Готові списки джерел за темами / Rocks, Carbonate

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Добірка наукової літератури з теми "Rocks, Carbonate"

Автор: Grafiati
Опубліковано: 4 червня 2021
Оновлено: 31 січня 2023

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Статті в журналах з теми "Rocks, Carbonate"

1

Yaxley, Gregory M., Bruce A. Kjarsgaard, and A. Lynton Jaques. "Evolution of Carbonatite Magmas in the Upper Mantle and Crust." Elements 17, no. 5 (October 1, 2021): 315–20. http://dx.doi.org/10.2138/gselements.17.5.315.

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Carbonatites are the most silica-poor magmas known and are amongst Earth’s most enigmatic igneous rocks. They crystallise to rocks dominated by the carbonate minerals calcite and dolomite. We review models for carbonatite petrogenesis, including direct partial melting of mantle lithologies, exsolution from silica-undersaturated alkali silicate melts, or direct fractionation of carbonated silicate melts to carbonate-rich residual melts. We also briefly discuss carbonatite–mantle wall-rock reactions and other processes at mid-to upper crustal depths, including fenitisation, overprinting by carbo
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2

Korinevsky, V. G., and E. V. Korinevsky. "Isotopic evidences of magmatic nature of the dolomite-calcite bodies of the Ilmeny Mountains and the Plastovsky district of the South Urals." Vestnik of Geosciences 11 (2020): 3–19. http://dx.doi.org/10.19110/geov.2020.11.1.

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The data obtained for the first time on the isotopic composition of oxygen and carbon of calcites and graphites of dolomitecalcite rocks of the Ilmeny Mountains and dykes of a similar composition in the Plastovsky district have confirmed their magmatic genesis. The temperature of formation of carbonate bodies (590—1000 °Ñ), determined from the isotopic ratios of C and O in calcite and graphite, corresponds to the temperature range (600—900 °Ñ) of the formation of carbonatite associations. According to the same ratios of isotopes in calcites, the protoliths of carbonate rocks are located within
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3

Bishop, Janice L., Rachel T. Schelble, Christopher P. McKay, Adrian J. Brown, and Kaysea A. Perry. "Carbonate rocks in the Mojave Desert as an analogue for Martian carbonates." International Journal of Astrobiology 10, no. 4 (July 1, 2011): 349–58. http://dx.doi.org/10.1017/s1473550411000206.

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AbstractCarbonate rocks in the Mojave Desert are presented as potential analogues for the carbonates on Mars. Rocks collected from the Little Red Hill site contain iron oxide-bearing coatings that greatly suppress the spectral features due to carbonate of the underlying material and impart a spectral slope. The Mojave Desert was formerly a lush pedogenic soil environment that, over time, transformed into the current arid climate with abundant rock varnish. One niche for microbes in the current desolate environment is inside and underneath the rocks where the microbes profit from solar protecti
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4

Arman, Hasan, Mahmoud Abu Saima, Osman Abdelghany, and Safwan Paramban. "Comparative Study on Degradability Characteristics of Evaporitic and Carbonate Rocks from Al Ain, United Arab Emirates." IOP Conference Series: Earth and Environmental Science 906, no. 1 (November 1, 2021): 012130. http://dx.doi.org/10.1088/1755-1315/906/1/012130.

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Abstract The slake durability index (SDI) test is a well know and extensively used to measure the degradability behaviour of rocks especially for weak rocks like mudstone, shale, evaporites, carbonates, etc. The degradability of rocks plays a critical role in engineering design process either on or in the rock mass for safe and sustainable structures. Evaporitic and carbonate rocks are vulnerable to physical, chemical and mechanical weathering, break down, as result of wetting-drying processes during the SDI test. Evaporites and carbonates are outcropped at the surface and subsurface of the Al
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5

Nikiforov, Anatoly V., Elena O. Dubinina, Nikolay A. Polyakov, Amina M. Sugorakova, and Aylan K. Khertek. "Influence of Host Marble Rocks on the Formation of Intrusive Alkaline Rocks and Carbonatites of Sangilen (E. Siberia, Russia)." Minerals 11, no. 7 (June 22, 2021): 666. http://dx.doi.org/10.3390/min11070666.

