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Journal articles on the topic 'Sequence stratigraphy'

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Published: 4 June 2021

Last updated: 25 July 2025

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1

Christie-Blick, Nicholas, Stephen F. Pekar, and Andrew S. Madof. "Is there a role for sequence stratigraphy in chronostratigraphy?" Stratigraphy 4, no. 2-3 (2007): 217–29. http://dx.doi.org/10.29041/strat.04.2.15.

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Sequence stratigraphy revolutionized the field of stratigraphy in the late 1970s and 1980s by providing an interpretive depositional framework for integrating diverse stratigraphic data at the scale of sedimentary basins. However, a lack of consensus on criteria for recognizing, mapping and hence dating sequence boundaries, interpretations of uneven quality, and doubts about the universal eustatic origin and global synchrony of unconformity-related sequences limit the usefulness of sequence stratigraphy in chronostratigraphy.

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Wu, Heyuan, Muneeb Khan, and Ping Song. "Sequence Stratigraphy towards its standardization—an important scientific scheme." E3S Web of Conferences 131 (2019): 01034. http://dx.doi.org/10.1051/e3sconf/201913101034.

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In the Post-Exxon Era of sequence stratigraphy, various sequence models for the complex stratigraphic records with their response mechanisms are developed. All the models with strong pertinence are endowed, which lead to misapprehension in the conceptual system. Therefore, the standardization of sequence stratigraphy with the aim to provide consistency in the terminology has become an important motive of modern sequence. During the development of sequence stratigraphy, the identification and distinction between normal and forced regression have laid important foundation for the system descript

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Li, Jin Hua. "Fluvial Facies Sequence Stratigraphy and its Application to Oil Exploration." Applied Mechanics and Materials 295-298 (February 2013): 2715–19. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.2715.

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It is considered that discussion on adaptability of sequence stratigraphy in fluvial sedimentation is significant for oil exploration. As the main controlling factor is the sea-level fluctuations in the coastal river system, Exxon sequence stratigraphy can be applied to divide the sequences into: lowstand, transgressive and highstand systems tracts. And in the inland fluvial system, the application of low- and high-accommodation systems tracts may keep more coincident with the actual stratigraphic record. From the Exxon stratigraphy to low- and high-accommodation systems tracts, each model wil

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Ross, W. C. "Cyclic stratigraphy, sequence stratigraphy, and stratigraphic modeling from 1964 to 1989: Twenty-five years of progress?" Bulletin (Kansas Geological Survey), no. 233 (April 16, 2024): 3–8. https://doi.org/10.17161/kgsbulletin.no.233.20445.

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The evolution of concept development in stratigraphy between 1964 and 1989 is reviewed by comparing and contrasting the contents of the golden book volume on cyclic stratigraphy (Merriam, 1964) with the present volume. Although separated by more than 25 years, both volumes treat strikingly similar subject material with an emphasis on cyclic stratigraphy, time stratigraphy, and the genetics of basin fill. The collection of papers found in the earlier volume reflects the culmination of work from the most prominent stratigraphers of the 1940's through the early 1960's, a period strongly affected

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Christie-Blick, Nicholas, and Neal W. Driscoll. "Sequence Stratigraphy." Annual Review of Earth and Planetary Sciences 23, no. 1 (1995): 451–78. http://dx.doi.org/10.1146/annurev.ea.23.050195.002315.

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6

Kauffman, Erle G., and Bradley B. Sageman. "Biological patterns in sequence stratigraphy; Cretaceous of the Western Interior Basin, North America." Paleontological Society Special Publications 6 (1992): 158. http://dx.doi.org/10.1017/s2475262200007188.

