Academic literature on the topic 'Geology|Petroleum Geology|Sedimentary Geology'
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Journal articles on the topic "Geology|Petroleum Geology|Sedimentary Geology"
Postma, George. "The geology of fluvial deposits, sedimentary facies, basin analysis and petroleum geology." Sedimentary Geology 110, no. 1-2 (May 1997): 149–50. http://dx.doi.org/10.1016/s0037-0738(96)00081-4.
Full textRoberts, David G. "Sedimentary basins and petroleum geology of the Middle East." Marine and Petroleum Geology 16, no. 4 (June 1999): 379. http://dx.doi.org/10.1016/s0264-8172(99)00008-2.
Full textBosence, Dan. "Sedimentary basins and petroleum geology of the middle east." Journal of African Earth Sciences 28, no. 3 (April 1999): 769–71. http://dx.doi.org/10.1016/s0899-5362(99)00046-9.
Full textWANG, An Sheng, and Noriyuki SUZUKI. "Petroleum geology and geochemistry of Paleogene Nan Xiang lacustrine sedimentary basin, China." Journal of the Japanese Association for Petroleum Technology 57, no. 5 (1992): 415–26. http://dx.doi.org/10.3720/japt.57.415.
Full textCook, R. A., E. M. Crouch, J. I. Raine, C. P. Strong, C. I. Uruski, and G. J. Wilson. "INITIAL REVIEW OF THE BIOSTRATIGRAPHY AND PETROLEUM SYSTEMS AROUND THE TASMAN SEA HYDROCARBON-PRODUCING BASINS." APPEA Journal 46, no. 1 (2006): 201. http://dx.doi.org/10.1071/aj05012.
Full textDrachev, Sergey S. "Chapter 25 Tectonic setting, structure and petroleum geology of the Siberian Arctic offshore sedimentary basins." Geological Society, London, Memoirs 35, no. 1 (2011): 369–94. http://dx.doi.org/10.1144/m35.25.
Full textChalmers, J. A., T. Dahl-Jensen, K. J. Bate, and R. C. Whittaker. "Geology and petroleum prospectivity of the region offshore southern West Greenland – a summary." Rapport Grønlands Geologiske Undersøgelse 165 (January 1, 1995): 13–21. http://dx.doi.org/10.34194/rapggu.v165.8272.
Full textWang, Bing, Harry Doust, and Jingyan Liu. "Geology and Petroleum Systems of the East China Sea Basin." Energies 12, no. 21 (October 26, 2019): 4088. http://dx.doi.org/10.3390/en12214088.
Full textYarboboev, T., Sh Akhmedov, and K. Usmonov. "Features of Distribution of Oil and Gas Deposits in the Earth’s Crust." Bulletin of Science and Practice 6, no. 8 (August 15, 2020): 135–44. http://dx.doi.org/10.33619/2414-2948/57/11.
Full textDrachev, Sergey S. "Erratum to Chapter 25 Tectonic setting, structure and petroleum geology of the Siberian Arctic offshore sedimentary basins." Geological Society, London, Memoirs 35, no. 1 (2011): 819. http://dx.doi.org/10.1144/m35.25err.
Full textDissertations / Theses on the topic "Geology|Petroleum Geology|Sedimentary Geology"
McClave, Graham A. "Stratigraphy and source rock analyses of the Heath Formation in Fergus, Garfield, Golden Valley, Musselshell, Petroleum, and Rosebud counties, central Montana." Colorado School of Mines, 2013.
Find full textStevenson, Mallory. "The Marcellus Shale| Erosional boundary and production analysis, southern West Virginia, U.S.A." Thesis, East Carolina University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=1606661.
Full textThe Middle Devonian Marcellus Shale is a natural gas producing formation that was deposited in the Appalachian foreland basin in what is now eastern North America. An unconformity truncates the Marcellus in southern West Virginia and progressively younger units onlap progressively older units. The zero isopach line that marks the edge of the Marcellus is mapped to reveal the southeastern boundary. A well production analysis is conducted to locate the region of maximum natural gas production. Four lithologic completions intervals in three different well fields are compared. This study shows that the most economically viable drilling is from the Marcellus Shale completion intervals that are less than 30 feet in Chapmanville gas field in western Logan County, West Virginia. Outside of the zero isopach are areas comprised of onlapping featheredges of younger formations that comprise a black shale unit mistakenly identified as “Marcellus Shale”. These areas produce significantly less gas than the “true” Marcellus Shale.
