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Journal articles on the topic 'Fluid inclusion stratigraphy'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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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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5

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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6

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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11

Jonk, Rene, John Parnell, and Andrew Whitham. "Fluid inclusion evidence for a Cretaceous–Palaeogene petroleum system, Kangerlussuaq Basin, East Greenland." Marine and Petroleum Geology 22, no. 3 (2005): 319–30. http://dx.doi.org/10.1016/j.marpetgeo.2005.01.002.

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12

Ayllón-Quevedo, F., V. Souza-Egipsy, M. E. Sanz-Montero, and J. P. Rodríguez-Aranda. "Fluid inclusion analysis of twinned selenite gypsum beds from the Miocene of the Madrid basin (Spain). Implication on dolomite bioformation." Sedimentary Geology 201, no. 1-2 (2007): 212–30. http://dx.doi.org/10.1016/j.sedgeo.2007.06.001.

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13

Faÿ-Gomord, O., C. Allanic, M. Verbiest, et al. "Understanding Fluid Flow during Tectonic Reactivation: An Example from the Flamborough Head Chalk Outcrop (UK)." Geofluids 2018 (2018): 1–17. http://dx.doi.org/10.1155/2018/9352143.

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Flamborough Head chalks are located at the extremities of E-W and N-S trending fault systems along the Yorkshire coast (UK). Rock deformation is expressed in Selwicks Bay where a normal fault is exposed along with a high density of calcite veins. The fault mineralization is tested using geochemistry. Crosscutting relationships are used to differentiate between three vein generations: a network of parallel veins that are oriented perpendicular to stratigraphy (Group I), hydraulic breccia with typical jigsaw puzzle structure (Group II), and a third generation of calcite veins crosscutting the tw

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14

Chipley, Don B. L., and T. Kurtis Kyser. "Fluid inclusion evidence for the deposition and diagenesis of the Patience Lake Member of the Devonian Prairie Evaporite Formation, Saskatchewan, Canada." Sedimentary Geology 64, no. 4 (1989): 287–95. http://dx.doi.org/10.1016/0037-0738(89)90054-7.

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15

Affolter, S., D. Fleitmann, and M. Leuenberger. "New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS)." Climate of the Past 10, no. 4 (2014): 1291–304. http://dx.doi.org/10.5194/cp-10-1291-2014.

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Abstract. A new online method to analyse water isotopes of speleothem fluid inclusions using a wavelength scanned cavity ring down spectroscopy (WS-CRDS) instrument is presented. This novel technique allows us simultaneously to measure hydrogen and oxygen isotopes for a released aliquot of water. To do so, we designed a new simple line that allows the online water extraction and isotope analysis of speleothem samples. The specificity of the method lies in the fact that fluid inclusions release is made on a standard water background, which mainly improves the δ D robustness. To saturate the lin

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16

Affolter, S., D. Fleitmann, and M. Leuenberger. "New on-line method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS)." Climate of the Past Discussions 10, no. 1 (2014): 429–67. http://dx.doi.org/10.5194/cpd-10-429-2014.

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Abstract. A new online method to analyse water isotopes of speleothem fluid inclusions using a wavelength scanned cavity ring down spectroscopy (WS-CRDS) instrument is presented. This novel technique allows us to simultaneously measure hydrogen and oxygen isotopes for a released aliquot of water. To do so, we designed a new simple line that allows the on-line water extraction and isotope analysis of speleothem samples. The specificity of the method lies in the fact that fluid inclusions release is made on a standard water background, which mainly improves the δD reliability. To saturate the li

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17

Espeche, María José J., Raúl Lira, and Nicolás A. Viñas. "Aportes a la metalogénesis del basamento proterozoico superior-cámbrico de las Sierras Pampeanas Orientales: mineralogía, termometría e isótopos de azufre del skarn Malagueño (Cu- Fe±Zn), Sierra Chica, Córdoba, Argentina." Andean Geology 47, no. 1 (2020): 14. http://dx.doi.org/10.5027/andgeov47n1-3112.