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The study of the O and C isotope composition of calcite from nepheline syenites, ijolites and carbonatites of the Chik intrusion and the intrusions of the Erzin–Tarbagatay group of Sangilen (Eastern Siberia, Russia) showed derivation from alkaline melts enriched with a carbonate component from the host marbleized sedimentary rocks. The calculations showed that about 40% of the initial mass of carbonates involved in the interaction with silicate melts have remained after decarbonation. During the assimilation of the carbonate, an oxygen isotope exchange took place between the residual carbonate
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6

Adam, Ludmila, Michael Batzle, and Ivar Brevik. "Gassmann's fluid substitution and shear modulus variability in carbonates at laboratory seismic and ultrasonic frequencies." GEOPHYSICS 71, no. 6 (November 2006): F173—F183. http://dx.doi.org/10.1190/1.2358494.

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Carbonates have become important targets for rock property research in recent years because they represent many of the major oil and gas reservoirs in the world. Some are undergoing enhanced oil recovery. Most laboratory studies to understand fluid and pressure effects on reservoir rocks have been performed on sandstones, but applying relations developed for sandstones to carbonates is problematic, at best. We measure in the laboratory nine carbonate samples from the same reservoir at seismic (3–3000 Hz) and ultrasonic [Formula: see text] frequencies. Samples are measured dry (humidified) and
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7

Chen, Jun-Qing, Xiong-Qi Pang, Song Wu, Zhuo-Heng Chen, Mei-Ling Hu, Luo-Fu Liu, Kui-You Ma, Bo Pang, and Zhi-Peng Huo. "Method for identifying effective carbonate source rocks: a case study from Middle–Upper Ordovician in Tarim Basin, China." Petroleum Science 17, no. 6 (September 19, 2020): 1491–511. http://dx.doi.org/10.1007/s12182-020-00489-z.

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AbstractHydrocarbon expulsion occurs only when pore fluid pressure due to hydrocarbon generation in source rock exceeds the force against migration in the adjacent carrier beds. Taking the Middle–Upper Ordovician carbonate source rock of Tarim Basin in China as an example, this paper proposes a method that identifies effective carbonate source rock based on the principles of mass balance. Data from the Well YW2 indicate that the Middle Ordovician Yijianfang Formation contains effective carbonate source rocks with low present-day TOC. Geological and geochemical analysis suggests that the hydroc
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8

Xu, Hengchao, Xiaotong Peng, Shun Chen, Jiwei Li, Shamik Dasgupta, Kaiwen Ta, and Mengran Du. "Macrofaunal burrowing enhances deep-sea carbonate lithification on the Southwest Indian Ridge." Biogeosciences 15, no. 21 (October 30, 2018): 6387–97. http://dx.doi.org/10.5194/bg-15-6387-2018.

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Abstract. Deep-sea carbonates represent an important type of sedimentary rock due to their effect on the composition of the upper oceanic crust and their contribution to deep-sea geochemical cycles. However, the role of deep-sea macrofauna in carbonate lithification remains poorly understood. A large lithified carbonate area, characterized by thriving benthic faunas and a tremendous amount of burrows, was discovered in 2008, blanketing the seafloor of the ultraslowly spreading Southwest Indian Ridge (SWIR). Benthic inhabitants – including echinoids, polychaetes, gastropods and crustaceans – ar
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9

Kuang, Hong Hai. "Pattern Recognition of Carbonate Rocks in Rs Image." Key Engineering Materials 500 (January 2012): 37–39. http://dx.doi.org/10.4028/www.scientific.net/kem.500.37.