Torn, Daniel. "Sedimentology and stratigraphy of diatomaceous sediments in the Casmalia Hills and Orcutt oil fields in the Santa Maria basin, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1528056.
Full textTwo industry acquired diatomite cores (Sisquoc Formation) from the Orcutt (Newlove 76-RD1) and Casmalia Hills (Stokes A-30804) oil fields were analyzed by core descriptions, laboratory analysis (XRD and SEM), and gamma ray logs. Based on these data, five distinct lithofacies, nine sedimentary features and compositional trends of both cores were established. Newlove 76-RD1 and Stokes A-30804 record an upward-shallowing succession at different depositional positions on the Pliocene paleo-slope of the Santa Maria basin. Stokes A-30804 reflects slope deposition on a lower flank of a paleo-bathymetric high receiving higher detrital influx from inter-ridge troughs. Slope deposition of Newlove 76-RD1 was closer to a paleo-bathymetric high where purer diatomaceous sediments accumulated. Within Stokes A-30804, purer opal-A dominant lithofacies contain the highest oil saturations. The diagenesis and precipitation of opal-CT and abundance of phyllosilicate significantly hinders oil saturation within lithofacies.
Brooke, James Michael. "Geologic analysis of the Upper Jurassic Cotton Valley Formation in Jefferson County, Mississippi." Thesis, Mississippi State University, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1570118.
Full textThough the Cotton Valley Group is productive in Mississippi, Louisiana, and Texas, little is known about production potential of the Bossier Formation (Lower Cotton Valley Shale) in southwest Mississippi. The Bossier Formation in Jefferson County, Mississippi is an organic-poor, carbonate-rich mudrock with siliciclastic intervals. Examination of cuttings by petrographic and scanning electron microscopy revealed fractures that have been filled by calcite and pore-filling pyrite. Porosity exists within and around pyrite framboids, in unfilled fractures, and within peloid grains. Organic matter is rare in Lower Cotton Valley samples suggesting it is not self-sourcing. Total Organic Carbon (TOC) values are low (0.86-1.1% TOC) compared to the productive Haynesville Shale Formation (2.8% TOC). Porosity of the Lower Cotton Valley Shale is low (2.5-4.2%) compared to productive Haynesville Shale Formations (8-12%). With current technology and gas prices, the Lower Cotton Valley Shale in Jefferson County, Mississippi does not have production potential.
Hunt, John Edward. "Conodont Biostratigraphy in Middle Osagean to Upper Chesterian Strata, North-Central Oklahoma, U.S.A." Thesis, Oklahoma State University, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10690774.
Full textThe informally known “Mississippian Limestone” stratigraphic interval in north-central Oklahoma, U.S.A. bears no chronostratigraphic markers and has no formally established biostratigraphic framework to date. Conodonts collected from four “Mississippian Limestone” cores in Logan, Payne, and Lincoln Counties provide the means for better constraining the stratigraphic age of the interval over the area studied. Conodont extraction was conducted by acid digestion of whole-rock samples and heavy liquid density separation after which conodont genera and species types were identified from scanning electron microscopy. Biostratigraphically significant conodonts recovered in combination with chemostratigraphic work by Dupont (2016) and earlier studies by Thornton (1958), Curtis and Chaplin (1959), McDuffie (1959), Rowland (1964), Selk and Ciriacks (1968), and Harris (1975) indicate the “Mississippian Limestone” ranges from middle Osagean to late Chesterian in age. In general, conodont element recoveries were too low in quantity and too poor of quality for use as biostratigraphic markers. The relatively low recovery and poor preservation quality of the conodont elements are attributed primarily to the elements being reworked soon after deposition by frequent storms on a mid- to outer-ramp environment in a low-latitude carbonate ramp setting. The results of this investigation are most significant in that they help place Mississippian deposition over the area studied within the context of a global Carboniferous stratigraphy. The results also allow for the Mississippian interval in the study area to be more accurately related to time-correlative strata with similar or better age constraint for constructing more temporally meaningful depositional models of the Oklahoma basin.
