Academic literature on the topic 'Fluid inclusion'

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Journal articles on the topic "Fluid inclusion"

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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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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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Van den Kerkhof, Alfons M., and Ulrich F. Hein. "Fluid inclusion petrography." Lithos 55, no. 1-4 (2001): 27–47. http://dx.doi.org/10.1016/s0024-4937(00)00037-2.

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Brown, Philip E. "Fluid inclusion research." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2149–50. http://dx.doi.org/10.1016/s0016-7037(97)83227-9.

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Brown, Philip E. "Fluid inclusion research." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2149. http://dx.doi.org/10.1016/s0016-7037(97)90192-7.

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Brown, Philip E. "Fluid inclusion research." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2149. http://dx.doi.org/10.1016/s0016-7037(97)90193-9.

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Brown, Philip E. "Fluid inclusion research." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2149. http://dx.doi.org/10.1016/s0016-7037(97)90194-0.

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FOSTER, R. P. "Fluid inclusion studies." Journal of the Geological Society 145, no. 1 (1988): 137–38. http://dx.doi.org/10.1144/gsjgs.145.1.0137.

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Moritz, Robert P. "Fluid inclusion research." Geochimica et Cosmochimica Acta 52, no. 6 (1988): 1743. http://dx.doi.org/10.1016/0016-7037(88)90247-5.

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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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Dissertations / Theses on the topic "Fluid 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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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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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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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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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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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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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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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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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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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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Books on the topic "Fluid inclusion"

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L, Atwood J., Davies J. E. D, and MacNicol D. D, eds. Inclusion compounds. Oxford University Press, 1991.

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H, Rankin A., and Alderton D. H. M, eds. A practical guide to fluid inclusion studies. Blackie, 1985.

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Landis, Gary P. Anomalous low-density wolframite and fluid inclusion control of density, evidence from fluid inclusion content of water and carbon dioxide. Dept. of the Interior, U.S. Geological Survey, 1990.

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Landis, Gary P. Anomalous low-density wolframite and fluid inclusion control of density, evidence from fluid inclusion content of water and carbon dioxide. Dept. of the Interior, U.S. Geological Survey, 1990.

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Landis, Gary P. Anomalous low-density wolframite and fluid inclusion control of density, evidence from fluid inclusion content of water and carbon dioxide. Dept. of the Interior, U.S. Geological Survey, 1990.

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Landis, Gary P. Anomalous low-density wolframite and fluid inclusion control of density, evidence from fluid inclusion content of water and carbon dioxide. Dept. of the Interior, U.S. Geological Survey, 1990.

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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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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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Book chapters on the topic "Fluid inclusion"

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Dolson, John. "Using Fluid Inclusion Data in Exploration." In Understanding Oil and Gas Shows and Seals in the Search for Hydrocarbons. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-29710-1_7.

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Blamey, Nigel J. F., and Alan G. Ryder. "Hydrocarbon Fluid Inclusion Fluorescence: A Review." In Reviews in Fluorescence. Springer New York, 2009. http://dx.doi.org/10.1007/978-0-387-88722-7_13.

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Tazreiter, Claudia, Leanne Weber, Sharon Pickering, Marie Segrave, and Helen McKernan. "Processes of Reception and Inclusion in Australia." In Fluid Security in the Asia Pacific. Palgrave Macmillan UK, 2016. http://dx.doi.org/10.1057/978-1-137-46596-2_9.

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Mitchell, Thomas M., Jose M. Cembrano, Kazuna Fujita, et al. "Fluid Inclusion Evidence of Coseismic Fluid Flow Induced by Dynamic Rupture." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch3.

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Hansteen, Thor H., and Andreas Klügel. "5. Fluid Inclusion Thermobarometry as a Tracer for Magmatic Processes." In Minerals, Inclusions And Volcanic Processes, edited by Keith D. Putirka and Frank J. Tepley III. De Gruyter, 2008. http://dx.doi.org/10.1515/9781501508486-006.

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Mekki, Mouna El, Claire Ramboz, Laurent Perdereau, Kirill Shmulovich, and Lionel Mercury. "Lifetime of Superheated Water in a Micrometric Synthetic Fluid Inclusion." In Metastable Systems under Pressure. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3408-3_20.

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Quesnel, Benoît, Christophe Scheffer, and Georges Beaudoin. "The Light Stable Isotope (Hydrogen, Boron, Carbon, Nitrogen, Oxygen, Silicon, Sulfur) Composition of Orogenic Gold Deposits." In Isotopes in Economic Geology, Metallogenesis and Exploration. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_10.

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AbstractOrogenic gold deposits formed in various terranes of most ages since the Paleoarchean and generally consist of quartz veins hosted in shear zones formed at the ductile brittle transition under greenschist to lower amphibolite metamorphic conditions. Vein mineralogy is dominated by quartz with various amounts of silicates, carbonates, phyllosilicates, borates, tungstates, sulfides, and oxides. The isotopic composition of these minerals and fluid inclusions has been investigated since the 1960s to constrain the characteristics of orogenic fluid systems involved in the formation of gold d
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Huston, David L., Robert B. Trumbull, Georges Beaudoin, and Trevor Ireland. "Light Stable Isotopes (H, B, C, O and S) in Ore Studies—Methods, Theory, Applications and Uncertainties." In Isotopes in Economic Geology, Metallogenesis and Exploration. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_8.

