Relevant bibliographies by topics / Sandstones of Seis

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Academic literature on the topic 'Sandstones of Seis'

Author: Grafiati
Published: 24 April 2022
Last updated: 30 July 2025

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Journal articles on the topic "Sandstones of Seis"

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Della Fávera, Jorge Carlos, Hernani Aquini Fernandes Chaves, Marco André Malmann Medeiros, et al. "STRATIGRAPHIC ANALYSIS OF THE ARATU STAGE (LOWER CRETACEOUS), RECÔNCAVO BASIN (BRAZIL), WITH HYDROCARBON RESERVOIR ROCKS." Journal of Sedimentary Environments 4, no. 2 (2019): 199–219. http://dx.doi.org/10.12957/jse.2019.43784.

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The section between the 7 and 11 electric markers in the Aratu Stage of the Recôncavo Basin (Lower Cretaceous) has been studied in order to perform a stratigraphic analysis. This section bear reservoir rocks known as Imbé, Cambuqui and Miranga sandstones. It produces petroleum in fields like Miranga, Araçás, Taquipe, Miranga Norte and Imbé.The isopach map showed a general trend of increased subsidence for south and southeast. A series of structural lows surround the platform region known as Quiricó High. Southwestward, the Taquipe Canyon is an indication of the lake deepening in that region.In
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Khalifazadeh, Ch M., S. Y. Hamashaeva-Muradova, and M. J. Hamashaeva. "Paleogeographical model of the late upper Pliocene eastern Azerbaijan and the Middle Kurin depression." Azerbaijan Oil Industry, no. 12 (December 15, 2024): 4–8. https://doi.org/10.37474/0365-8554/2024-12-4-8.

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The paleogeography of the late Pliocene is poorly studied. Meanwhile, more detailed studies of the paleogeography of the late Pliocene are of great importance for understanding the historical and geological development of the Pliocene-anthropogenic structural stage within the Southern Caspian and Eastern Azerbaijan. We have created a paleogeographic model based on the generalization of a huge amount of factual material - regional geophysical works, stratigraphic-paleontological data and complex sedimentological research.Late Upper Pliocene seas are characterized by their salinization and the d
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Pratt, Brian R., and Juan J. Ponce. "Sedimentation, earthquakes, and tsunamis in a shallow, muddy epeiric sea: Grinnell Formation (Belt Supergroup, ca. 1.45 Ga), western North America." GSA Bulletin 131, no. 9-10 (2019): 1411–39. http://dx.doi.org/10.1130/b35012.1.

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AbstractInterpreting the deposits of ancient epeiric seas presents unique challenges because of the lack of direct modern analogs. Whereas many such seas were tectonically relatively quiescent, and successions are comparatively thin and punctuated by numerous sedimentary breaks, the Mesoproterozoic Belt Basin of western North America was structurally active and experienced dramatic and continuous subsidence and sediment accumulation. The Grinnell Formation (ca. 1.45 Ga) in the lower part of the Belt Supergroup affords an opportunity to explore the interplay between sedimentation and syndeposit
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Richardson, Larry J., and Dennis E. Hedke. "Seismic Expression of a Subtle Stratigraphic Trap, Lexington Field, Clark County, Kansas." Bulletin (Kansas Geological Survey), no. 237 (April 16, 2024): 103–11. https://doi.org/10.17161/kgsbulletin.no.237.20432.

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Lexington field is located in northeastern Clark County, Kansas, principally in secs. 19 and 20, T. 31 S., R. 21 W. Geologically, the field is situated on the northeastern shelf of the Hugoton embayment of the Anadarko basin, near the eastern limit of Morrowan Stage deposition. The field has yielded over 4 million bbls of oil and about 4 BCF gas from combined Morrow and Mississippian reservoirs. Fluvial sandstones within the Morrow section are responsible for over 96% of the oil and about 75% of the gas produced from the field. Productive Morrow sandstones within the field were deposited in a
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Finney, Stanley C., and Raymond L. Ethington. "Graptolite and conodont faunas in Ordovician Vinini Formation, Roberts Mountains, central Nevada, demonstrate that the Roberts Mountains allochthon is not an exotic terrane." Paleontological Society Special Publications 6 (1992): 97. http://dx.doi.org/10.1017/s2475262200006572.