Dubois, Kalli Alyse. "Regional Stratigraphy and Lithologic Characterization of the Tuscaloosa Marine Shale in Southwest Mississippi." Thesis, Mississippi State University, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10843538.
Full textThe Tuscaloosa Marine Shale (TMS) in southwest Mississippi and south-central Louisiana has potential to become a prolific source of fossil fuels using hydraulic fracturing technology. The objective of this study is to better understand the sequence and regional stratigraphy, lithology, and character of the TMS. Studying the TMS’s lithologic, depositional, and diagenetic properties is essential to maximize potential production. Characterization of the eastern TMS was performed with cuttings from two wells provided by the Mississippi Oil and Gas Board through MDEQ, and two provided by the USGS. Thirty-one petrophysical logs were correlated, to make cross sections and trace sequence stratigraphic intervals within the TMS. Results of the study showed lithologic variability and compaction across the study area, and a sequence stratigraphic correlation of the highstand systems track between the Tuscaloosa and Eagle Ford Groups. This research aims to work toward the greatest potential of the TMS as an unconventional reservoir.
Liner, Thomas. "Subsurface Analysis of Mississippian Tripolitic Chert in Northwest Arkansas." Thesis, University of Arkansas, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10975846.
Full textOver the past 70 years the Mississippian strata of Northwest Arkansas have been studied in great detail. The study area is located on the escarpment between the Boston Mountains Plateau and the Springfield Plateau where a surface occurrence of Mississippian age rock allows for access to outcrops in close proximity to gas wells that encounter subsurface Mississippian strata. Many outcrops found in Northwest Arkansas expose Lower Mississippian (Kinderhookian-Osagean) strata that represent a full third order transgressive/regressive sequence that is unconformity bounded. These Mississippian outcrops are commonly treated as surface analogs to the Mississippi Lime Play in North Central Oklahoma. This thesis focuses on the analysis of Boone tripolitic chert in the subsurface utilizing wireline data available from selected gas wells within the study area. The primary goal of this project is to determine and quantify the subsurface stratigraphic position of tripolitic chert from wells that cut a complete section of the Boone Formation. 24 of the 27 (89%) wells within the study with bulk density logs penetrated a substantial section of the Boone Formation and confirmed the presence of tripolite through a density value less than 2.1 g/cc.
Analysis of wireline data from selected wells is used to characterize the Mississippian system with a specific focus on the distribution of tripolitic chert. Correlation of Mississippian gas production to tripolitic chert occurrence along with the correlation of subsurface data with outcrop data are secondary objectives.
Barker, Abram Max. "An Integrated Well Log and 3D Seismic Interpretation of Missourian Clinoforms, Osage County, Oklahoma." Thesis, University of Arkansas, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10981180.
Full textIntegrated analysis of well and geophysical data can provide detailed geologic interpretation of the subsurface in Osage County, Oklahoma. Systems tracts and depositional system successions can be interpreted at marginal seismic resolution using well log motif with seismic reflector character within a depositional context. Shelf-prism and subaqueous, delta-scale clinoforms of Missourian age observed in 3D seismic were interpreted with greater sequence stratigraphic detail when coupled with wireline well logs. The Late Pennsylvanian Midcontinent Sea was thought to be approximately 150 feet average depth across the southern Midcontinent during the Missourian Stage, and deepen towards the Arkoma and Anadarko Basins to the south. Here we show that the Late Pennsylvanian Midcontinent Sea floor was in water depths greater than 600 feet and sloped to the southeast, toward major, southern basins, during the Missourian Stage in Osage County. Shelf-prism and delta scale clinoforms up to 600 and 300 feet of relief, respectively, were observed in paired seismic and well log cross sections, thickness maps, and structure maps dipping northwest at 052° strike, upon a basin floor dipping southeast at 253° strike. Lithologic and sequence stratigraphic interpretation revealed a mixed carbonate-siliciclastic system comprising of delta, offshore shelf, and carbonate buildup depositional systems of mesothem, 3rd order sequence magnitude. The observed succession included: 1) falling stage to lowstand, sand-prone, subaqueous delta, 2) transgressive to highstand offshore shelf and carbonate bank, and 3) falling stage delta. The depositional sucession demonstrates how carbonate banks related spatially to terrigenous sediment input in northeastern Oklahoma during the Late Pennsylvanian because of glacio-eustasy and possible tectonism.
