Relevant bibliographies by topics / Fluid inclusion stratigraphy

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
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Academic literature on the topic 'Fluid inclusion stratigraphy'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Fluid inclusion stratigraphy"

1

Norman, David I., Lorie Dilley, Kristie McLin, and Joseph N. Moore. "Applying fluid inclusion stratigraphy analyses to geothermal systems." Geochimica et Cosmochimica Acta 70, no. 18 (2006): A449. http://dx.doi.org/10.1016/j.gca.2006.06.902.

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2

Török, Kálmán. "Multiple fluid migration events and REE+Th mineralisation during Alpine metamorphism in the Sopron micaschist from the Eastern-Alps (Sopron area, Western Hungary)." Földtani Közlöny 150, no. 1 (2020): 45. http://dx.doi.org/10.23928/foldt.kozl.2020.150.1.45.

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Four fluid migration events were recorded during the Alpine metamorphism in the Sopron micaschist from the Grob gneiss series of the Lower Austroalpine Unit of the Eastern Alps near Sopron, using mineral chemistry data, geothermo-barometry and fluid inclusion studies.1. Tourmaline mineralisation in quartz veins and to some extent in the host rock. Similar mineral compositions in the quartz-tourmaline veins and in the host rock show equilibrium between fluid and the host rock. Geothermo-barometry gives 560-610oC temperature and 950-1230 MPa pressure for the formation of quartz-tourmaline veins
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3

Uemura, Ryu, Yudai Kina, Chuan-Chou Shen, and Kanako Omine. "Experimental evaluation of oxygen isotopic exchange between inclusion water and host calcite in speleothems." Climate of the Past 16, no. 1 (2020): 17–27. http://dx.doi.org/10.5194/cp-16-17-2020.

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Abstract. The oxygen and hydrogen isotopic compositions of water in fluid inclusions in speleothems are important hydroclimate proxies because they provide information on the isotopic compositions of rainwater in the past. Moreover, because isotopic differences between fluid inclusion water and the host calcite provide information on the past isotopic fractionation factor, they are also useful for quantitative estimation of past temperature changes. The oxygen isotope ratio of inclusion water (δ18Ofi), however, may be affected by isotopic exchange between the water and the host carbonate. Thus
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4

Körmös, Sándor, Georgina Lukoczki, and Félix Schubert. "Indication of hydrocarbon migration in the Western Mecsek Mountains evidenced by fluid inclusion chemostratigraphy." Földtani Közlöny 150, no. 4 (2020): 611. http://dx.doi.org/10.23928/foldt.kozl.2020.150.4.611.

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Primary and secondary hydrocarbon-bearing fluid inclusion (HCFI) assemblages occur in the Middle Triassic Lapis Limestone in the Szuadó Valley of the Western Mecsek Mts. The primary HCFIs were trapped in saddle dolomite crystals, and the secondary HCFIs were enclosed in calcite neospar and fracture-filling calcite. Solid bitumen is also present along fractures. The volatile compounds liberated from fluid inclusions are characterized by non-hydrocarbon and hydrocarbon species. The fluorescent properties of HCFIs, the occurrence of the solid bitumen, as well as the composition of inclusion oils
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Spadin, F., D. Marti, R. Hidalgo-Staub, et al. "Technical Note: How accurate can stalagmite formation temperatures be determined using vapour bubble radius measurements in fluid inclusions?" Climate of the Past Discussions 10, no. 5 (2014): 3689–713. http://dx.doi.org/10.5194/cpd-10-3689-2014.

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Abstract. Stalagmites are natural archives containing detailed information on continental climate variability of the past. Microthermometric measurements of fluid inclusion homogenisation temperatures allow determination of stalagmite formation temperatures by measuring the radius of stable laser-induced vapour bubbles inside the inclusions. A reliable method for precisely measuring the radius of vapour bubbles is presented. The method is applied to stalagmite samples for which the formation temperature is known. An assessment of the bubble radius measurement accuracy and how this error influe
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Spadin, F., D. Marti, R. Hidalgo-Staub, J. Rička, D. Fleitmann, and M. Frenz. "Technical Note: How accurate can stalagmite formation temperatures be determined using vapour bubble radius measurements in fluid inclusions?" Climate of the Past 11, no. 6 (2015): 905–13. http://dx.doi.org/10.5194/cp-11-905-2015.

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Abstract. Stalagmites are natural archives containing detailed information on continental climate variability of the past. Microthermometric measurements of fluid inclusion homogenisation temperatures allow determination of stalagmite formation temperatures by measuring the radius of stable laser-induced vapour bubbles inside the inclusions. A reliable method for precisely measuring the radius of vapour bubbles is presented. The method is applied to stalagmite samples for which the formation temperature is known. An assessment of the bubble radius measurement accuracy and how this error influe
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7

Rogerson, Mike, Yuri Dublyansky, Dirk L. Hoffmann, Marc Luetscher, Paul Töchterle, and Christoph Spötl. "Enhanced Mediterranean water cycle explains increased humidity during MIS 3 in North Africa." Climate of the Past 15, no. 5 (2019): 1757–69. http://dx.doi.org/10.5194/cp-15-1757-2019.