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High-resolution stratigraphic analysis of Cretaceous strata in the Western Interior Basin (WIB) of North America has allowed definition of numerous disconformity-bounded, eustatically and/or tectonically driven sequences and their systems tracts at 2nd- through 4th-order scale, as well as 5th- to 7th-order climate-induced cycles. Integrated event chronostratigraphy and biostratigraphy allow detailed regional tracing and facies analysis of these sequences, leading to three-dimensional modeling of facies evolution. Whether driven by relative sealevel changes or smaller scale climate cycles, Cret

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Wu, He Yuan, and Bin Hao. "Third-Order Sequence Division of Yunmengshan and Baicaoping Formation of Proterozoic in Yuxi District of China: an Example from Xiatang Profile in Lushan." Advanced Materials Research 998-999 (July 2014): 1492–97. http://dx.doi.org/10.4028/www.scientific.net/amr.998-999.1492.

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There are controversies on the Proterozoic stratigraphic genesis, division, correlation and palaeogeographical evolution of western Henan in China. Based on the basic description of sedimentary facies, Yunmengshan and Baicaoping formation of Proterozoic typical section in western Henan is divided into 4 third-order sequences. Sequence stratigraphy framework which reflects sedimentary and overlap is established with basis of two kinds of facies-change surface and two kinds of diachrononism in stratigraphical records. Although chronostratigraphic belonging of Precambrian strata is controversial

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Zhou, Guangzhao, Zhiming Hu, Xianggang Duan, and Jin Chang. "Identification of sequence stratigraphy in the Dongying Formation of the Liaoxi low uplift, Bohai Bay Basin, China." Canadian Journal of Earth Sciences 57, no. 5 (2020): 647–61. http://dx.doi.org/10.1139/cjes-2018-0276.

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A change in sea level (or lake level) causes a change in accommodation space and sediment compensation, which then controls the formation and evolution of sequences. A multidisciplinary approach based on the integration of clay minerals, major and trace elements, paleosalinity, and three-dimensional seismic data were applied to interpret the stratigraphic sequence of the Dongying Formation in the Liaoxi low uplift. The sequence surface indicates that multistage tectonic action, paleoclimate, paleosalinity, and lake level change jointly controlled the sequence stratigraphy. The illite and illit

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Catuneanu, Octavian, William E. Galloway, Christopher G. S. t. C. Kendall, et al. "Sequence Stratigraphy: Methodology and Nomenclature." Newsletters on Stratigraphy 44, no. 3 (2011): 173–245. http://dx.doi.org/10.1127/0078-0421/2011/0011.

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10

Xu, Haichun, Nan Wu, Xinyan Xu, Bo Yu, and Ke Xu. "Orbital-Scale Modulation of the Middle Miocene Third-Order Eustatic Sequences from the Northern South China Sea." Journal of Marine Science and Engineering 13, no. 5 (2025): 921. https://doi.org/10.3390/jmse13050921.

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The Miocene Hanjiang Formation (HJF) is a remarkable exploration target in the Pearl River Mouth Basin (PRMB). However, challenges such as bias in current sequence stratigraphic schemes, limitations in high-resolution stratigraphic schemes, and incomplete understanding of genetic mechanisms may present obstacles for refining hydrocarbon exploration strategies. This study integrates gamma ray (GR) logging data, lithological variations, sequence stratigraphy, and cyclostratigraphy to delineate connections between sequence stratigraphy and astronomical forcing. The analysis utilizes gamma-ray log

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McAnany, Patricia A., and Ian Hodder. "Thinking about stratigraphic sequence in social terms." Archaeological Dialogues 16, no. 1 (2009): 1–22. http://dx.doi.org/10.1017/s1380203809002748.

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AbstractFor archaeologists, stratification is an important character of archaeological deposits. Through it, layering is discerned and cultural and evolutionary interpretations are proposed. Archaeologists possess much implicit knowledge about the social practices that produce stratigraphic sequence and the specific, contextualized manner in which layers were built upon or cut into previous deposits. The aim of this paper is to gather together and formalize this knowledge so as to codify conceptual ‘tools to think by’ when recording and interpreting stratigraphy. Relevant literature is widely

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Ripepe, Maurizio, and Alfred G. Fischer. "Stratigraphic rhythms synthesized from orbital variations." Bulletin (Kansas Geological Survey), no. 233 (April 16, 2024): 335–44. https://doi.org/10.17161/kgsbulletin.no.233.20466.