Mosher, Annie. "Detailed lithostratigraphic characterization of Chico Martinez Creek, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1527400.
Full textA 6012-foot Monterey Formation succession at Chico Martinez Creek, San Joaquin basin, is characterized at high spatial resolution by spectral gamma-ray data in 2- foot increments, 5-foot lithologic descriptions, and qualitative XRD and FTIR analysis. Based on these data, the 4 Monterey members–the Gould, Devilwater, McDonald and Antelope shales–are subdivided into 7 distinctive lithofacies. New paleomagnetic data, combined with industry-provided biostratigraphy establishes a chronostratigraphic framework and allows determination of linear sediment accumulation rates. Condensed sedimentation at the onset of McDonald deposition (~14 Ma) is also observed in correlative members in the Pismo, Santa Maria and Santa Barbara basins. This regional event is associated with eustatic regression from the Mid-Miocene highstand related to formation of the East Antarctic Ice Sheet and ongoing thermotectonic basin subsidence. A surge in linear sediment accumulation rates in the siliceous upper McDonald and Antelope (~10.4 Ma) is attributed to a regional increase in diatom productivity.
Stobart, Ryan Patrick. "The Kaskaskia-Absaroka Boundary in the Subsurface of Athens County, Ohio." Ohio University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1574437212920114.
Full textBooks on the topic "Geology|Petroleum Geology|Sedimentary Geology"
pétrole, Institut français du, ed. Sedimentary geology: Sedimentary basins, depositional environments, petroleum formation. Paris: Editions Technip, 2002.
Find full textThe geology of fluvial deposits: Sedimentary facies, basin analysis, and petroleum geology. Berlin: Springer, 1996.
Find full textMiall, Andrew D. The geology of fluvial deposits: Sedimentary facies, basin analysis, and petroleum geology. 4th ed. Berlin: Springer, 2011.
Find full textM, Nairn A. E., ed. Sedimentary basins and petroleum geology of the Middle East. Amsterdam: Elsevier, 1997.
Find full textSelley, R. C. Ancient sedimentary enviroments: And their sub-surface diagnosis. 3rd ed. London: Chapman & Hall, 1985.
Find full textOrganization of Arab Petroleum Exporting Countries. Technical Department. Jīyūlūjīyat baʻḍ al-aḥwāḍ al-tarsībīyah fī al-Sharq al-Awsaṭ wa-imkānīyātuhā al-batrūlīyah. [Kuwait]: [Munaẓẓamat al-Aqṭār al-ʻArabīyah al-Muṣaddirah lil-Batrūl, Awābik], 2010.
Find full textDong bei Ya chen ji pen di de xing cheng yan hua ji qi han you qi yuan jing. Beijing: Di zhi chu ban she, 1997.
Find full textTian, Zaiyi. Petroliferous sedimentary basins in China and basin analysis. Beijing, China: Petroleum Industry Press, 1997.
Find full text1953-, Allen John R., ed. Basin analysis: Principles and applications. 2nd ed. Malden, MA: Blackwell Pub., 2005.
Find full text1953-, Allen John R., ed. Basin analysis: Principles and applications. Oxford [England]: Blackwell Scientific Publications, 1990.
Find full textBook chapters on the topic "Geology|Petroleum Geology|Sedimentary Geology"
Bjørlykke, Knut Olav. "Sedimentary Facies." In Sedimentology and Petroleum Geology, 55–111. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-72592-0_5.