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Abstract. We report a new fluid inclusion dataset from northeastern Libyan speleothem SC-06-01, which is the largest speleothem fluid inclusion dataset for North Africa to date. The stalagmite was sampled in Susah Cave, a low-altitude coastal site, in Cyrenaica, on the northern slope of the Jebel Al-Akhdar. Speleothem fluid inclusions from the latest Marine Isotope Stage (MIS) 4 and throughout MIS 3 (∼67 to ∼30 kyr BP) confirm the hypothesis that past humid periods in this region reflect westerly rainfall advected through the Atlantic storm track. However, most of this moisture was sourced fro
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8

Osborne, Mark, and Stuart Haszeldine. "Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfields." Marine and Petroleum Geology 10, no. 3 (1993): 271–78. http://dx.doi.org/10.1016/0264-8172(93)90109-6.

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9

Sellwood, B. W., T. J. Shepherd, M. R. Evans, and B. James. "Origin of late cements in oolitic reservoir facies: a fluid inclusion and isotopic study (Mid-Jurassic, southern England)." Sedimentary Geology 61, no. 3-4 (1989): 223–37. http://dx.doi.org/10.1016/0037-0738(89)90059-6.

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10

Martı́n Crespo, Tomás, Antonio Delgado, Elena Vindel Catena, José Angel López Garcı́a, and Cécile Fabre. "The latest Post-Variscan fluids in the Spanish Central System: evidence from fluid inclusion and stable isotope data." Marine and Petroleum Geology 19, no. 3 (2002): 323–37. http://dx.doi.org/10.1016/s0264-8172(02)00020-x.

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Dissertations / Theses on the topic "Fluid inclusion stratigraphy"

1

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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2

Tremblay, François. "Étude de reconnaissance en géochimie isotopique de l'oxygene et de l'hydrogène : application à quelques minéralisations de la région de Chibougamau, Québec, Canada /." 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 en vue de l'obtention d'un diplôme de M.Sc.A." CaQCU Document électronique également accessible en format PDF. CaQCU
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3

See, Jeannette. "L'analyse des inclusions fluides et magmatiques des dépôts aurifères dans la région du Lac Shortt, Abitibi, Québec : l'interprétation thermodynamique et métallogénétique du rôle des fluides minéralisants à l'Archéen /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1994. http://theses.uqac.ca.

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4

Drieberg, Susan L. "The magmatic-hydrothermal architecture of the Archean Volcanic Massive Sulfide (VMS) System at Panorama, Pilbara, Western Australia." University of Western Australia. School of Earth and Geographical Sciences, 2003. http://theses.library.uwa.edu.au/adt-WU2004.0064.

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[Truncated abstract. Formulae and special characters can only be approximated here. Please see the pdf version of this abstract for an accurate representation.] The 3.24 Ga Panorama VMS District, located in the Pilbara Craton of Western Australia, is exposed as a cross-section through subvolcanic granite intrusions and a coeval submarine volcanic sequence that hosts Zn-Cu mineralization. The near-complete exposure across the district, the very low metamorphic grade, and the remarkable preservation of primary igneous and volcanic textures provides an unparalleled opportunity to examine the P-
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Books on the topic "Fluid inclusion stratigraphy"

1

Dilley, Lorie M. Fluid inclusion stratigraphy: A new method for geothermal reservoir assessment. [California Energy Commission], 2007.

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2

Schmidt-Mumm, Andreas. Die Entwicklung der Fluid-Systeme während der oberprotorozoischen [i.e. oberproterozoischen] Damara-Orogenese am Südrand des Damara-Orogens, Namibia. Selbstverlag der Geologischen Institute der Georg-August-Universität Göttingen, 1989.

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3

Kleinefeld, Bärbel. The charnockite-anorthosite suite of rocks exposed in central Dronning Maud Land, East Antarctica: A study on fluid-rock interactions, and post-entrapment change of metamorphic fluid inclusions = Die charnockitischen und anorthositischen Gesteinsserien im zentralen Dronning Maud Land : Fluid-Gesteins-Wechselwirkungen und die Veränderung metamorpher Fluid-Einschlüsse nach ihrer Bildung. Alfred-Wegener-Institut für Polar- und Meeresforschung, 2003.

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4

M, Friedman Gerald, ed. Post-Devonian sediment cover over New York State: Evidence from fluid-inclusion, organic maturation, clay diagenesis, and stable isotope studies. Springer-Verlag, 1995.

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5

Geological Survey (U.S.), ed. A preliminary study of thermometry and metal sources of the Spar Lake strata-bound copper-silver deposit, Belt Supergroup, Montana. U.S. Geological Survey, 1990.

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Book chapters on the topic "Fluid inclusion stratigraphy"

1

Walz, C., G. Chi, and P. K. Pedersen. "Petrographic, Stable Isotope and Fluid Inclusion Characteristics of the Viking Sandstones: Implications for Sequence Stratigraphy, Bayhurst Area, SW Saskatchewan, Canada." In Linking Diagenesis to Sequence Stratigraphy. John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118485347.ch14.

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Conference papers on the topic "Fluid inclusion stratigraphy"

1

Gruenwald, R. M., A. V. Milcov, M. Loegering, and B. Bailey. "Integration of IsoTube Analysis, Fluid Inclusion Stratigraphy and Basin Modeling in the Mozambique Basin." In First EAGE Eastern Africa Petroleum Geoscience Forum. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201414454.

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Reports on the topic "Fluid inclusion stratigraphy"

1

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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2

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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3

Fluid inclusion stratigraphy (FIS) data for the following exploratory oil/gas wells: Exxon Corporation Canning River Unit Block A-1, Exxon Corporation Canning River Unit B-1, ARCO Alaska Inc. Kavik #1, and ARCO Alaska Inc. Kavik Unit #2. Alaska Division of Geological & Geophysical Surveys, 2002. http://dx.doi.org/10.14509/19156.

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Journal articles
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