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Relevant bibliographies by topics / Evaporite and carbonate and siliciclastic minerals

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Journal articles
Dissertations / Theses
Conference papers

Academic literature on the topic 'Evaporite and carbonate and siliciclastic minerals'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Evaporite and carbonate and siliciclastic minerals"

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Sadooni, Fadhil N., Fares Howari, Howell G. M. Edwards, and Ayman El-Saiy. "Lithology, mineral assemblages and microbial fingerprints of the evaporite-carbonate sediments of the coastal sabkha of Abu Dhabi and their extraterrestrial implications." International Journal of Astrobiology 9, no. 3 (2010): 147–56. http://dx.doi.org/10.1017/s1473550410000078.

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AbstractDeep-core and surface samples collected from the coastal sabkha of Abu Dhabi were subjected to a multi-proxy study, including petrographic, geochemical and spectroscopic analyses. The sediments studied are composed of biochemical carbonate-evaporite mineral suites, such as calcite, dolomite, aragonite and gypsum, as well as clastic minerals, such as quartz, feldspar and serpentine. These sediments were also strongly influenced by microbial activities as reflected by the presence of cyanobacterial mats, boring, gas bubble structures, pustular and other macro and micro textures. A combin

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Martini, Anna M., Lynn M. Walter, Timothy W. Lyons, Victoria C. Hover, and John Hansen. "Significance of early-diagenetic water-rock interactions in a modern marine siliciclastic/evaporite environment: Salina Ometepec, Baja California." GSA Bulletin 114, no. 9 (2002): 1055–69. http://dx.doi.org/10.1130/0016-7606(2002)114<1055:soedwr>2.0.co;2.

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Abstract Although marine brines are a significant component of pore waters in sedimentary basins, there are few geochemical studies of modern analogues of such systems, especially in siliciclastic settings. For these reasons, we chose the evaporite-associated siliciclastic sediments deposited in the salt flats of the Salina Ometepec, Baja California, for an integrated investigation of sediment, pore-water, and overlying brine geochemistry. Here, the detrital components include quartz, K-feldspar, plagioclase, chlorite, biotite, and smectite, and authigenic minerals are dominated by halite, gyp

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KLEIN, CARLA, and ANA MARIA PIMENTEL MIZUSAKI. "Cimentação Carbonática em Reservatórios Siliciclásticos - O Papel da Dolomita -." Pesquisas em Geociências 34, no. 1 (2007): 91. http://dx.doi.org/10.22456/1807-9806.19465.

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Carbonates are important diagenetic cements in siliciclastic rocks thus important to determine these rocks as hydrocarbon reservoirs. The cement is the material had chemically precipitated partial or totally pore filling, affecting rock values of porosity and permeability. The acknowledgment of diagenetic patterns those are associated to the carbonatic cement precipitation and their impacts in the reservoirs quality can decrease the risks of exploration and exploitation of new reservoirs. Therefore is necessary the knowledge of origin and processes of carbonate cement’s precipitation. These ce

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Majzlan, Juraj, Maria Brey-Funke, Alexander Malz, Stefan Donndorf, and Rastislav Milovský. "Fluid evolution and mineralogy of Mn-Fe-barite-fluorite mineralizations at the contact of the Thuringian Basin, Thüringer Wald and Thüringer Schiefergebirge in Germany." Geologica Carpathica 67, no. 1 (2016): 3–20. http://dx.doi.org/10.1515/geoca-2016-0001.

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Abstract Numerous small deposits and occurrences of Mn-Fe-fluorite-barite mineralization have developed at the contact of the Thuringian Basin, Thüringer Wald and Thüringer Schiefergebirge in central Germany. The studied mineralizations comprise the assemblages siderite+ankerite-calcite-fluorite-barite and hematite-Mn oxides-calcite-barite, with the precipitation sequence in that order within each assemblage. A structural geological analysis places the origin of the barite veins between the Middle Jurassic and Early Cretaceous. Primary fluid inclusions contain water vapour and an aqueous phase

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Ben Ismail, Mohamed Hédi, and Ali M'Rabet. "Evaporite, carbonate, and siliciclastic transitions in the Jurassic sequences of southeastern Tunisia." Sedimentary Geology 66, no. 1-2 (1990): 65–82. http://dx.doi.org/10.1016/0037-0738(90)90007-g.

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Purser, Bruce H., Mohamad Soliman, and Ali M'Rabet. "Carbonate, evaporite, siliciclastic transitions in Quaternary rift sediments of the northwestern Red Sea." Sedimentary Geology 53, no. 3-4 (1987): 247–67. http://dx.doi.org/10.1016/0037-0738(87)90037-6.

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Kenter, Jeroen A. M., F. F. Podladchikov, Marc Reinders, Sjierk J. Van der Gaast, Bruce W. Fouke, and Mark D. Sonnenfeld. "Parameters controlling sonic velocities in a mixed carbonate‐siliciclastics Permian shelf‐margin (upper San Andres formation, Last Chance Canyon, New Mexico)." GEOPHYSICS 62, no. 2 (1997): 505–20. http://dx.doi.org/10.1190/1.1444161.