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Pattern recognition of carbonate rocks in RS image have been studied in the paper. Samples of carbonate rocks were scanned into rock images.By analysing these samples of carbonate rocks,a new arithmetic was chosed and a standard curve of carbonate rocks by the arithmetic can be gotten.Rs images were divided into grids.There are curves by the arithmetic in grids. The standard curve of carbonate rocks and curves in grids were compared.If both of curves look very similar,the grid is carbonate rocks area.
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10

Ehlmann, Bethany L., John F. Mustard, Scott L. Murchie, Francois Poulet, Janice L. Bishop, Adrian J. Brown, Wendy M. Calvin, et al. "Orbital Identification of Carbonate-Bearing Rocks on Mars." Science 322, no. 5909 (December 19, 2008): 1828–32. http://dx.doi.org/10.1126/science.1164759.

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Geochemical models for Mars predict carbonate formation during aqueous alteration. Carbonate-bearing rocks had not previously been detected on Mars' surface, but Mars Reconnaissance Orbiter mapping reveals a regional rock layer with near-infrared spectral characteristics that are consistent with the presence of magnesium carbonate in the Nili Fossae region. The carbonate is closely associated with both phyllosilicate-bearing and olivine-rich rock units and probably formed during the Noachian or early Hesperian era from the alteration of olivine by either hydrothermal fluids or near-surface wat
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Дисертації з теми "Rocks, Carbonate"

1

Freiman, Gabriel, Jean-Pierre Korb, Benjamin Nicot, and Patrice Ligneul. "Microscopic wettability of carbonate rocks." Universitätsbibliothek Leipzig, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-192328.

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Nuclear Magnetic Relaxation Dispersion (NMRD) is strongly sensitive to the microscopic wettability of oil and brine bearing carbonate rocks. Exploring a very large range of low frequency enables isolating the typical NMRD dispersion features, 1/T1Surf, associated to the different processes of molecular surface dynamics. This allows a separation of the surface and bulk microdynamics of oil and water even for a biphasic saturation of petroleum rocks. Several surface dynamical parameters were determined and related to the concept of microscopic wettability of oil and water in porous media.
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2

Dong, Chengli. "Acidizing of naturally-fractured carbonate formations." Access restricted to users with UT Austin EID Full text (PDF) from UMI/Dissertation Abstracts International, 2001. http://wwwlib.umi.com/cr/utexas/fullcit?p3031042.

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3

Schmidt, Volkmar. "Magnetic and mineral fabrics in carbonate rocks /." Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17090.

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4

Berhanu, Solomon Assefa. "Seismic and petrophysical properties of carbonate reservoir rocks." Thesis, University of Reading, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262633.

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5

Bosak, Tanja Kirschvink Joseph L. "Laboratory models of microbial biosignatures in carbonate rocks /." Diss., Pasadena, Calif. : California Institute of Technology, 2005. http://resolver.caltech.edu/CaltechETD:etd-12102004-144939.

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6

Huang, Wentao, Peter C. Lippert, Yang Zhang, Michael J. Jackson, Mark J. Dekkers, Juan Li, Xiumian Hu, Bo Zhang, Zhaojie Guo, and Hinsbergen Douwe J. J. van. "Remagnetization of carbonate rocks in southern Tibet: Perspectives from rock magnetic and petrographic investigations." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/624349.

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The latitudinal motion of the Tibetan Himalayathe northernmost continental unit of the Indian plateis a key component in testing paleogeographic reconstructions of the Indian plate before the India-Asia collision. Paleomagnetic studies of sedimentary rocks (mostly carbonate rocks) from the Tibetan Himalaya are complicated by potentially pervasive yet cryptic remagnetization. Although traditional paleomagnetic field tests reveal some of this remagnetization, secondary remanence acquired prior to folding or tilting easily escapes detection. Here we describe comprehensive rock magnetic and petrog
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7

Huang, Tianping. "Wormhole modeling in carbonate acidizing /." Digital version accessible at:, 2000. http://wwwlib.umi.com/cr/utexas/main.

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8

El-Maghraby, Rehab Motasiem Nasr Ali. "Measurements of CO₂ trapping in carbonate and sandstone rocks." Thesis, Imperial College London, 2013. http://hdl.handle.net/10044/1/11066.