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Previous work on a pelagic stratigraphic sequence in the Middle Cretaceous (Albian) of Italy, about 100 Ma, defined a hierarchy of oscillations. These were identified as variations in carbonate productivity and bottom fauna linked to seafloor aeration. The sequence geometry suggests response to orbitally driven climatic variations, reflecting Berger's precession index, which depicts the precession cycle as a carrier wave modulated by orbital eccentricity. Here we use Berger's astronomic precession index curve for the past 1,500 k.y. in combination with the stratigraphic data to construct a for

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Zhang, Lei, Lun Wei Zhu, and Xue Juan Zhang. "High Resolution Sequence Stratigraphy of Silurian Strata in Tazhong Area." Advanced Materials Research 734-737 (August 2013): 111–16. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.111.

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According to the fundamental principles of high resolution sequence stratigraphy, this paper focused on the application of high resolution sequence stratigraphy to Silurian strata in Tazhong area. Based on the comprehensive study of logging, drilling and seismic information, the high resolution sequence boundaries of Silurian strata and two scales of datum level cycles (long-term and intermediate-term) can be recognized in Tazhong area. Seven chronstratigraphic boundaries can be recognized in Silurian strata, including four sequence boundaries, which were the transformation from datum level fa

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McGowran, Brian, and Qianyu Li. "Stratigraphy: gateway to geohistory and biohistory." Stratigraphy 4, no. 2-3 (2007): 173–85. http://dx.doi.org/10.29041/strat.04.2.11.

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Concerned with the ordination, correlation and age determination of the rock record and the events entombed therein, stratigraphy is the central discipline in geohistory and biohistory. We consider (from our Cenozoic perch) changes in stratigraphy since the gestation of the International Stratigraphic Guide—changes in response to the “revolutions" of plate tectonics, bolide theory, sequence stratigraphy and cyclostratigraphy, and a cultural shift away from Lyellian gradualism. We discuss certain strictly stratigraphic matters in terms of the “Hedberg triad" of lithostratigraphy, biostratigraph

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Yuan, Hong Qi, Ying Hua Yu, and Dong Li Sun. "Sequence Boundaries Identification of Putaohua Oil Layer in Qijia-Gulong Area." Advanced Materials Research 734-737 (August 2013): 166–69. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.166.

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Sequence is a relatively conformable succession of genetically related strata bounded by unconformities or their correlative conformities. The correct identification of sequence boundaries is the key to the success of the sequence stratigraphic approach. Stratigraphic boundaries provide the fundamental framework for the genetic interpretation of any sedimentary succession, irrespective of how one may choose to name the packages of strata between them. Sequence stratigraphy of main research content is mainly chronohorizon (unconformity or conformity) identification, and to determine its causes

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Lebedev, M. V. "FACIAL UNCONFORMITIES AND FACIAL SERIES IN THE SEQUENCE STRATIGRAPHY." Oil and Gas Studies, no. 6 (January 20, 2019): 24–32. http://dx.doi.org/10.31660/0445-0108-2018-6-24-32.

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The sequence stratigraphy is currently, on the one hand, a leading approach in the study of the internal structure of sedimentary basins, on the other hand, a creatively developing discipline, the conceptual basis of which is being developed. The concept of a «system tract» is one of the most questionable concepts of sequence stratigraphy. According to the classical definition, system tract is a lateral sequence of facies, in accordance with modern definitions system tract is a geological body bounded by sequence-stratigraphic surfaces. It remains unclear: whether the idea of the lateral order

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Pemberton, S. George, Janok P. Bhattacharya, James A. MacEachern, and Erin A. L. Pemberton. "Harry Eugene Wheeler (1907-1987): A Pioneer of Sequence Stratigraphy." Stratigraphy 13, no. 2 (2016): 95–110. http://dx.doi.org/10.29041/strat.13.2.02.

