Relevant bibliographies by topics / Stratigraphic Limestone Diagenesis Lithofacies

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  2. Dissertations / Theses
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Academic literature on the topic 'Stratigraphic Limestone Diagenesis Lithofacies'

Author: Grafiati
Published: 4 June 2021
Last updated: 16 February 2022

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Journal articles on the topic "Stratigraphic Limestone Diagenesis Lithofacies"

1

Suriamin, Fnu, and Matthew J. Pranter. "Stratigraphic and lithofacies control on pore characteristics of Mississippian limestone and chert reservoirs of north-central Oklahoma." Interpretation 6, no. 4 (2018): T1001—T1022. http://dx.doi.org/10.1190/int-2017-0204.1.

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We have determined how stratigraphy and lithofacies control pore structures in the Mississippian limestone and chert reservoir of north-central Oklahoma. There are 17 lithofacies and 29 high-frequency cycles documented in the Mississippian interval of this study. The high-frequency cycles have thicknesses ranging from 0.3 to 30.5 m (1–100 ft) and are mainly asymmetric regressive phases. The pore characteristics, measured through digital-image analysis (DIA) of thin-sections photomicrographs ([Formula: see text]100), exhibit unique correlations with core porosity, permeability, and lithofacies
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Cather, Martha, Dylan Rose-Coss, Sara Gallagher, et al. "Deposition, Diagenesis, and Sequence Stratigraphy of the Pennsylvanian Morrowan and Atokan Intervals at Farnsworth Unit." Energies 14, no. 4 (2021): 1057. http://dx.doi.org/10.3390/en14041057.

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Farnsworth Field Unit (FWU), a mature oilfield currently undergoing CO2-enhanced oil recovery (EOR) in the northeastern Texas panhandle, is the study area for an extensive project undertaken by the Southwest Regional Partnership on Carbon Sequestration (SWP). SWP is characterizing the field and monitoring and modeling injection and fluid flow processes with the intent of verifying storage of CO2 in a timeframe of 100–1000 years. Collection of a large set of data including logs, core, and 3D geophysical data has allowed us to build a detailed reservoir model that is well-grounded in observation
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Abbaszadeh, Maghsood, Naoki Koide, and Yoya Murahashi. "Integrated Characterization and Flow Modeling of a Heterogeneous Carbonate Reservoir in Daleel Field, Oman." SPE Reservoir Evaluation & Engineering 3, no. 02 (2000): 150–59. http://dx.doi.org/10.2118/62514-pa.

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Summary This article presents applications of deterministic and conditional geostatistical reservoir characterization methods to the heterogeneous carbonates of the upper Shuaiba formation in Daleel field, Oman. High-resolution reservoir descriptions based on the integration of logs, core, pressure transient tests, geology, and seismic data are constructed; and upscaled for use in reservoir simulation models to history match field performance data. Generally, geostatistical techniques combined with geology and proper upscaling of permeability heterogeneity yield best results without artificial
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4

Cahyaningsih, Catur, Anjas Latif Ritonga, Shaury Aldila, and Zulhikmah Zulhikmah. "Lithofacies And Depositional Analysis Environment Of West Section Kolok Nan Tuo Village, Sawahlunto City, West Of Sumatera." Journal of Geoscience, Engineering, Environment, and Technology 3, no. 2 (2018): 128. http://dx.doi.org/10.24273/jgeet.2018.3.2.340.

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Research areas were located in the west of Kolok Nan Tuo Village. Geographically this area is located at coordinates 00 ° 36'57,85 '' - 00 ° 37'56,89 '' latitude and 100 ° 42'10,08 '' 100 ° 43'47,28 " BT. The methods used in research is geological mapping. Based on the results of stratigraphic research area is divided into three units consist of: Crystalline Limestone Unit (SBGK) consisting Crystalline Limestone of and mudstone lithofacies, Conglomerate Units (SK) consists of polymic conglomerate and sandstones greywacke lithofacies while claystone Unit (SBL) lithofacies consists of claystone
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Qureshi, Kamil Ahmed, Muhammad Raza Shah, Ishaque Ali Meerani, Shah Fahad, Hamid Hussain, and Umer Habib. "Sedimentology and Economic Significance of Hangu Formation, Northwest Pakistan." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 48–55. http://dx.doi.org/10.46660/ijeeg.vol11.iss1.2020.411.