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AbstractVariations in the abundances of light stable isotopes, particularly those of hydrogen, boron, carbon, oxygen and sulfur, were essential in developing mineralization models. The data provide constraints on sources of hydrothermal fluids, carbon, boron and sulfur, track interaction of these fluids with the rocks at both the deposit and district scales, and establish processes of ore deposition. In providing such constraints, isotopic data have been integral in developing genetic models for porphyry-epithermal, volcanic-hosted massive sulfide, orogenic gold, sediment-hosted base metal and
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Spitzenberger, Andy, Katrin Bauer, and Rüdiger Schwarze. "Reactive Cleaning and Active Filtration in Continuous Steel Casting." In Multifunctional Ceramic Filter Systems for Metal Melt Filtration. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-40930-1_17.

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AbstractBasic fluid dynamic processes of melt filtration have been investigated in order to increase the performance and efficiency of filtration systems in steelmaking, especially for continuous steel casting. Numerical simulations have been performed to investigate the interactions between filter structures and the mean melt flow, the development of endogenous non-metallic inclusion (NMI) populations in the flow, and inclusion removal from the melt. For this purpose, Euler–Lagrange models of the particle-laden flow have been developed. As a major finding, the reactive cleaning process of the
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Li, Yanlong, Lifeng Zhang, and Ying Ren. "Fluid Flow, Alloy Dispersion and Inclusion Motion in Argonstirred Steel Ladles." In Celebrating the Megascale. John Wiley & Sons, Inc., 2014. http://dx.doi.org/10.1002/9781118889657.ch66.

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Conference papers on the topic "Fluid inclusion"

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Li, Hui, Junjia Fan, Xiaojiu Xu, Lijun Wang, and Meng Lei. "Fluid Inclusion Detection Based on Improved YOLOX." In 2023 4th International Conference on Computer, Big Data and Artificial Intelligence (ICCBD+AI). IEEE, 2023. http://dx.doi.org/10.1109/iccbd-ai62252.2023.00070.

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Kirschenmann, Jacob, Kenneth Hart, Timothy Homewood, Jessica Wilmot, and Matthew J. Severs. "FLUID INCLUSION INVESTIGATION OF SHAWANGUNK MINERAL DEPOSITS." In 59th Annual GSA Northeastern Section Meeting - 2024. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024ne-397628.

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Krieger, F. W., P. J. Eadington, and M. Lisk. "Fluid Inclusion Data for Rw in Reserves Estimation." In SPE Asia Pacific Oil and Gas Conference. Society of Petroleum Engineers, 1996. http://dx.doi.org/10.2118/36975-ms.

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Xu, Jinming, Bin Liu, and Qiang Xie. "Microscopic Heterogeneity of Fluid Inclusion Distributions in Rocks." In GeoCongress 2008. American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40972(311)26.

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Stoller, Patrick, Jaro Ricka, Martin Frenz, and Yves Kruger. "Ultra-short pulse lasers in geological fluid inclusion analysis." In 2007 European Conference on Lasers and Electro-Optics and the International Quantum Electronics Conference. IEEE, 2007. http://dx.doi.org/10.1109/cleoe-iqec.2007.4386316.

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Towbin, William Henry, Evan M. Smith, Ulrika F. S. D'Haenens-Johansson, and Daniel C. Jones. "Macle Diamonds: Primary Fluid Inclusion Entrapment Along the Twinning Plane." In International Kimberlite Conference. University of Alberta, 2024. http://dx.doi.org/10.29173/ikc4165.

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Mamedov, Sergey. "APPLICATIONS OF RAMAN SPECTROSCOPY TO SOLID AND FLUID INCLUSION PHASE IDENTIFICATION." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-394796.

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Dubosq, Renelle, Anna Rogowitz, David Schneider, Kevin Schweinar, and Baptiste Gault. "Fluid inclusion induced hardening in pyrite: Results from atom probe tomography." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.3515.

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Lima, Annamaria, Robert J. Bodnar, and Benedetto De Vivo. "Fluid and Melt Inclusion Evidence for Immiscibility at Somma Vesuvius Volcano (Italy)." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1558.

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Wan, Zhenzhu, Peter Jenden, Andreas Schmidt Mumm, and Khaled Arouri. "STABLE CARBON ISOTOPIC VARIATION OF FLUID INCLUSION GASES FOR CHARGE HISTORY ANALYSIS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319945.

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Reports on the topic "Fluid inclusion"

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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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Dilley, Lorie M. Methodologies for Reservoir Characterization Using Fluid Inclusion Gas Chemistry. Office of Scientific and Technical Information (OSTI), 2015. http://dx.doi.org/10.2172/1177790.

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Dilley, Lorie M., David Norman, and Lara Owens. Identifying Fracture Types and Relative Ages Using Fluid Inclusion Stratigraphy. Office of Scientific and Technical Information (OSTI), 2008. http://dx.doi.org/10.2172/933170.

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Lorie M. Dilley. Chemical Signatures of and Precursors to Fractures Using Fluid Inclusion Stratigraphy. Office of Scientific and Technical Information (OSTI), 2011. http://dx.doi.org/10.2172/1010306.

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Chi, G. Fluid compositions and temperature-pressure conditions of intrusion-related gold systems in southwestern New Brunswick - a fluid-inclusion study. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213694.

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Cattalani, S., and A. E. Williams-Jones. Geological and Fluid Inclusion Studies At the Saint-Robert Ag, W, Bi Deposit. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120388.

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Aulstead, K. L., and R. Spencer. Fluid Inclusion Evidence On the Diagenesis of the Manetoe Facies, Yukon and Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130032.

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Stevens, K. Mineral zoning and fluid inclusion studies in the Candego / Madeleine Mines area, Gaspe, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/130187.

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Chi, G., B. Dubé, and K. Williamson. Preliminary fluid-inclusion microthermometry study of fluid evolution and temperature-pressure conditions in the Goldcorp High-Grade zone, Red Lake mine, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213205.

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