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Harry Eugene Wheeler (1907-1987) of the University of Washington was a pioneer of genetic stratigraphic principles that form the basis of our modern concept of sequence stratigraphy. Wheeler's papers on what he liked to refer to as "stratology" included the classification of stratigraphic units into lithostratigraphic and biostratigraphic entities, as well as cyclothems, unconformity-bounded units, and the analysis of base-level and its role in forming stratigraphic discontinuities. His work on unconformity-bounded "sequences" ultimately led the International Subcommission on Stratigraphic Cla

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Li, Jing Zhe, Jing Liang Zhang, Yong Yuan, et al. "Sequence Stratigraphy of Jurassic Succession in Central Junggar Basin, China." Advanced Materials Research 734-737 (August 2013): 440–43. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.440.

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Sequence stratigraphic features of the Jurassic succession in Central Junggar Basin were investigated by integrating multiple materials including cores, well and seismic data. Due to their unique formation mechanism, sequences of the target interval were analyzed with a binary systems tract mode (each complete sequence contains a transgressive systems tract and a highstand systems tract) rather than the traditional one. Basic principles and analytical methods of high-resolution sequence stratigraphy were also applied to this research. By adopting cyclic correlation and hierarchical control tec

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Simmons, M. D., and C. L. Williams. "Sequence stratigraphy and eustatic sea-level change: the role of micropalaeontology." Journal of Micropalaeontology 11, no. 2 (1992): 112. http://dx.doi.org/10.1144/jm.11.2.112.

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Abstract. Following the May 1992 meeting in Dijon, which initiated an international project on the “Sequence Stratigraphy of European Basins”, it seems an appropriate time to consider the contribution micropalaeontology can make to the science of sequence stratigraphy. In this short note, we assume that readers are familiar with sequence stratigraphic terminology; if not, see Van Wagoner et al. (1988).WHAT ARE THE CHALLENGES FACING SEQUENCE STRATIGRAPHY?Demonstrating global eustatic sea-level change. We accept that the basic sequence stratigraphy model put forward by Peter Vail and his colleag

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Nainggolan, T. B., U. Nurhasanah, and I. Setiadi. "Depositional sequence interpretation using seismic and well data of offshore Central Sumatra Basin." IOP Conference Series: Earth and Environmental Science 944, no. 1 (2021): 012002. http://dx.doi.org/10.1088/1755-1315/944/1/012002.

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Abstract Offshore Central Sumatra Basin is an integral part of Central Sumatra Basin known for producing hydrocarbon basins. The derivation of stratigraphic study of seismic and well data is intended to improve accuracy of geological interpretation. Sequence stratigraphy studies have a significant role in exploratory studies to determine which depositional sequence can be inferred as hydrocarbon reservoir and its correlation in petroleum system. This study aims to identify biogenic gas sequential interpretation using seismic and well data of offshore Central Sumatra Basin. The procedure to ana

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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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Reilly, Mark, Suzanne Hurter, Zsolt Hamerli, Claudio L. de Andrade Vieira Filho, Andrew LaCroix, and Sebastian Gonzalez. "An integrated approach to the Surat Basin stratigraphy." APPEA Journal 59, no. 2 (2019): 940. http://dx.doi.org/10.1071/aj18073.

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The stratigraphy of the Surat Basin, Queensland, has historically been sub-divided by formation and unit nomenclature with a few attempts by other authors to apply sequence stratigraphy to existing formation boundaries. At a local- to field-scale, lithostratigraphy may be able to represent stratigraphy well, but at regional-scale, lithostratigraphic units are likely to be diachronous. To date, this lithology-driven framework does not accurately reflect time relationships in the sub-surface. An entirely new integrated methodological approach, involving well tied seismic data and sequence strati

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Pedersen, Stig A. Schack. "Glaciodynamic sequence stratigraphy." Geological Society, London, Special Publications 368, no. 1 (2012): 29–51. http://dx.doi.org/10.1144/sp368.2.