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The Hangu Formation (Paleocene) consists of sandstone, siltstone, carbonaceous shale, coal and laterite. It is well exposed in the Trans Indus Surghar range and the southern Hazara basin. The sandstone is yellowish brown, fine to coarse grained and medium to thick bedded. The sandstone of the Hangu Formation is classified as quartz arenite on the Q-F-L diagram. It is mostly grain supported and are cemented by silica cement. The study of different stratigraphic sections reveal that Hangu Formation can be sub-divided into a number of lithofacies on the basis of sedimentary structures and litholo
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Qureshi, Kamil Ahmed, Muhammad Raza Shah, Ishaque Ali Meerani, Shah Fahad, Hamid Hussain, and Umer Habib. "Sedimentology and Economic Significance of Hangu Formation, Northwest Pakistan." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 48–55. http://dx.doi.org/10.46660/ojs.v11i1.411.

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The Hangu Formation (Paleocene) consists of sandstone, siltstone, carbonaceous shale, coal and laterite. It is well exposed in the Trans Indus Surghar range and the southern Hazara basin. The sandstone is yellowish brown, fine to coarse grained and medium to thick bedded. The sandstone of the Hangu Formation is classified as quartz arenite on the Q-F-L diagram. It is mostly grain supported and are cemented by silica cement. The study of different stratigraphic sections reveal that Hangu Formation can be sub-divided into a number of lithofacies on the basis of sedimentary structures and litholo
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7

Abdullah, Mustafa A., Faris N. Hassan, and Abdulsalam M.Saleh. "Microfacies and Palaeoenvironment of Avanah Formation (Middle Eocene) Geli Bessri in Dohuk City / North of Iraq." Tikrit Journal of Pure Science 25, no. 1 (2020): 85. http://dx.doi.org/10.25130/j.v25i1.940.

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This research is based on (23) Samples selected from the Avanah Formation (Middle Eocene) in the Geli Bessri section in Dohuk to recognize the microfacies and depositional environments. The Avanah Formation consists of rocks of marly limestone and limestone containing Alveolina and thin layers of sandstone lithofacies found in the lower part of the Formation. The depositional environment was determined depending on skeletal and non- skeletal grains. The facies of the Avanah Formation were divided into four main microfacies and four submicrofacies based on skeletal and non- skeletal grains: The
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8

Peng, Jun, Ledan Yu, Tianyu Xu, Yubin Wang, and Haodong Han. "Analysis of Sedimentary Environment Conditions for Lacustrine Fine-Grained Sedimentary Rocks and Its Control of Lithofacies Development: A Case Study of the Lower Submember of Member 3 of Shahejie Formation in FY-1 Well, Dongying Sag, Bohai Bay Basin, China." Geofluids 2021 (September 12, 2021): 1–16. http://dx.doi.org/10.1155/2021/6640706.

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In recent years, the studies on fine-grained sedimentation mainly focus on the rock type, sedimentary environment, sedimentation, and sequence stratigraphy, while those on the relationship between sedimentary environment and lithofacies development are rare. However, a clear understanding on the relationship is of great significance to the muddy shale oil and gas exploration. This paper studied the muddy shale of semideep and deep lacustrine facies in the lower submember of Member 3 of Shahejie Formation in FY-1 Well, Dongying Sag, Bohai Bay Basin, East China. Based on geochemical data, the se
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Messent, B. E. J., C. Wilson, and K. Flynn. "ASSESSMENT OF THE SEAL POTENTIAL OF TERTIARY CARBONATES, DUNTROON BASIN, SOUTH AUSTRALIA." APPEA Journal 36, no. 1 (1996): 233. http://dx.doi.org/10.1071/aj95013.