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On-going mining operations in a marble quarry (Cantera Centro) from Malagueño, Sierra Chica de Córdoba, Argentina, have unearthed veins, veinlets and lenses of sulfides (pyrrhotite>pyrite≅ chalcopyrite>>sphalerite). These veins and lenses are up to 0.3 m thick and 2-3 m long, although intermittently can extend about a hundred meters. They are associated with skarns. The metasedimentary host sequence, largely composed of gneisses, amphibolites and marbles, was intruded by amphibolic metagabbro and metadiorite dykes, metatonalite plutons and alkali-feldspar metagranites; the whole

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18

Marchesini, Barbara, Paolo Stefano Garofalo, Luca Menegon, Jussi Mattila, and Giulio Viola. "Fluid-mediated, brittle–ductile deformation at seismogenic depth – Part 1: Fluid record and deformation history of fault veins in a nuclear waste repository (Olkiluoto Island, Finland)." Solid Earth 10, no. 3 (2019): 809–38. http://dx.doi.org/10.5194/se-10-809-2019.

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Abstract. The dynamic evolution of fault zones at the seismogenic brittle–ductile transition zone (BDTZ) expresses the delicate interplay between numerous physical and chemical processes. Deformation and fluid flow at the BDTZ are closely related and mutually dependent during repeating and transient cycles of frictional and viscous deformation. Despite numerous studies documenting in detail seismogenic faults exhumed from the BDTZ, uncertainties remain as to the exact role of fluids in facilitating broadly coeval brittle and ductile deformation at that structural level. We combine structural a

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19

O’Reilly, C., P. M. Shannon, and M. Feely. "A fluid inclusion study of cement and vein minerals from the Celtic Sea Basins, offshore Ireland." Marine and Petroleum Geology 15, no. 6 (1998): 519–33. http://dx.doi.org/10.1016/s0264-8172(98)00047-6.

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20

Burley, S. D., J. Mullis, and A. Matter. "Timing diagenesis in the Tartan Reservoir (UK North Sea): constraints from combined cathodoluminescence microscopy and fluid inclusion studies." Marine and Petroleum Geology 6, no. 2 (1989): 98–120. http://dx.doi.org/10.1016/0264-8172(89)90014-7.

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21

Worden, R. H., E. A. Warren, P. C. Smalley, T. J. Primmer, and N. H. Oxtoby. "Discussion of ‘Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfields’ by Osborne and Haszeldine (1993)." Marine and Petroleum Geology 12, no. 5 (1995): 566–70. http://dx.doi.org/10.1016/0264-8172(95)90014-4.

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22

Robertson, Clay, Greg A. Ludvigson, R. M. Joeckel, Sahar Mohammadi, and James I. Kirkland. "Differentiating early from later diagenesis in a Cretaceous sandstone and petroleum reservoir of the Cedar Mountain Formation, Utah." Rocky Mountain Geology 56, no. 1 (2021): 19–36. http://dx.doi.org/10.24872/rmgjournal.56.1.19.

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ABSTRACT Previously published anomalous whole-rock stable isotopic values from the Poison Strip Sandstone Member of the Cretaceous Cedar Mountain Formation (CMF) of eastern Utah are of uncertain origins. This study investigated the diagenetic history and the processes responsible for these anomalous data. Accordingly, we integrated photomicroscopic techniques including polarized light microscopy, epifluorescence and cathodoluminescence (CL) imaging, micromilling of stable isotope samples, and fluid-inclusion heating and freezing measurements to this end. The key observations involved the micro

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23

Ruggieri, Giovanni, Guia Morelli, Marco Benvenuti, et al. "Origin of the As anomaly in Quaternary sediments of Southern Tuscany (Italy): New insights from geological, geochemical and fluid inclusion data from the Pecora River and Bruna River Valleys." Sedimentary Geology 416 (April 2021): 105876. http://dx.doi.org/10.1016/j.sedgeo.2021.105876.