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Ainsworth, R. Bruce, Jamie B. McArthur, Simon C. Lang, and Adam J. Vonk. "Quantitative sequence stratigraphy." AAPG Bulletin 102, no. 10 (2018): 1913–39. http://dx.doi.org/10.1306/02201817271.

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Catuneanu, O., M. A. Martins-Neto, and P. G. Eriksson. "Precambrian sequence stratigraphy." Sedimentary Geology 176, no. 1-2 (2005): 67–95. http://dx.doi.org/10.1016/j.sedgeo.2004.12.009.

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Martins-Neto, M. A., and O. Catuneanu. "Rift sequence stratigraphy." Marine and Petroleum Geology 27, no. 1 (2010): 247–53. http://dx.doi.org/10.1016/j.marpetgeo.2009.08.001.

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de Graciansky, Pierre Charles. "Siliciclastic sequence stratigraphy." Marine and Petroleum Geology 12, no. 6 (1995): 691–92. http://dx.doi.org/10.1016/0264-8172(95)90033-0.

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Veillette, Jean J., and F. M. Nixon. "Sequence of Quaternary Sediments in the Bélanger Sand Pit, Pointe-Fortune, Québec-Ontario." Géographie physique et Quaternaire 38, no. 1 (2007): 59–68. http://dx.doi.org/10.7202/032536ar.

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ABSTRACT Drilling in the floor of the Bélanger sand pit (Ontario) near Pointe-Fortune, Québec, added 3 stratigraphic units to those already exposed in the pit: a lowermost till, and an intermediate organic-bearing (?) sand-clay unit overlain by a massive lacustrine clay. The subsurface units, comprising about 70% of the stratigraphy, complete the Quaternary sequence exposed in the pit face : an organic-bearing silty sand (>40 000 years BP) unit truncated by an unfos-siliferous sand unit and overlain by the uppermost till. The overall sequence forms a continuous 18 m column of Quaternary sed

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Masuda, Fujio, and Shuichi Tokuhashi. "Sequence stratigraphy; seeking its possibility. Sequence stratigraphy: Its effect on "stratigraphy" and its future." Journal of the Japanese Association for Petroleum Technology 59, no. 1 (1994): 4–17. http://dx.doi.org/10.3720/japt.59.4.

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Brake, A. T. "AVOIDING STRATIGRAPHIC CONFUSION IN EXPLORATION: THE NEED FOR STANDARDS IN SEQUENCE STRATIGRAPHY." APPEA Journal 39, no. 1 (1999): 485. http://dx.doi.org/10.1071/aj98029.

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As interpretations of sequence stratigraphy are published in increasing numbers in the petroleum exploration literature, the potential for confusion also increases because there are no rules for the classification or naming of the identified sequences. At present it is difficult to apply databases and geographic information systems to sequence stratigraphy, particularly when organisations with different outlooks and approaches attempt to collaborate and merge their databases.Despite sequence stratigraphic concepts having been in the literature for over two decades, no scheme for standardisatio

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Didei, I. S., and N. E. Ajaegwu. "Palynological and Sequence Stratigraphy Framework of Campanian-Maastrichtian Deposit of Anambra Basin, Awgu Section, Southeast Nigeria." Journal of Applied Sciences and Environmental Management 28, no. 6 (2024): 1697–708. http://dx.doi.org/10.4314/jasem.v28i6.7.

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A combination of palynological and palynofacies data are used as lithological evidence to describe sequence stratigraphic framework. Hence, the objective of this paper as to deploy the palynological and sequence stratigraphy framework of Campanian-Maastrichtian deposit of Anambra Basin, Awgu Section, Southeast Nigeria using standard techniques. The sequence stratigraphic analysis of the various succession in the studied outcrop sections identified parasequences limited by flooding surfaces with no evidence of erosion. The Nkporo and Mamu Formations were dated using the associated palynomorphs.

