mineralization in British Columbia and Alberta. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327994.

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A comprehensive study of Mississippi Valley-type base-metal deposits across the Canadian Cordillera was done to compare and contrast their features. Extensive dissolution of host rocks is followed by multiple generations of dolomite cements from early, low-temperature, fine-grained to coarser, higher temperature types that overlap with Zn-Pb sulfide minerals; late-stage calcite occludes residual porosity. Dolomite is generally chemically stoichiometric, but ore-stage types are often rich in Fe (<1.3 weight per cent FeO) with small sphalerite inclusions. Sphalerite-hosted fluid inclu
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David I. Norman and Joseph Moore. Gas Analysis of Geothermal Fluid Inclusions: A New Technology For Geothermal Exploration. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/822434.

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Tweedale, F., J. J. Hanley, D. J. Kontak, and N. Rogers. Methodology for solute characterization of fluid inclusions by petrographic and SEM/EDS complementary analysis. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296495.

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Boreham, C. J., D. S. Edwards, J. H. Sohn, P. Palatty, J. H. Chen, and A. J. Mory. Gas systems in the onshore Canning Basin as revealed by gas trapped in fluid inclusions. Geoscience Australia, 2020. http://dx.doi.org/10.11636/135207.

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Sloan, Jr., Richard Charles. Development and application of a mass spectrometric system to study volatile components of fluid inclusions. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/10152018.

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Sloan, R. C. Jr. Development and application of a mass spectrometric system to study volatile components of fluid inclusions. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/5148689.

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Stasiuk, L. D. Hydrocarbon fluid inclusions and free oils within basal Cambrian and Elk Point Group sandstones, southern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/220359.

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Sangster, D. F., and J. J. Carriere. Preliminary Studies of Fluid Inclusions in Sphalerite From the Robb Lake Mississippi Valley - Type Deposit, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132625.

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Carriere, J. J., and D. F. Sangster. Preliminary studies of fluid inclusions in sphalerite quartz and dolomite from Gayna River Mvt Deposit, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132786.

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