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24

Leroy, J. L., D. Hube, and E. Marcoux. "EPISODIC DEPOSITION OF Mn MINERALS IN COCKADE BRECCIA STRUCTURES IN THREE LOW-SULFIDATION EPITHERMAL DEPOSITS: A MINERAL STRATIGRAPHY AND FLUID-INCLUSION APPROACH." Canadian Mineralogist 38, no. 5 (2000): 1125–36. http://dx.doi.org/10.2113/gscanmin.38.5.1125.

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25

Koger, Jace M., and Dennis L. Newell. "Spatiotemporal history of fault–fluid interaction in the Hurricane fault, western USA." Solid Earth 11, no. 6 (2020): 1969–85. http://dx.doi.org/10.5194/se-11-1969-2020.

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Abstract. The Hurricane fault is a ∼250 km long, west-dipping, segmented normal fault zone located along the transition between the Colorado Plateau and the Basin and Range tectonic provinces in the western USA. Extensive evidence of fault–fluid interaction includes calcite mineralization and veining. Calcite vein carbon (δ13CVPDB) and oxygen (δ18OVPDB) stable isotope ratios range from −4.5 ‰ to 3.8 ‰ and from −22.1 ‰ to −1.1 ‰, respectively. Fluid inclusion microthermometry constrains paleofluid temperatures and salinities from 45 to 160 ∘C and from 1.4 wt % to 11.0 wt % as NaCl, respectively

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26

Barker, Charles E., Yvonne Bone, and Michael D. Lewan. "Fluid inclusion and vitrinite-reflectance geothermometry compared to heat-flow models of maximum paleotemperature next to dikes, western onshore Gippsland Basin, Australia." International Journal of Coal Geology 37, no. 1-2 (1998): 73–111. http://dx.doi.org/10.1016/s0166-5162(98)00018-4.

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27

Dong, Shaofeng, Daizhao Chen, Hairuo Qing, et al. "Hydrothermal alteration of dolostones in the Lower Ordovician, Tarim Basin, NW China: Multiple constraints from petrology, isotope geochemistry and fluid inclusion microthermometry." Marine and Petroleum Geology 46 (September 2013): 270–86. http://dx.doi.org/10.1016/j.marpetgeo.2013.06.013.

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28

Osborne, Mark, and R. Stuart Haszeldine. "Reply to a discussion of ‘Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfields’ by Osborne and Haszeldine (1993)." Marine and Petroleum Geology 12, no. 5 (1995): 561–65. http://dx.doi.org/10.1016/0264-8172(95)90013-6.

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29

Osborne, Mark, and R. Stuart Haszeldine. "Reply to a discussion of ‘Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfields’ by Osborne and Haszeldine (1993)." Marine and Petroleum Geology 12, no. 5 (1995): 570–75. http://dx.doi.org/10.1016/0264-8172(95)90015-2.

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30

Kronenberg, Andreas K., Hasnor F. B. Hasnan, Caleb W. Holyoke III, Richard D. Law, Zhenxian Liu, and Jay B. Thomas. "Synchrotron FTIR imaging of OH in quartz mylonites." Solid Earth 8, no. 5 (2017): 1025–45. http://dx.doi.org/10.5194/se-8-1025-2017.

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Abstract. Previous measurements of water in deformed quartzites using conventional Fourier transform infrared spectroscopy (FTIR) instruments have shown that water contents of larger grains vary from one grain to another. However, the non-equilibrium variations in water content between neighboring grains and within quartz grains cannot be interrogated further without greater measurement resolution, nor can water contents be measured in finely recrystallized grains without including absorption bands due to fluid inclusions, films, and secondary minerals at grain boundaries.Synchrotron infrared

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31

Su, Ao, Honghan Chen, Jian-xin Zhao, and Yue-xing Feng. "Integrated fluid inclusion analysis and petrography constraints on the petroleum system evolution of the central and southern Biyang Sag, Nanxiang Basin, Eastern China." Marine and Petroleum Geology 118 (August 2020): 104437. http://dx.doi.org/10.1016/j.marpetgeo.2020.104437.