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Pemberton, S. George, Janok P. Bhattacharya, James A. MacEachern, and Erin A. L. Pemberton. "Unsung Pioneers of Sequence Stratigraphy: Eliot Blackwelder, Joseph Barrell, Amadeus Grabau, John Rich and Harry Wheeler." Stratigraphy 13, no. 4 (2017): 223–43. http://dx.doi.org/10.29041/strat.13.4.01.

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Few facies analysts or stratigraphers would argue against the contention that the transition to facies-driven sequence strati- graphic correlations represents one of the most important paradigm shifts in modern stratigraphy. What is less commonly appreciated is that most of the fundamental underpinnings of sequence stratigraphy were derived from a relatively small number of pioneers in the early to mid-1900s; most of them largely unknown or underappreciated by the current generation of sequence stratigraphers. Chief among these are Eliot Blackwelder, Amadeus Grabau, Joseph Barrell, John Rich,

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Li, Ang, Lai Xing Cai, Shuang Liu, and Qi Li. "Characteristics of Sedimentation Evolution Based on the Sequence Stratigraphic Frameworks in Shahezi Formation of Southern Xujiweizi Fault Depression." Advanced Materials Research 1010-1012 (August 2014): 1359–64. http://dx.doi.org/10.4028/www.scientific.net/amr.1010-1012.1359.

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Many scholars in China introduced the theory of sequence stratigraphy,applying to Chinese continental fault depression lake, they have made a lot of achievements in scientific research. However, there are still a lot of controversy according to the establishment in Shahezi group of sequence stratigraphic framework in Xujiaweizi fault depression.Sequence boundary identification method in this paper is based on the “instruction of Vail’s sequence stratigraphy theory, identification of seismic unconformity, verification by using logging methords”. And, following the principle of isochronous ,sequ

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Situmorang, Dr B. "Seismic Stratigraphy Of The Makassar Basin." Scientific Contributions Oil and Gas 10, no. 1 (2022): 3–38. http://dx.doi.org/10.29017/scog.10.1.895.

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Seismic reflection profiles from the Makassar basin have been analysed in terms of seismic stratigraphy. Systematic patterns of reflection terminations indicate the existence of at least three surfaces of discontinuity across the profiles-designated in order of superposition as C1, C2 and C3 - which define the boundaries of four seismic sequences, ie. :- seismic sequence I : topped by C1- seismic sequence II : the interval between C1 and C2- seismic sequence III : the interval between C2 and C3- seismic sequence IV : the interval between Cz and the sea floor Seismic sequence II is dominated by

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Herdiansyah, Firman, M. Burhannudinnur, Suryo Prakoso, et al. "Sequence Stratigraphy of Miocene Mixed Carbonate-Siliciclastic in Fold and Thrust Belt System, Banggai Basin." IOP Conference Series: Earth and Environmental Science 1104, no. 1 (2022): 012045. http://dx.doi.org/10.1088/1755-1315/1104/1/012045.

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Abstract This study was specifically analyzed in the southern part of the Banggai Basin, precisely in the TKA Field. In the Tertiary, regional stratigraphy reveals, the Banggai Sula microplate comprises carbonate shelf and siliciclastic sequence. Several previous studies had been concluding, the tertiary limestone was deposited during the Early Eocene to Middle Miocene. Carbonate formations which has been known by Tomori and Minahaki Formation. Meanwhile, their siliciclastic dominated is Matindok Formation and Celebes Mollase. These sequences formed a distinct stratigraphic style in the geophy

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Riaz, Muhammad, Shahid Ghazi, and Muhammad Waqas. "Sedimentology and Sequence Stratigraphy of the Late Permian Wargal Limestone: Implication for Reservoir Potential in the Salt Range, Pakistan." Journal Of The Geological Society Of India 100, no. 6 (2024): 887–900. http://dx.doi.org/10.17491/jgsi/2024/173919.