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Two very different plate-tectonic models have been proposed to explain the development and emplacement of the Robert Mountains allochthon (RMA) onto the North America craton during the Late Devonian-Early Mississippian Antler Orogeny. In one model, the RMA represents a far-traveled accretionary prism that migrated eastwards over a west-dipping subduction zone. In the other, the eugeoclinal strata of the RMA were deposited on the continental rise of western North America within a closed back-arc basin. Siliciclastic sediments, especially quartz sandstones, compose much of the RMA, yet knowledge
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Carr, Timothy R., Neil L. Anderson, and Tim Pulliam. "Case History of Walta Field (Simpson and Mississippian), Sumner County, Kansas." Bulletin (Kansas Geological Survey), no. 237 (April 16, 2024): 153–57. https://doi.org/10.17161/kgsbulletin.no.237.20438.

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Walta field (448 MBO) is a small field located in Sumner County, Kansas (principally in secs. 19 and 30, T. 33 S., R. 3 W., and sec. 25, T. 33 S., R. 4 W.). Cumulative production of 448 MBO is principally from a sandstone traditionally assigned to the uppermost Simpson Group (Middle Ordovician), but which may be Misener (Upper Devonian-Lower Mississippian), the basal transgressive sand below the Chattanooga Shale. Secondary production is from the Mississippian (Osagean) "chat" just beneath the sub-Pennsylvanian unconformity. Production at the Mississippian level is structurally trapped, but de
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Lovegrove, Jack, Andrew J. Newell, David I. Whiteside, and Michael J. Benton. "Testing the relationship between marine transgression and evolving island palaeogeography using 3D GIS: an example from the Late Triassic of SW England." Journal of the Geological Society 178, no. 3 (2021): jgs2020–158. http://dx.doi.org/10.1144/jgs2020-158.

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The Rhaetian transgression marked a major change in landscape. The Permian and Triassic had been a time of terrestrial conditions across Europe, including much of mainland UK, as well as the North Sea and Irish Sea, represented by red bed clastic successions. Seas flooded across Europe at 205.7 Ma and the shift from terrestrial to marine environments is marked in the UK by the switch from the red beds of the Mercia Mudstone Group to the black mudstones and shelly limestones and sandstones of the Penarth Group. The area around Bristol was marked by a complex landscape in which an archipelago of
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Ponciano, Luiza Corral Martins de Oliveira, Deusana Maria da Costa Machado, Ana Carolina Gelmini de Faria, Ana Carolina Maciel, Juliana Matos, and Mariana Novaes. "Hábitos de vida dos Gastropoda e Bellerophontida da formação Maecuru, Devoniano Médio, Bacia do Amazonas, Brasil." Anuário do Instituto de Geociências 30, no. 1 (2007): 197–203. http://dx.doi.org/10.11137/2007_1_197-203.

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The Maecuru Formation comprises the Devonian-Carboniferous sedimentary sequence of Amazonas Basin and consists of fluvialdeltaics to neritics sandstones and pelites layers. Its fossiliferous sediments (the uppermost part of the Lontra Member) consists of hummocky cross-stratified fine-grained to very coarse sandstones beds.With the purpose of adding more information about the palaeoecology of The Maecuru Formation fossils, the life habits of gastropods and bellerophontids were inferred based on functional analysis and similarities with the living forms. The more significant features used were:
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Langford, R. P., K. M. Pearson, K. A. Duncan, D. M. Tatum, L. Adams, and P. A. Depret. "Eolian Topography as a Control on Deposition Incorporating Lessons from Modern Dune Seas: Permian Cedar Mesa Sandstone, SE Utah, U.S.A." Journal of Sedimentary Research 78, no. 6 (2008): 410–22. http://dx.doi.org/10.2110/jsr.2008.045.

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Jeans, C. V., D. S. Wray, R. J. Merriman, and M. J. Fisher. "Volcanogenic clays in Jurassic and Cretaceous strata of England and the North Sea Basin." Clay Minerals 35, no. 1 (2000): 25–55. http://dx.doi.org/10.1180/000985500546710.

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AbstractThe nature and origin of authigenic clay minerals and silicate cements in the Jurassic and Cretaceous sediments of England and the North Sea are discussed in relation to penecontemporaneous volcanism in and around the North Sea Basin. Evidence, including new REE data, suggests that the authigenic clay minerals represent the argillization of volcanic ash under varying diagenetic conditions, and that volcanic ash is a likely source for at least the early silicate cements in many sandstones. The nature and origin of smectite-rich, glauconite-rich, berthierine-rich and kaolin-rich volcanog
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Books on the topic "Sandstones of Seis"

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Ali, Syed A., Leonard Kalfayan, and Carl T. Montgomery. Acid Stimulation. Society of Petroleum Engineers, 2016. http://dx.doi.org/10.2118/9781613994269.