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32

Duschl, Florian, Alfons van den Kerkhof, Graciela Sosa, et al. "Fluid inclusion and microfabric studies on Zechstein carbonates (Ca2) and related fracture mineralizations – New insights on gas migration in the Lower Saxony Basin (Germany)." Marine and Petroleum Geology 77 (November 2016): 300–322. http://dx.doi.org/10.1016/j.marpetgeo.2016.06.020.

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33

Berra, Fabrizio, Karem Azmy, and Giovanna Della Porta. "Stable-isotope and fluid inclusion constraints on the timing of diagenetic events in the dolomitized Dolomia Principale inner platform (Norian, Southern Alps of Italy)." Marine and Petroleum Geology 121 (November 2020): 104615. http://dx.doi.org/10.1016/j.marpetgeo.2020.104615.

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34

Grobe, Arne, Christoph von Hagke, Ralf Littke, et al. "Tectono-thermal evolution of Oman's Mesozoic passive continental margin under the obducting Semail Ophiolite: a case study of Jebel Akhdar, Oman." Solid Earth 10, no. 1 (2019): 149–75. http://dx.doi.org/10.5194/se-10-149-2019.

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Abstract. We present a study of pressure and temperature evolution in the passive continental margin under the Oman Ophiolite using numerical basin models calibrated with thermal maturity data, fluid-inclusion thermometry, and low-temperature thermochronometry and building on the results of recent work on the tectonic evolution. Because the Oman mountains experienced only weak post-obduction overprint, they offer a unique natural laboratory for this study. Thermal maturity data from the Adam Foothills constrain burial in the basin in front of the advancing nappes to at least 4 km. Peak tempera

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35

Liu, Dongdong, Chen Zhang, Zhankun Pan, et al. "Natural fractures in carbonate-rich tight oil reservoirs from the Permian Lucaogou Formation, southern Junggar Basin, NW China: Insights from fluid inclusion microthermometry and isotopic geochemistry." Marine and Petroleum Geology 119 (September 2020): 104500. http://dx.doi.org/10.1016/j.marpetgeo.2020.104500.

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36

Hendrickson, Michael D. "Regional and local controls on Archean rock-hosted cobalt mineralization at the McAra deposit, southern Superior Province, Ontario, Canada." Canadian Journal of Earth Sciences 57, no. 12 (2020): 1447–62. http://dx.doi.org/10.1139/cjes-2020-0059.

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The McAra deposit is in eastern Ontario, Canada, and is hosted in an Archean inlier to the Paleoproterozoic Huronian basin. It is currently estimated to contain ∼2.4 million pounds of cobalt at an average grade of 1.25%. New drill data show the mineralized zone comprises glaucodot–cobaltite veins and breccias that transect a mafic–siliciclastic volcanogenic massive sulfide (VMS) deposit. The high cobalt grade and host stratigraphy at the McAra deposit contrast with five-element (Ag–Co–Ni–Bi–As) deposits at the Cobalt and Gowganda camps in the region that produced high-grade silver and by-produ

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37

Wang, Yue, Xiangchun Chang, Yuzhuang Sun, Bingbing Shi, and Shenjun Qin. "Investigation of fluid inclusion and oil geochemistry to delineate the charging history of Upper Triassic Chang 6, Chang 8, and Chang 9 tight oil reservoirs, Southeastern Ordos Basin, China." Marine and Petroleum Geology 113 (March 2020): 104115. http://dx.doi.org/10.1016/j.marpetgeo.2019.104115.