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CO2 storage in saline aquifers (sandstone/carbonate types) has been proposed as a promising solution to help reduce CO2 emissions to the atmosphere. CO2 will likely be stored as a dense, supercritical (sc.) phase. There are different mechanisms by which CO2 could be stored safely underground; structural and stratigraphic trapping, dissolution trapping, capillary trapping, and mineral trapping. I study capillary trapping. We assume that in the middle of a CO2 plume, many kilometres in extent, the CO2, brine and rock have been in mutual contact for several years. In these circumstances, the degr
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9

Johnson, Aaron W. "Regional-scale geochemical analysis of carbonate cements : reconstructing multiple fluid interactions related to dolomitization and mineralization in lower carboniferous rocks of the Irish Midlands /." free to MU campus, to others for purchase, 2003. http://wwwlib.umi.com/cr/mo/fullcit?p3101027.

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Stafford, Kevin Wayne. "Structural controls on megaporosity in eogenetic carbonate rocks Tinian, CNMI /." Master's thesis, Mississippi State : Mississippi State University, 2003. http://library.msstate.edu/etd/show.asp?etd=etd-10302003-080242.

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Книги з теми "Rocks, Carbonate"

1

E, Tucker Maurice, and Bathurst Robin G. C, eds. Carbonate diagenesis. Oxford: Blackwell Scientific Publications, 1990.

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2

Bagrint︠s︡eva, K. I. Carbonate reservoir rocks. Hoboken, New Jersey: John Wiley & Sons, 2015.

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3

Bagrintseva, Ksenia I. Carbonate Reservoir Rocks. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2015. http://dx.doi.org/10.1002/9781119084006.

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4

An introduction to carbonate sediments and rocks. Glasgow: Blackie, 1987.

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5

1953-, Wright V. Paul, and Dickson J. A. D, eds. Carbonate sedimentology. Oxford [England]: Blackwell Scientific Publications, 1990.

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6

Prudic, David E. Conceptual evaluation of regional ground-water flow in the carbonate-rock province of the Great Basin, Nevada, Utah, and adjacent states. Carson City, Nev: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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7

Prudic, David E. Conceptual evaluation of regional ground-water flow in the carbonate-rock province of the Great Basin, Nevada, Utah, and adjacent states. Washington: U.S. G.P.O., 1995.

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8

Prudic, David E. Conceptual evaluation of regional ground-water flow in the carbonate-rock province of the Great Basin, Nevada, Utah, and adjacent states. Washington: U.S. G.P.O., 1995.

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9

Bathurst, Robin G. C. Carbonate sediments and their diagenesis. 2nd ed. Amsterdam: Elsevier, 1986.

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10

1934-, Mackenzie Fred T., ed. Geochemistry of sedimentary carbonates. Amsterdam: Elsevier, 1990.

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Частини книг з теми "Rocks, Carbonate"

1

Whittaker, Alun. "Carbonate Rocks." In Formation Evaluation, 75–117. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5353-6_3.

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2

Flügel, Erik. "Reservoir Rocks and Host Rocks." In Microfacies of Carbonate Rocks, 877–94. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08726-8_17.

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3

Flügel, Erik. "Carbonate Depositional Environments." In Microfacies of Carbonate Rocks, 7–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08726-8_2.

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Flügel, Erik. "Carbonate Depositional Environments." In Microfacies of Carbonate Rocks, 7–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03796-2_2.

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Flügel, Erik. "Practical use of microfacies: Reservoir Rocks and Host Rocks." In Microfacies of Carbonate Rocks, 877–94. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03796-2_17.

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6

Singhal, B. B. S., and R. P. Gupta. "Hydrogeology of carbonate rocks." In Applied Hydrogeology of Fractured Rocks, 275–93. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-015-9208-6_13.

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Singhal, B. B. S., and R. P. Gupta. "Hydrogeology of Carbonate Rocks." In Applied Hydrogeology of Fractured Rocks, 269–89. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-8799-7_15.

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Flügel, Erik. "New Perspectives in Microfacies." In Microfacies of Carbonate Rocks, 1–6. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08726-8_1.

