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Academic literature on the topic 'Lowstand System Tracks'

Author: Grafiati

Published: 5 June 2025

Last updated: 2 August 2025

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Journal articles on the topic "Lowstand System Tracks"

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Peter, S. Ola, J. Ohiochioya Aghomon, and O. Alabere Abdulquadri. "Sequence Stratigraphy and Petrophysical Analysis of 'Aje' Field, Offshore Niger Delta." Journal of Scientific and Engineering Research 8, no. 4 (2021): 167–78. https://doi.org/10.5281/zenodo.10589294.

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<strong>Abstract</strong> A detailed sequence stratigraphic and petrophysical analysis was performed on six (6) wells in the "AJE" field, Niger Delta. The purpose is to re-evaluate the petrophysical properties, determine the depositional environment of reservoirs as well as the sequence stratigraphic attributes of hydrocarbon bearing section of six wells in AJE Field in the Niger delta. Four (4) sand reservoirs were identified across the field. Biofacies and shape of well logs signatures; funnel, cylindrical or blocky shapes were used to infer the depositional environment. Based on biostratigr

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Buatois, Luis A., Gabriela Mángano, Christopher G. Maples, and William P. Lanier. "Allostratigraphic and Sedimentologic Applications of Trace Fossils to the Study of Incised Estuarine Valleys: An Example from the Virgilian Tonganoxie Sandstone Member of Eastern Kansas." Bulletin (Kansas Geological Survey), no. 241 (July 30, 1998): 1–27. https://doi.org/10.17161/kgsbulletin.no.241.20401.

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The Tonganoxie Sandstone Member (Stranger Formation) records part of the infill of an estuarine valley system that was incised during a late Missourian (Late Carboniferous) drop in sea level and subsequently infilled during a transgressive episode later in the Virgilian (Late Carboniferous). At Buildex Quarry, in an eastern valley-margin position, this unit is represented by planar-bedded-and-laminated siltstone beds (tidal rhythmites) overlying a coplanar surface of lowstand erosion and subsequent transgression. These tidal rhythmites contain a relatively diverse ichnofauna dominated by arthr

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Ainsworth, R. Bruce, and Simon A. J. Pattison. "Where have all the lowstands gone? Evidence for attached lowstand systems tracts in the Western Interior of North America." Geology 22, no. 5 (1994): 415. http://dx.doi.org/10.1130/0091-7613(1994)022<0415:whatlg>2.3.co;2.

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Csato, Istvan, and Octavian Catuneanu. "Quantitative conditions for the development of systems tracts." Stratigraphy 11, no. 1 (2014): 39–59. http://dx.doi.org/10.29041/strat.11.1.02.

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Systems tracts are defined on the basis of stratal stacking patterns. This paper explores quantitatively the possible relationships between different systems tracts and the relative sea-level in siliciclastic depositional systems. The development of systems tracts depends on the manifestation of forced regressions, normal regressions (lowstand and highstand) and transgressions, irrespective of the magnitudes of relative sea-level rise preceding and succeeding a stage of relative fall. As such, the transgressive and highstand systems tracts of one sequence may form when the elevation of the rel

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Umukoro, A. G., and K. O. Okengwu. "Sequence stratigraphic framework of ‘AKOS’ field, Niger Delta." Scientia Africana 21, no. 1 (2022): 133–48. http://dx.doi.org/10.4314/sa.v21i1.12.

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The aim of this study is to investigate the sequence-stratigraphic framework of a hydrocarbon prospect of ‘AKOS’ Field, Niger Delta, using well logs, and 3-D seismic data. To achieve this, the researchers identify the various sand/shale and seismic facies, build a sequencestratigraphic framework of the oilfield, and assess the petroleum play of identified system tracts. A fault analysis reveal twelve (12) fault sets (Fault 1-12) mapped across the seismic volume. These faults are picked on an increment of 50 and examined for consistency using time slice and variance attributes. Faults-1 and 2 a

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Yu, Bao, and Ling Yu Xu. "Sequence Stratigraphic Characteristics of Damoguaihe Formation in the North of Wuerxun Sag." Applied Mechanics and Materials 733 (February 2015): 84–87. http://dx.doi.org/10.4028/www.scientific.net/amm.733.84.

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Using the theories and methods of high-resolution sequence stratigraphy in rift lacustrine basins, we analyzed seismic, logging and drilling core data of the Damoguaihe Formation in the northern Wuerxun Sag area of the Hailaer Basin in order to understand its sequence stratigraphy characters. We identified third-order sequence boundaries and maximum flooding surfaces and established the sequence stratigraphic framework of the Damoguaihe Formation, which is a set of type sequence. It includes lowstand system tracts (LST), transgressive system tracts (TST) and highstand system tracts (HST).