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Stimulation of oil, gas, and injection wells with acid is almost as old as the petroleum engineering industry itself. Acid Stimulation, ensures a comprehensive and up-to-the-minute presentation by 19 subject matter experts, all at the forefront of the development of acidizing technology. Each chapter delivers an authoritative presentation of the key areas of Acid Stimulation, providing an important resource for anyone who designs, analyzes, and/or improves acidizing treatments. Acid Stimulation includesA concise review of the tremendous amount of information that has been gathered on the subje
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Book chapters on the topic "Sandstones of Seis"

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Walker, Roger G. "ANCIENT EXAMPLES OF TIDAL SAND BODIES FORMED IN OPEN, SHALLOW SEAS." In Shelf Sands and Sandstone Reservoirs. SEPM (Society for Sedimentary Geology), 1985. http://dx.doi.org/10.2110/scn.85.13.0303.

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Barton, Mark D., Edward S. Angle, and Noel Tyler. "Stratigraphic Architecture of Fluvial-Deltaic Sandstones from the Ferron Sandstone Outcrop, East-Central Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c7.

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Abstract The Cretaceous Ferron Sandstone is a fluvial-deltaic system that is superbly exposed along the western flank of the San Rafael Swell in east-central Utah. The Ferron consists of fluvial, near shorezone, and shallow-marine strata that were deposited along the active margin of an evolving foreland basin. The 180-m-thick (590-ft) Ferron Sandstone forms an east- to northeast-thinning clastic wedge that is bounded by marine strata and pinches out over the distance of 40 km (25 mi). Numerous local transgressive intervals further subdivide the Ferron into 10-20-m (30-60-ft) thick successions
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Bergh, T. C. V. van den, and James R. Garrison. "The Geometry, Architecture, and Sedimentology of Fluvial and Deltaic Sandstones Within the Upper Ferron Sandstone Last Chance Delta." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c18.

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Abstract The Turonian-Coniacian Upper Ferron Sandstone Last Chance Delta was deposited along the western margin of the Western Interior Seaway as a wave-modified, river-dominated deltaic system. The Last Chance Delta was deposited during a slow relative sea-level rise whose rate of rise decreased with time. The sedimentation rate progressively decreased throughout the deposition of the Last Chance Delta. Architectural and sedimentological data for deltaic near-marine sandstones indicate that primary deltaic depositional style is directly correlated with degree of wave-modification, which is co
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Garrison, James R., and T. C. V. van den Bergh. "High-Resolution Depositional Sequence Stratigraphy of the Upper Ferron Sandstone Last Chance Delta." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c6.

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Abstract The deposition of the late Turonian-early Coniacian Upper Ferron Sandstone Last Chance Delta occurred during a long slow relative rise in sea level, interrupted only by three minor 4th-order relative falls in sea level. An analysis of stratigraphic, geometric, and architectural data, for both near-marine and non-marine facies indicate that Last Chance Delta architecture was controlled by changes in sediment supply. The systems tract style and parasequence set stacking pattern within deposition-al sequences reflect the relationship of the rate of sedimentation to the rate of relative c
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Kenkmann, T., P. W. Haines, I. P. Sweet, and K. Mitchell. "The Cleanskin impact structure, Northern Territory and Queensland, Australia: A reconnaissance study." In Large Meteorite Impacts and Planetary Evolution VI. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2550(03).

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ABSTRACT We report on the Cleanskin structure (18°10′00″S, 137°56′30″E), situated at the border between the Northern Territory and Queensland, Australia, and present results of preliminary geological fieldwork, microscopic analyses, and remote sensing. The Cleanskin structure is an eroded complex impact structure of ~15 km apparent diameter with a polygonal outline caused by two preexisting regional fault sets. The structure has a central uplift of ~6 km diameter surrounded by a rather shallow ring syncline. Based on stratigraphy, the uplift in the center may not exceed ~1000 m. The documentat
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Anderson, Paul B., and Thomas A. Ryer. "Regional Stratigraphy of the Ferron Sandstone." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c8.

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Abstract The Ferron Sandstone Member of the Mancos Shale is divided informally into upper and lower units. The upper Ferron has been divided by earlier workers into seven or eight delta-front units. These units correspond to parasequence sets. We suggest one additional delta-front or parasequence set, bringing the total to nine for the upper Ferron. The opportunity to study many of these stratal units in detail on outcrop has led to the further division into numerous parasequences. These parasequences often contain distinct, mappable genetically related packages of beds which are clearly not b
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Elkateb Tamer. "The Point Load Test in the Persian Gulf Carbonate Rocks." In Proceedings of the 17th International Conference on Soil Mechanics and Geotechnical Engineering. IOS Press, 2009. https://doi.org/10.3233/978-1-60750-031-5-372.