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38

Mozafari, Mahtab, Rudy Swennen, Fabrizio Balsamo, Hamdy El Desouky, Fabrizio Storti, and Conxita Taberner. "Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration." Solid Earth 10, no. 4 (2019): 1355–83. http://dx.doi.org/10.5194/se-10-1355-2019.

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Abstract. The Lower Jurassic platform and basinal deposits exposed in the Montagna dei Fiori Anticline (Central Apennines, Italy) are pervasively affected by dolomitization. Based on the integration of field work, petrography, and geochemistry, two fault-related dolomitization events were recognized and interpreted as having occurred before and during the Apenninic orogeny. Fluid inclusion analysis indicates moderate to elevated salinity values of 3.5 to 20.5 and 12.8 to 18.6 eq. wt % NaCl in the first and the second event, respectively. The estimated salinities, in combination with δ18O value

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39

Su, Ao, Honghan Chen, Jian-xin Zhao, Tong-wei Zhang, Yue-xing Feng, and Cunwu Wang. "Natural gas washing induces condensate formation from coal measures in the Pinghu Slope Belt of the Xihu Depression, East China Sea Basin: Insights from fluid inclusion, geochemistry, and rock gold-tube pyrolysis." Marine and Petroleum Geology 118 (August 2020): 104450. http://dx.doi.org/10.1016/j.marpetgeo.2020.104450.

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40

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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41

Repetski, J. E., M. E. Taylor, D. S. Collins, A. R. Palmer, G. D. Wood, and R. C. Tobin. "Integrating paleontology, geothermometry, and sedimentology in determining the history of the Reelfoot Basin, southern midcontinent, U.S.A." Paleontological Society Special Publications 6 (1992): 243. http://dx.doi.org/10.1017/s2475262200008030.

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The northeast-trending Reelfoot basin, extending from northeast Arkansas and westernmost Tennessee into southeastern Missouri, southernmost Illinois, and westernmost Kentucky, is geologically, and socioeconomically, significant because it is co-extensive with the New Madrid Seismic Zone, one of the most seismically active areas of the central and eastern United States. The basin has been periodically active from its inception as a rift basin in the Proterozoic to the present and has accumulated up to at least 5,000 m of sediment, including up to at least 1 km of Cretaceous and Tertiary sedimen

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42

Glover, Paul W. J. "Archie's law – a reappraisal." Solid Earth 7, no. 4 (2016): 1157–69. http://dx.doi.org/10.5194/se-7-1157-2016.

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Abstract. When scientists apply Archie's first law they often include an extra parameter a, which was introduced about 10 years after the equation's first publication by Winsauer et al. (1952), and which is sometimes called the “tortuosity” or “lithology” parameter. This parameter is not, however, theoretically justified. Paradoxically, the Winsauer et al. (1952) form of Archie's law often performs better than the original, more theoretically correct version. The difference in the cementation exponent calculated from these two forms of Archie's law is important, and can lead to a misestimation

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43

Miranda-Gasca, Miguel A., Jose Arturo Gomez-Caballero, and Christopher J. Eastoe. "Borate deposits of northern Sonora, Mexico; stratigraphy, tectonics, stable isotopes, and fluid inclusions." Economic Geology 93, no. 4 (1998): 510–23. http://dx.doi.org/10.2113/gsecongeo.93.4.510.

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44

Zheng, Haofu, Yongsheng Ma, Guoxiang Chi, et al. "Stratigraphic and Structural Control on Hydrothermal Dolomitization in the Middle Permian Carbonates, Southwestern Sichuan Basin (China)." Minerals 9, no. 1 (2019): 32. http://dx.doi.org/10.3390/min9010032.