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Flügel, Erik. "Fossils in Thin Section: It is Not That Difficult." In Microfacies of Carbonate Rocks, 399–574. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08726-8_10.

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Flügel, Erik. "Summarizing Microfacies Criteria: Microfacies Types." In Microfacies of Carbonate Rocks, 575–86. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08726-8_11.

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Тези доповідей конференцій з теми "Rocks, Carbonate"

1

Li, Chengcheng, Kefei Zhang, Zhonggao Ma, and Weihua Liu. "Rock property measurement and analysis of carbonate rocks." In SEG 2018 Workshop: Reservoir Geophysics, Daqing, China, 5-7 August 2018. Society of Exploration Geophysicists and the Chinese Geophysical Society, 2018. http://dx.doi.org/10.1190/rege2018-08.1.

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2

Lamy, Celine Marie Marguerit, Stefan Iglauer, Christopher Holst Pentland, Martin Julian Blunt, and Geoffrey Colin Maitland. "Capillary Trapping In Carbonate Rocks." In SPE EUROPEC/EAGE Annual Conference and Exhibition. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/130720-ms.

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3

de Assis, Pinto, Leonardo, and De Ceia. "Acoustic properties of carbonate rocks." In 13th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 26-29 August 2013. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2013. http://dx.doi.org/10.1190/sbgf2013-406.

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Alvarez, Walter, Joke Belza, Philippe Claeys, David Peacock, and Enrico Tavarnelli. "EXPANSION BRECCIAS IN CARBONATE ROCKS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282404.

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Sapiie, B. "Fractures Characterization in Carbonate Rocks." In 72nd EAGE Conference and Exhibition incorporating SPE EUROPEC 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609.201400907.

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Bolourinejad, Panteha, Dirk Groenendijk, Johannes Van Wunnik, and Miranda Mooijer- van den Heuvel. "Surfactant Adsorption on Carbonate Rocks." In SPE Conference at Oman Petroleum & Energy Show. SPE, 2022. http://dx.doi.org/10.2118/200079-ms.

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Abstract In order to improve the waterflooding efficiency, surfactants and polymers are added to the water; this process is called surfactant–polymer (SP) flooding. One of the problems for this process is high adsorption of surfactants to the rock surface and specially to carbonate rock surfaces. The focus of this work is: to quantify experimentally the adsorption of anionic surfactants to carbonate rock surfaces, obtain a qualitative understanding of the mechanisms at play and identify suitable adsorption inhibitors. The main outcomes of the work are: the adsorption of the surfactants used ca
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Sain, Ratnanabha, Ganglin Chen, Shiyu Xu, Michael A. Payne, and Akmal Awas Sultan. "Carbonate rock physics: Geophysical and petrophysical pore types of carbonate rocks from an offshore carbonate field." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059226.

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Azuara Diliegros, Brenda, and Roberto Aguilera. "A New Method for Determination of Rock Fabric Number from Well Logs in Unconventional Tight Oil Carbonates." In SPE Canadian Energy Technology Conference. SPE, 2022. http://dx.doi.org/10.2118/208893-ms.

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Abstract This paper develops a new method for estimation of rock fabric number (RFN) from well logs in unconventional tight oil carbonates with less than 0.1 md. The objective is to investigate the oil potential of a Middle Cretaceous tight carbonate in Mexico. Development of a method for these conditions is challenging as the current approach developed by Lucia (1983) has been explained for carbonates with more than 0.1md. The method is calibrated with data from cores and cuttings and allows estimating the presence of grainstone, packstone and wackstone rocks in unconventional tight carbonate
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Boeije, C. S., and W. R. Rossen. "SAG Foam Flooding in Carbonate Rocks." In IOR 2017 - 19th European Symposium on Improved Oil Recovery. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700337.

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Peacock, David C. P., and Andrew Mann. "Controls on fracturing in carbonate rocks." In SPE Middle East Oil and Gas Show and Conference. Society of Petroleum Engineers, 2005. http://dx.doi.org/10.2118/92980-ms.