Full textBjørlykke, Knut Olav. "Description of Sedimentary Rocks and Facies." In Sedimentology and Petroleum Geology, 35–54. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-72592-0_4.
Full textWeimer, Paul, and Martin H. Link. "Global Petroleum Occurrences in Submarine Fans and Turbidite Systems." In Frontiers in Sedimentary Geology, 9–67. New York, NY: Springer New York, 1991. http://dx.doi.org/10.1007/978-1-4684-8276-8_2.
Full textWilde, Pat, William R. Normark, T. E. Chase, and Christina E. Gutmacher. "Potential Petroleum Reservoirs on Deep-Sea Fans off Central California." In Frontiers in Sedimentary Geology, 35–42. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5114-9_7.
Full textLindsay, John F., and John D. Gorter. "Clastic Petroleum Reservoirs of the Late Proterozoic and Early Paleozoic Amadeus Basin, Central Australia." In Frontiers in Sedimentary Geology, 39–74. New York, NY: Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4757-0160-9_3.
Full textSchofield, Nick, Dougal A. Jerram, Simon Holford, Stuart Archer, Niall Mark, Adrian Hartley, John Howell, et al. "Sills in Sedimentary Basins and Petroleum Systems." In Physical Geology of Shallow Magmatic Systems, 273–94. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/11157_2015_17.
Full textSchofield, Nick, Dougal A. Jerram, Simon Holford, Stuart Archer, Niall Mark, Adrian Hartley, John Howell, et al. "Sills in Sedimentary Basins and Petroleum Systems." In Physical Geology of Shallow Magmatic Systems, 273–94. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-14084-1_17.
Full textLafoy, Y. "The Sedimentary Basins of the New Caledonia Region." In Hydrocarbon and Petroleum Geology of France, 427–29. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-78849-9_31.
Full textBouysse, Ph, and A. Mascle. "Sedimentary Basins and Petroleum Plays Around the French Antilles." In Hydrocarbon and Petroleum Geology of France, 431–43. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-78849-9_32.
Full textAlsharhan, A. S., and A. E. M. Nairn. "PREFACE." In Sedimentary Basins and Petroleum Geology of the Middle East, v—vi. Elsevier, 2003. http://dx.doi.org/10.1016/b978-044482465-3/50000-0.
Full textConference papers on the topic "Geology|Petroleum Geology|Sedimentary Geology"
Witte, Jan, Daniel Trümpy, Jürgen Meßner, and Hans Georg Babies. "Petroleum Potential of Rift Basins in Northern Somalia – A Fresh Look." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2573746-ms.
Full textKhomsi, S., M. M. Turki, H. Zouari, and D. Turki. "Structural Inheritance and Tectono-Sedimentary Analysis in Amdoun Zone, North Tunisia." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406049.
Full textPérez-Belzuz, F., B. Alonso, and A. Galimont. "High-Frequency Sea-Level Changes Control the Recent Sedimentary Architecture of a Small Modern Turbidite System." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406002.
Full textLebreiro, S., and B. Alonso. "Sedimentary Activity of the Guadiaro Turbidite System During the Last Deglaciation to Holocen, SW Alboran Sea." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406077.
Full textH. Negra, M., B. Mardassi, and S. Melk. "Sedimentary Characters Changes in Fractured Micritic Reservoirs - Example of the Abiod-Bou Dabbous Formations in Northern Tunisia." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406047.
Full textAlmalki, F., and S. Hayton. "Sedimentary facies and depositional environments of an Early Silurian sandstone." In Seventh Arabian Plate Geology Workshop: Pre-Cambrian to Paleozoic Petroleum Systems in the Arabian Plate. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201900216.
Full textWu, Ivan Zhia, Sarvagya Parashar, Banu Andhika, Susan Syahdina, Arrie Kurniawan, Yoga Wismoyo, and Muhammad Ardhyan Jannatan. "Sand Body Trend Delineation Decrypting from Stratigraphic Dip Pattern Analysis: Case Study within a Fluvio-Deltaic Setting, East Kalimantan, Indonesia." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21466-ms.
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