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The Qixia Formation and Maokou Formation of Middle Permian in the southwestern Sichuan Basin were pervasively dolomitized during the diagenetic history. Petrographically, four types of dolomites, namely three replacive dolomites (Rd1, Rd2, and Rd3) and one dolomite cement (Cd), were distinguished. Rd1 dolomite occurs as very fine (<50 µm), planar-s to nonplanar crystals; Rd2 dolomite shows planar-e to planar-s crystal shapes with fine crystal sizes (50–250 µm) and is characterized by center-frog and margin-clear; Rd3 dolomite occurs as medium to coarse (250 µm–2 mm), nonplanar crystals; and

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Mihalynuk, M. G., and E. D. Ghent. "Regional depth-controlled hydrothermal metamorphism in the Zymoetz River area, British Columbia." Canadian Journal of Earth Sciences 33, no. 8 (1996): 1169–84. http://dx.doi.org/10.1139/e96-088.

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An estimated 6 km of basic to silicic volcanic flows and clastic rocks of the Early Jurassic Telkwa Formation is exposed in moderately east-dipping fault blocks along the Zymoetz River, British Columbia. Extensive wholesale zeolitic replacement of porous tuff beds suggests widespread hydrothermal activity. Metamorphic grade increases regionally from laumontite–albite facies to prehnite–pumpellyite facies with increasing stratigraphic depth. Telkwa Formation strata and the imparted metamorphic zonation are cut and tilted by rotational block faulting, and are repeated in each of the upturned blo

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Liedmann, Wolfgang, and Roman Koch. "Diagenesis and fluid inclusions of Upper Jurassic sponge-algal reefs in SW Germany." Facies 23, no. 1 (1990): 241–67. http://dx.doi.org/10.1007/bf02536715.

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Robinson, Andrew, Shona Grant, and Norman Oxtoby. "Evidence against natural deformation of fluid inclusions in diagenetic quartz." Marine and Petroleum Geology 9, no. 5 (1992): 568–72. http://dx.doi.org/10.1016/0264-8172(92)90067-o.

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Petrychenko, Oleh, Tadeusz Marek Peryt, and Brian Roulston. "Seawater composition during deposition of Viséan evaporites in the Moncton Subbasin of New Brunswick as inferred from the fluid inclusion study of halite." Canadian Journal of Earth Sciences 39, no. 2 (2002): 157–67. http://dx.doi.org/10.1139/e01-066.

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The Viséan evaporites of the Windsor Group in the Moncton Subbasin at the western limit of the Maritimes Basin of eastern Canada represent an important stratigraphic sequence to study in determining changes in the chemistry of marine brines. Seventeen samples of halite have been selected for fluid inclusion study. The chemical composition of inclusion brines was examined using the Petrichenko method of glass capillaries with applied ultramicroanalytical techniques. The results of the study indicate that the conditions of evaporite deposition in the Windsor Basin differed from those recorded in

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Rollet, Nadege, Chris Nicholson, Andrew Jones, Emmanuelle Grosjean, George Bernardel, and John Kennard. "New exploration opportunities in the offshore Houtman and Abrolhos sub-basins, northern Perth Basin, WA." APPEA Journal 53, no. 1 (2013): 97. http://dx.doi.org/10.1071/aj12008.

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The 2013 Acreage Release Areas W13-19 and W13-20 in the offshore northern Perth Basin, Western Australia, cover more than 19,000 km2 in parts of the Houtman, Abrolhos, Zeewyck and Gascoyne sub-basins. The Release Areas are located adjacent to WA-481-P, the only active offshore exploration permit in the Perth Basin, granted to joint venture partners Murphy Australia Oil Pty Ltd, Kufpec Australia Pty Ltd and Samsung Oil and Gas Australia Pty Ltd in August 2012. Geoscience Australia recently undertook a regional prospectivity study in the area as part of the Australian Government’s Offshore Energ

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CONIGLIO, M., and A. E. WILLIAMS-JONES. "Diagenesis of Ordovician carbonates from the north-east Michigan Basin, Manitoulin Island area, Ontario: evidence from petrography, stable isotopes and fluid inclusions." Sedimentology 39, no. 5 (1992): 813–36. http://dx.doi.org/10.1111/j.1365-3091.1992.tb02155.x.

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