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Звіти організацій з теми "Rocks, Carbonate"

1

Simandl, G. J., R. J. D'Souza, S. Paradis, and J. Spence. Rare-earth element content of carbonate minerals in sediment-hosted Pb-Zn deposits, southern Canadian Rocky Mountains. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328001.

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Paleozoic platform carbonate rocks of the Rocky Mountains host Mississippi Valley-type (MVT), magnesite, barite, and REE-barite-fluorite deposits. Farther west, platform carbonate rocks of the Kootenay Arc host MVT and fracture-controlled replacement (FCR) deposits. This is the first systematic LA-ICP-MS study of carbonates in MVT and FCR deposits. We investigated seven MVT deposits in the Rocky Mountains, and five MVT deposits in the Kootenay Arc. None of the post-Archean Australian shale (PAAS)-normalized REE profiles show light REE (LREE) depletion and strong negative Ce anomalies character
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2

Lekhov, A. V. Studies of permeability changes and mass transfer in carbonate rocks. Office of Scientific and Technical Information (OSTI), September 1996. http://dx.doi.org/10.2172/760313.

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3

Paradis, S., G. J. Simandl, N. Drage, R J D'Souza, D. J. Kontak, and Z. Waller. Carbonate-hosted deposits (Mississippi Valley-type, magnesite, and REE-F-Ba) of the southeastern Canadian Cordillera: a review and isotopic data comparison. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327995.

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The Mississippi Valley-type, magnesite, and REE-F-Ba deposits in the southeastern Canadian Cordillera are in the weakly deformed/metamorphosed Paleozoic carbonate platform of the Rocky Mountains. Most are hosted in dolostones of the middle Cambrian Cathedral, upper Cambrian Jubilee, and Upper Devonian Palliser formations and spatially associated with hydrothermal dolomite. They occur along structurally controlled facies transitions between the shallow-water carbonate platform and deeper water basin rocks of the Paleozoic continental margin. Their location and morphology reflect episodic riftin
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4

Wood, James R., and William B. Harrison. Advanced Characterization of Fractured Reservoirs in Carbonate Rocks: The Michigan Basin. Office of Scientific and Technical Information (OSTI), December 2002. http://dx.doi.org/10.2172/805238.

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5

James R. Wood and William B. Harrison. ADVANCED CHARACTERIZATION OF FRACTURED RESERVOIRS IN CARBONATE ROCKS: THE MICHIGAN BASIN. Office of Scientific and Technical Information (OSTI), February 2002. http://dx.doi.org/10.2172/834671.

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6

James R. Wood and William B. Harrison. ADVANCED CHARACTERIZATION OF FRACTURED RESERVOIRS IN CARBONATE ROCKS: THE MICHIGAN BASIN. Office of Scientific and Technical Information (OSTI), April 2001. http://dx.doi.org/10.2172/834678.

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7

James R. Wood and William B. Harrison. ADVANCED CHARACTERIZATION OF FRACTURED RESERVOIRS IN CARBONATE ROCKS: THE MICHIGAN BASIN. Office of Scientific and Technical Information (OSTI), April 2000. http://dx.doi.org/10.2172/835050.

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8

James R. Wood and William B. Harrison. ADVANCED CHARACTERIZATION OF FRACTURED RESERVOIRS IN CARBONATE ROCKS: THE MICHIGAN BASIN. Office of Scientific and Technical Information (OSTI), December 2002. http://dx.doi.org/10.2172/826063.

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9

Wood, James R., and William B. Harrison. Advanced Characterization of Fractured Reservoirs in Carbonate Rocks: The Michigan Basin. Office of Scientific and Technical Information (OSTI), October 2000. http://dx.doi.org/10.2172/765659.

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10

Wood, J. R., and W. B. Harrison. Advanced Characterization of Fractured Reservoirs in Carbonate Rocks: The Michigan Basin. Office of Scientific and Technical Information (OSTI), January 2001. http://dx.doi.org/10.2172/773383.

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