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Wang, Zhe, Zhen Kui Jin, and Gui Zai Li. "Sequence Stratigraphic Analysis of Badaowan Formation in Dishuiquan Area, Junggar Basin." Advanced Materials Research 616-618 (December 2012): 56–59. http://dx.doi.org/10.4028/www.scientific.net/amr.616-618.56.

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In the light of the principle and method of sequence stratigraphy, the sequence stratigraphic framework of Badaowan formation in the Dishuiquan area was established. The results show that the sequence of Badaowan formation is one and half, including 5 system tracts. The whole experiences the process of retrogradation, progradation and then retrogradation again. There develop three types of sedimentary facies such as braided river, braided river delta and lakes, five types of sedimentary subfacies and 10 types of sedimentary microfacies. Most of JSQ1 sequence lowstand system tract is braided ri

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Ross, M. I. "INFLUENCE OF PLATE TECTONIC RE-ORGANISATIONS AND TECTONIC SUBSIDENCE ON THE MESOZOIC STRATIGRAPHY OF NORTHWESTERN AND SOUTHEASTERN AUSTRALIA: IMPLICATIONS FOR SEQUENCE STRATIGRAPHIC ANALYSIS." APPEA Journal 35, no. 1 (1995): 253. http://dx.doi.org/10.1071/aj94016.

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Determining and predicting the interplay of plate tectonic events, subsidence, flexure and depositional systems is important in frontier exploration, play concept development, and maturation modelling. A circum-Australian plate tectonic model is here tied to an internally consistent global plate tectonic model to determine the timing and orientation of changes in the lithospheric stress regime induced by plate tectonic changes. One-and three-dimensional geohistory results for the Otway Basin and North West Shelf/Exmouth Plateau are presented, based on an integrated sequence stratigraphic frame

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GURI, S., L. GJANI, S. RANXHA, M. GURl, and A. XHAXHIU. "Sequence stratigraphy, quaternary basin analyses in the Adriatic Foredeep." Bulletin of the Geological Society of Greece 34, no. 2 (2018): 635. http://dx.doi.org/10.12681/bgsg.17117.

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This paper intends to give the characterization of Quaternary loose deposits, near and along the sea coast zone, by evaluating lithological-geologic parameters, depositional environments and the tectonic subsidence. The main objectives are: - The lithologic-facial zone by mapping of lithologie composition and facies distribution. - The Quaternary basin analyses by interpreting depositional sequences of third order, where system tracts (lowstand, shelf wedge, transgressive and highstand) are individualized. - The present fluvial processes and delta configuration (Shkumbin, Seman).

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Armentrout, John M. "Biostratigraphic signature of sequence boundaries, maximum flooding surfaces, condensed sections, and depositional systems tracts – with examples from the gulf of mexico plio-pleistocene." Paleontological Society Special Publications 6 (1992): 9. http://dx.doi.org/10.1017/s2475262200005694.

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The primary horizons utilized in sequence stratigraphic analysis are the sequence boundary, and the maximum flooding surface which occurs within the condensed section in areas of low sediment accumulation rates. These regionally correlative surfaces can be identified on seismic reflection profiles, on wireline logs, in stratigraphic sections, and from checklists of fossil abundance and diversity. Both surfaces are time-transgressive but nevertheless can be used as correlation horizons for partitioning depositional cycles into discrete phases of relative sea-level rise and fall. Sediments depos

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Book chapters on the topic "Lowstand System Tracks"

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Kendall, Christopher George St Clement. "Sedimentary Sequence/Parasequence/Systems Tracts (Highstand, Lowstand, Transgressive, Shelf Margin)." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6644-0_177-1.

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Mansurbeg, H., S. Morad, P. Plink-Björklund, M. A. K. El-Ghali, M. A. Caja, and R. Marfil. "Diagenetic Alterations Related to Falling Stage and Lowstand Systems Tracts of Shelf, Slope and Basin Floor Sandstones (Eocene Central Basin, Spitsbergen)." In Linking Diagenesis to Sequence Stratigraphy. John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118485347.ch15.

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Bohacs, Kevin, Remus Lazar, Tim Demko, Jeff Ottmann, and Ken Potma. "7 Sequence Sets and Composite Sequences." In Sequence Stratigraphy: Applications to Fine-Grained Rocks. The American Association of Petroleum Geologists and Brazilpetrostudies, 2022. http://dx.doi.org/10.1306/137123021283.