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The Point Load test is an index test used to provide an economical and quick estimate of the Uniaxial Compressive Strength (UCS) especially for highly fractured rock cores that with geometry not suitable for UCS testing. This is usually done using an empirical conversion factor (K) between the Point Load Index of 50-mm diameter rock cores (Is50) and the UCS. A value of the K factor equal to 24 has been traditionally used in the rock mechanics literature based on the work of Broch and Franklin (1972). Several studies have disputed the applicability of this universal value, especially for weak r
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Cox, Morgan A., Aaron J. Cavosie, Michael Poelchau, Thomas Kenkmann, Phil A. Bland, and Katarina Miljković. "Shock deformation microstructures in xenotime from the Spider impact structure, Western Australia." In Large Meteorite Impacts and Planetary Evolution VI. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2550(19).

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ABSTRACT The rare earth element–bearing phosphate xenotime (YPO4) is isostructural with zircon, and therefore it has been predicted that xenotime forms similar shock deformation microstructures. However, systematic characterization of the range of micro structures that form in xenotime has not been conducted previously. Here, we report a study of 25 xenotime grains from 10 shatter cones in silicified sandstone from the Spider impact structure in Western Australia. We used electron backscatter diffrac tion (EBSD) in order to characterize deformation and microstructures within xenotime. The stud
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Conference papers on the topic "Sandstones of Seis"

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Zhang, Baosen, Xin Jin, Yitian Xiao, et al. "Quantitative Identification of Sandstone Lithology Based On Thin-Section Micrographs Using the U-net and U-net++ Semantic Segmentation Network." In International Petroleum Technology Conference. IPTC, 2023. http://dx.doi.org/10.2523/iptc-22865-ea.

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Abstract Quantitative identification of sandstone microscopic images is an essential task for sandstone reservoir characterization. The widely-used classical Gazzi-Dickinson point-counting method can be subjective, inconsistent and time-consuming. Furthermore, by directly putting labeled microscopic images of all rock types into image recognition models for training, most previous studies did not address the petrographic principle of artificial identification. In this study, U-Net and U-Net++ semantic segmentation networks that incorporated the sandstone petrographic principle in quantitative
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Piewmoh, Watcharapong, and Pitsanupong Kanjanapayont. "Fracture Characterisation and Basement Reservoir Potential of Phra Wihan Formation in Southern Part of Uttaradit Province, Northern Thailand." In International Petroleum Technology Conference. IPTC, 2023. http://dx.doi.org/10.2523/iptc-22845-ms.

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Abstract This research describes the characterization of fractures in the Mesozoic sandstones Phra Wihan Formation exposed at the southern part of Uttaradit province, Northern Thailand. Fracture characterization of outcrop analog is important to determine potential of subsurface reservoir. The methodology using field study and petrography analysis to determine the relationship of fractures and other structures such as bedding plane and fold geometry. In addition, microstructure analysis can be analoged to the potential of reservoir. The Phra Wihan Formation composed of thick quartz arenite san
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Osukuku, Godfred, Abiud Masinde, Bernard Adero, Edmond Wanjala, and John Ego. "Integrated Geophysical Interpretation of Kerio Valley Basin Stratigraphy, Kenya Rift." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2670415-ms.

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Abstract This research work attempts to map out the stratigraphic sequence of the Kerio Valley Basin using magnetic, gravity and seismic data sets. Regional gravity data consisting of isotactic, free-air and Bouguer anomaly grids were obtained from the International Gravity Bureau (BGI). Magnetic data sets were sourced from the Earth Magnetic Anomaly grid (EMAG2). The seismic reflection data was acquired in 1989 using a vibrating source shot into inline geophones. Gravity Isostacy data shows low gravity anomalies that depict a deeper basement. Magnetic tilt and seismic profiles show sediment t
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Wu, Tao, Hanzhi Fang, Hu Sun, et al. "A Data-Driven Approach to Evaluate Fracturing Practice in Tight Sandstone in Changqing Field." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21821-ms.

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Abstract Unconventional reservoirs such as shale and tight sandstones that with ultra-low permeability, are becoming increasingly significant in global energy structures (Pejman T, et al., 2017). For these reservoirs, successful hydraulic fracturing is the key to extract the hydrocarbon resources efficiently and economically. However, the intrinsic mechanisms of fracturing growth in the tight formations are still unclear. In practice, fracturing design mainly depends on hypothetical models and previous experience, which leads to difficulties in evaluating the performance of the fracturing jobs
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Xin, Chen, Zhao Min, Cui Jingbin, et al. "Seismic Motion Inversion Based on Geological Conditioning and Its Application in Thin Reservoir Prediction, Middle East." In ADIPEC. SPE, 2022. http://dx.doi.org/10.2118/211627-ms.