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We have measured the acoustic properties and mineralogic composition of 48 rock specimens from mixed carbonate‐siliciclastic outcrops of the Permian upper San Andres formation in Last Chance Canyon, New Mexico. The goals were: (1) identify and model the parameters controlling the sonic velocities; (2) assess the influence of postburial diagenesis on the acoustic velocities. The variation in sonic velocity in the 0 to 25% porosity range is primarily controlled by porosity, and secondly by the ratio of carbonate‐siliciclastic material. Linear multivariate fitting resulted in a velocity‐porosity‐

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Zhang, Biao, Dan Zhao, Pengpeng Zhou, Shen Qu, Fu Liao, and Guangcai Wang. "Hydrochemical Characteristics of Groundwater and Dominant Water–Rock Interactions in the Delingha Area, Qaidam Basin, Northwest China." Water 12, no. 3 (2020): 836. http://dx.doi.org/10.3390/w12030836.

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Groundwater is undoubtedly important for water supplies and eco-environment protection, especially for arid and semi-arid regions. Analyzing the characteristics and evolution of groundwater is significant for the rational management of groundwater resources. This study investigated the hydrogeochemical characteristics and evolutions of groundwater in the Delingha area, northeast of the Qaidam Basin, northwest China, with a total of 123 water samples, including 105 unconfined groundwater samples, 12 confined groundwater samples, and 6 surface water samples. Hydrochemical results showed that the

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Husinec, Antun, and Lukas A. Harvey. "Late Ordovician climate and sea-level record in a mixed carbonate-siliciclastic-evaporite lithofacies, Williston Basin, USA." Palaeogeography, Palaeoclimatology, Palaeoecology 561 (January 2021): 110054. http://dx.doi.org/10.1016/j.palaeo.2020.110054.

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Hewton, M. L., D. D. Marshall, L. Ootes, L. E. Loughrey, and R. A. Creaser. "Colombian-style emerald mineralization in the northern Canadian Cordillera: integration into a regional Paleozoic fluid flow regime." Canadian Journal of Earth Sciences 50, no. 8 (2013): 857–71. http://dx.doi.org/10.1139/cjes-2012-0128.

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Emerald in the Mackenzie Mountains is hosted in extensional quartz–carbonate veins cutting organic-poor Neoproterozoic sandstones and siltstones within the hanging wall of a thrust fault that emplaced these strata above Paleozoic rocks. Isotopic compositions of water extracted from emerald are typical of evolved sedimentary sulphate brines. Fluid inclusion studies indicate two saline fluid populations: a CO2–N2-bearing, high-salinity brine (20.4–25.8 wt.% NaCl equivalent), and a gas-free, saline brine (7.6–15.3 wt.% NaCl equivalent). Both populations display evidence of post-entrapment volume

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Dissertations / Theses on the topic "Evaporite and carbonate and siliciclastic minerals"

1

Al-Yousef, Mariam. "Mineralogy, geochemistry and origin of Quaternary sabkhas in the Qatar peninsula, Arabian Gulf." Thesis, University of Southampton, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.274567.

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Best, Mairi M. R. "Fates of skeletal carbonate in tropical marine siliciclastic and carbonate sediments, Panama /." 2000. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:9965048.

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Conference papers on the topic "Evaporite and carbonate and siliciclastic minerals"

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Xu, Z., S. Hu, W. Zhao, H. Zeng, Q. Fu, and L. Wang. "Lithology of a Mixed Siliciclastic-Carbonate-Evaporite System: Triassic Jialingjiang Formation, Sichuan Basin, China." In 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202010936.

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Slowakiewicz, Miroslaw, Richard D. Pancost, Lisa Thomas, Maurice E. Tucker, Sher Mey Didi-Ooi, and Fiona Whitaker. "Holocene Intertidal Microbial Mats Of Qatar And Their Implications For Petroleum Source Rock Formation In Carbonate-Siliciclastic-Evaporite Systems." In International Petroleum Technology Conference. International Petroleum Technology Conference, 2014. http://dx.doi.org/10.2523/iptc-17400-ms.

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Slowakiewicz, Miroslaw, Richard D. Pancost, Lisa Thomas, Maurice E. Tucker, Sher Mey Didi-Ooi, and Fiona Whitaker. "Holocene Intertidal Microbial Mats Of Qatar And Their Implications For Petroleum Source Rock Formation In Carbonate-Siliciclastic-Evaporite Systems." In International Petroleum Technology Conference. International Petroleum Technology Conference, 2014. http://dx.doi.org/10.2523/17400-ms.

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Słowakiewicz, M., R. D. Pancost, L. Thomas, M. E. Tucker, S. Mey Didi-Ooi, and F. Whitaker. "Holocene Intertidal Microbial Mats of Qatar and Their Implications for Petroleum Source Rock Formation in Carbonate-Siliciclastic-Evaporite Systems." In IPTC 2014: International Petroleum Technology Conference. European Association of Geoscientists & Engineers, 2014. http://dx.doi.org/10.3997/2214-4609-pdb.395.iptc-17400-ms.

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Xu, Zhaohui, Wenzhi Zhao, Suyun Hu, Hongliu Zeng, and Qilong Fu. "Facies analysis of a mixed siliciclastic-carbonate-evaporite system by using 3D seismic and well data: Lower Triassic Jialingjiang Formation, Sichuan Basin, southwestern China." In SEG Technical Program Expanded Abstracts 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/segam2017-17359320.1.

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