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ABSTRACT This chapter presents definitions, recognition criteria, and examples of sequence sets and composite sequences within a sequence-stratigraphic framework. This stratigraphic scale provides useful insights into shale-gas and tight-liquid plays with mudstone reservoirs that can be profitably grouped into four families based on stratal stacking at the sequence-set scale. Depositional sequences stack in progradational, aggradational, retrogradational, or degradational patterns to form sequence sets—exactly analogous to the stacking patterns of parasequences within depositional sequences di

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Potma, K., R. Jonk, and K. M. Bohacs. "10 Canol Formation, Northwest Territories, Canada—An Outcrop-to-Subsurface Analog for the Paleozoic Horn River Shale-gas Play." In Sequence Stratigraphy: Applications to Fine-Grained Rocks. The American Association of Petroleum Geologists and Brazilpetrostudies, 2022. http://dx.doi.org/10.1306/137123053861.

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ABSTRACT The Late Devonian Canol Formation and associated stratal units in the Northwest Territories of Canada illustrate the expression of sequence-stratigraphic surfaces and units in a distal Paleozoic carbonate shelf to relatively deep-basin setting. These Devonian strata are time equivalent and quite analogous in depositional conditions and petroleum-system characteristics to the proven shale-gas deposits in the Horn River Basin of northeastern British Columbia. The Canol Depositional Sequence spans the upper part of the Ramparts Formation, the Canol Formation, and the lowermost part of th

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Bohacs, K. M., O. R. Lazar, R. D. Wilson, and J. H. S. Macquaker. "12 Mowry Shale–Belle Fourche Shale, Bighorn Basin, Wyoming, USA—A Mesozoic Clastic-Biosiliceous Shelf System: A Prolific Source Rock with Associated Mudstone Reservoir Potential." In Sequence Stratigraphy: Applications to Fine-Grained Rocks. The American Association of Petroleum Geologists and Brazilpetrostudies, 2022. http://dx.doi.org/10.1306/137123071283.

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ABSTRACT The Cretaceous Mowry Shale and associated units in the Bighorn Basin of Wyoming, illustrate the expression of sequence-stratigraphic surfaces and units in a Mesozoic epeiric sea in a proximal to distal, detrital-to-biogenic–dominated shelf setting. Associated units include the Muddy Sandstone, Belle Fourche Shale, and Frontier Formation and are of Albian–Cenomanian age. The Mowry Shale is a highly siliceous mudstone, significantly enriched in marine organic matter that served as a prolific source rock across the Western Interior basin of the United States. It is also a source of bento

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Conference papers on the topic "Lowstand System Tracks"

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Wood, J., and A. E. Schwartzbard. "Upper Jurassic lowstand and highstand systems tracts on the dip slope of Snorre-Vigdis-Tordis megafootwall." In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410173.

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Winarni, R. A. "Facies and Stratigraphic Sequences Analysis Based on Well Log, Mud Log, and 2D Seismic Data of GHC Field, Baong Formation, Aru Sub-Basin, North Sumatera Basin." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-sg-170.

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The Baong Formation is one of the formations that have hydrocarbon potential in the Aru Sub Basin, North Sumatra Basin. However, there is still limited geological information in the area including the Analysis of Sequence Stratigraphy. The geological information is also needed to easier find out the distribution of potential layers of oil and gas in order to maximize exploration results. The method used in this research was Electrofacies Analysis to show the appearance of rock grain size and geological processes that affect formation. Well--Seismic Tie and interpretation of the horizon along w

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Yulitha, G. C. "Sequence Stratigraphy Analysis Based on Wireline Log, Mudlog, and 2D Seismic of GHC Field, Baong Formation, Aru Sub Basin, North Sumatra Basin." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-sg-229.

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The Baong Formation is one of the formations that has hydrocarbon potential in the Aru Sub Basin, North Sumatra Basin (Figure 1). However, geological information in that area is still far less than is available in others. Analysis of sequence stratigraphy needs to be done to enrich geological information of the study area, maximize the results of exploration before exploitation, and make it easier to find the distribution of potential layers of oil and gas. Methods that are used in this research are electrofacies analysis to show the appearance of rock grain size and geological processes that

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Reports on the topic "Lowstand System Tracks"

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Ambrose, William A., Tucker F. Hentz, Harold Rogers, and David L. Carr. Regional and Local Variability in Lowstand Valley Fill and Deltaic Deposits in the Tannehill Sandstone (Cisco Group), Eastern Shelf of the Permian Basin. University of Texas at Austin, Bureau of Economic Geology, 2024. https://doi.org/10.23867/ri0290d.

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Lowstand valley fill and shelf-edge deltaic deposits in the Tannehill sandstone (Wolfcampian Cisco Group) in the Eastern Shelf of the Permian Basin are major targets for oil and gas exploration. The most-productive trends link coarse-grained alluvial systems in Baylor County to shelf-edge and upper-slope deepwater systems in Dickens County. Depositional axes in the Tannehill sandstone in the updip (eastern) facies tract in Wichita, Archer, Clay, and Montague Counties, proximal to sediment source areas in the Ouachita fold belt and the Arbuckle Mountains, contain 40 to 80 ft (12–24 m) of net sa

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