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Abstract With the development of exploration and development, thin reservoir prediction is becoming more and more important. However, due to the limit of seismic resolution, thin reservoir prediction has always been an important challenge in the Middle East. Thin reservoir prediction based on conventional geophysical techniques is not accurate enough to meet the requirements of development. In order to improve the accuracy of thin reservoir prediction, a new thin reservoir prediction technique is proposed. This technical workflow main includes 4 steps: (1) Sedimentary facies identification bas
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Zhang, Q. X., Y. Zhang, J. Y. Feng, and J. Luo. "Granite Rock Mass Identification and Geothermal Well Location Deployment Based on the Wide Field Electromagnetic Method: A Case Study of Sanshui Basin." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0165.

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ABSTRACT: Due to the special geological environment, two sets of geothermal reservoirs of Buxin Formation with lithology of sandstone and deep volcanic rocks have been formed in Sanshui Basin. Although a lot of research progress has been made in the geological conditions such as heat source, channel, reservoir and cover layer in this area, the depth and range of deep dry hot rock mass are not clear. Therefore, effective exploration methods are needed to provide technical support for geothermal well deployment and resource assessment. In this paper, based on the principle of wide field electrom
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Chen, Ming, Yongde Gao, Jinbo Wu, et al. "Shale Oil Quality Evaluation of Sand-Shale Laminated Reservoir Based on Wireline Formation Test." In International Petroleum Technology Conference. IPTC, 2024. http://dx.doi.org/10.2523/iptc-23404-ms.

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Abstract Shale oil and gas are among the most potential and strategic oil and gas replacement resources in China. The second member and third member of the Paleogene Liushagang Formation (Liu-2 Member and Liu-3 Member) in the Weixinan Sag of Beibuwan the Basin in the western South China Sea are the main source rocks, and there are multiple mature laminated shale/sand oil reservoirs. To characterize the quality of shale oil, nuclear magnetic resonance (NMR) and elemental and conventional logging methods are used in this area. These logging evaluation methods are all aimed at the evaluation of t
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XiaoJie, Z., H. Tan, and Z. Ma. "Pre-Stack Detailed Frequency Variation Study and Application in Complex Sandstone Reservoir Hydrocarbon Detection." In International Petroleum Technology Conference. IPTC, 2025. https://doi.org/10.2523/iptc-24900-ea.

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Bohai oilfield is an important offshore oil and gas producing area in China. The fluvial sandstone reservoir is an important production series, which accounts for about 45% in the total proved reserves. However, in recent years, the fluvial sandstone exploration encountering new challenges. The target fluvial sandstone series are buried shallow, about 1000-1600 meters underground, due to the large sedimentary accommodation space, huge river channels are developed. Now, almost all huge river channels have been drilled, the remaining complex river channels that drastic changes in both vertical a
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Afagwu, C. C., and R. Weijermars. "Production Analysis of Offshore Gas Wells (UK North Sea) Using Bootstrapped Arps Method: Reserves Estimation Without Reservoir Model." In International Petroleum Technology Conference. IPTC, 2024. http://dx.doi.org/10.2523/iptc-24380-ms.

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Abstract This study analyzes recently released proprietary daily production data from 31 decommissioned dry gas fields located on the UK Continental Shelf (UKCS). First, the hydrocarbon fields in the UKCS region were assigned to five groups, based on their geological source origin. The data analyzed here are from two lease areas comprising gas fields, sourcing from two of the five groups distinguished. One set of wells produced from Carboniferous Westphalian sandstones, the other from Permian Rotliegendes sandstones: both reservoir types remain active sub-salt targets. The production profiles
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Britton, Allen, and Katrina Cox. "An Image-Based Artificial Intelligence Approach for the Determination of Analog Petrophysical Rock Properties From Drill Cuttings." In 2024 SPWLA 65th Annual Symposium. Society of Petrophysicists and Well Log Analysts, 2024. https://doi.org/10.30632/spwla-2024-0086.

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A thin-section image-based artificial intelligence (AI) model, leveraging an associated database of 100 conventional core samples, has been developed, validated, and published for the determination of analog petrophysical properties when conventional core is unavailable. The AI model, with newly available data, continues to be updated, resulting in an ongoing learning process. In this study, we will focus on applying this technology to synthetic drill cuttings and present gained insight into additional factors that may also impact the AI-based analog drill cuttings results. A subset of 20 samp
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