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The seal potential of the Wilson Bluff and Nullarbor Limestone Formations was assessed over high-graded Pidinga Formation leads of the Duntroon Basin that contain significant hydrocarbon potential. The work quantified the risk associated with these plays. Regional geological knowledge was integrated with the results of special core analysis and petrography to address the 3 critical aspects of seal quality: seal capacity, seal geometry and seal integrity.This work established a clear relationship between seal potential and lithofacies, namely, the higher the clastic content, the better the seal
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10

Cecca, Fabrizio, Berengere Savary, Annachiara Bartolini, Juergen Remane, and Fabrice Cordey. "The Middle Jurassic-Lower Cretaceous Rosso Ammonitico succession of Monte Inici (Trapanese Domain, western Sicily); sedimentology, biostratigraphy and isotope stratigraphy." Bulletin de la Société Géologique de France 172, no. 5 (2001): 647–59. http://dx.doi.org/10.2113/172.5.647.

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Abstract The pelagic Jurassic successions of the Trapani region of western Sicily are dominated by the characteristic Tethyan Rosso Ammonitico lithofacies. In order to revise the stratigraphy (sedimentology, microbiofacies, ammonite and calpionellid biostratigraphy, isotope stratigraphy) and to define a reference section, a well exposed succession of Rosso Ammonitico, spanning the Callovian-Upper Berriasian interval, has been selected in the eastern sector of Monte Inici, Trapani province. A sedimentological study has enabled us to distinguish three subfacies within the Rosso Ammonitico: nodul
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Dissertations / Theses on the topic "Stratigraphic Limestone Diagenesis Lithofacies"

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Kanō, Akihiro. "Deposition, palaeoecology, and diagenesis of the Silurian reef-like limestones on Gotland." Stockholm : Dept. of Geology and Geochemistry, University of Stockholm, 1990. http://catalog.hathitrust.org/api/volumes/oclc/23697432.html.

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Monreal, Rogelio. "Lithofacies, depositional environments, and diagenesis of the Mural limestone (Lower Cretaceous), lee siding area, Cochise County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558029.

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3

Ahsan, Mustafa. "Integrated subsurface study on lithofacies and diagenetic controls over porosity distribution in the Upper Ordovician Trenton Limestone in Northwestern Ohio." Bowling Green State University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1546435185616111.

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4

Osborn, Caleb R. "Microfacies Analysis, Sedimentary Petrology, and Reservoir Characterization of the Sinbad Limestone Based Upon Surface Exposures in the San Rafael Swell, Utah." BYU ScholarsArchive, 2007. https://scholarsarchive.byu.edu/etd/1414.

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The Lower Triassic Sinbad Limestone Member of the Moenkopi Formation has produced minor amounts of oil in the Grassy Trail Creek field near Green River, Utah and is present below much of central Utah including the recently discovered Covenant field. Superb outcrops of this thin (15 m), mixed carbonate-silicilastic unit in the San Rafael Swell permit detailed analysis of its vertical and lateral reservoir heterogeneity. Vertically, the Sinbad Limestone comprises three facies associations: (A) a basal storm-dominated, well-circulated skeletal-oolitic-peloidal limestone association, (B) a storm-d
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Desrochers, Andre. "The lower and middle ordovician platform carbonates of the Mingan Islands, Quebec : stratigraphy, sedimentology, paleokarst, and limestone diagenesis /." 1985. http://collections.mun.ca/u?/theses,102471.

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Books on the topic "Stratigraphic Limestone Diagenesis Lithofacies"

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Armstrong, Augustus K. Facies, diagenesis, and mineralogy of the Jurassic Todilto Limestone Member, Grants uranium district, New Mexico. New Mexico Bureau of Mines & Mineral Resources, 1995.

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2

Ryder, Robert T. Stratigraphic framework of Cambrian and Ordovician rocks in the central Appalachian basin from Morrow County, Ohio, to Pendleton County, West Virginia. U.S. G.P.O., 1992.

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3

Hoffmann, Heidi. Depositional and diagenetic model for the Middle Devonian Denay Limestone, northern Antelope Range, Eureka County, Nevada. 1989.

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4

Collamer, Stephen Vaughn. Aspects of deposition and diagenesis in the lower Ordovician rockview member (Axemann limestone) in the vicinity of Bellefonte and State College, Pennsylvania. 1985.

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Conference papers on the topic "Stratigraphic Limestone Diagenesis Lithofacies"

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Gill, M. Mehboob. "Diagenesis, Depositional Model and Stratigraphic Evolution of the Margalla Hill Limestone, Southeast Hazara." In 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202010215.

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