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ABSTRACT The present work comprehensively highlights the Late Permian Wargal limestone exposed in the western Salt Range, Pakistan. The purpose of this study is to determine its hydrocarbon with the help of sedimentology and sequence stratigraphy. The outcrop data classified the studied formation into nine lithological units in the Nammal Gorge, Gundi, and Lakrakki Nala sections. Our sequence stratigraphic interpretation reveals that the Wargal Limestone consists of four depositional sequences. These sequences consist of regressive system tract and tansgressive system tract that developed duri

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Gearon, James H., Cornel Olariu, and Ronald J. Steel. "The supply-generated sequence: A unified sequence-stratigraphic model for closed lacustrine sedimentary basins with evidence from the Green River Formation, Uinta Basin, Utah, U.S.A." Journal of Sedimentary Research 92, no. 9 (2022): 813–35. http://dx.doi.org/10.2110/jsr.2021.096.

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Abstract Closed lakes and oceans are stratigraphically distinct systems. However, closed-lake stratigraphy is often interpreted using conventional sequence stratigraphic concepts which were generated for marine settings. As a consequence, lacustrine stratigraphy has long been vexing and applied on an ad-hoc basis. To remedy this, we present a novel, unified sequence stratigraphic model for hydrologically closed (endorheic) basins: the Supply-Generated Sequence (SGS) Model. This model was generated to interpret our outcrop-based correlation—the largest to date at ∼ 30 km—across the Sunnyside In

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Hu, Guang Ming, Shun She Luo, Marjorie A. Chan, and Hong Ping Xiao. "Significance of Terrace Deposits in Fluvial Sequence Stratigraphy." Applied Mechanics and Materials 318 (May 2013): 423–27. http://dx.doi.org/10.4028/www.scientific.net/amm.318.423.

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The terrace deposits in a river valley are key records to the research of fluvial sequence stratigraphy. Terrace deposits and the basal sequence boundary comprise the half-cycle of base level fall, and the fluvial infillings belong to the half-cycle of base level rise. Thus, terrace deposits and the basal sequence boundary are part of the regressive systems tract, and should be separated from the transgressive or lowstand systems tracts in previously published littoral fluvial sequence stratigraphic models. In addition, in the upstream portions of the fluvial system where sea level cannot reac

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Al-Husseini, Moujahed, and Robley K. Matthews. "Arabian Orbital Stratigraphy: Periodic Second-Order Sequence Boundaries?" GeoArabia 10, no. 2 (2005): 165–84. http://dx.doi.org/10.2113/geoarabia1002165.

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ABSTRACT A simplified model of orbital-forcing suggests that the Phanerozoic Eon may be represented by 38 periodic second-order depositional sequences (DS2) each lasting about 14.58 million years (my). The DS2s are separated by second-order sequence boundaries (SB2, maximum regression surface) that should be manifested as regional stratigraphic discontinuities (unconformity, disconformity, time hiatus). To test this simple model, the Arabian succession was reviewed to identify candidate regional stratigraphic discontinuities that might be periodic at 14.58 my. Of the 38 predicted SB2s, 34 regi

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Borgomano, Jean, Cyprien Lanteaume, Philippe Léonide, François Fournier, Lucien F. Montaggioni, and Jean-Pierre Masse. "Quantitative carbonate sequence stratigraphy: Insights from stratigraphic forward models." AAPG Bulletin 104, no. 5 (2020): 1115–42. http://dx.doi.org/10.1306/11111917396.

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Kreager, B. Z., N. D. LaDue, T. F. Shipley, R. D. Powell, and B. A. Hampton. "Spatial skill predicts success on sequence stratigraphic interpretation." Geosphere 18, no. 2 (2022): 750–61. http://dx.doi.org/10.1130/ges02428.1.

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Abstract Sequence stratigraphic interpretation and three-dimensional spatial and spatiotemporal skills are considered important for the petroleum industry. However, little is known about the relationship between the two. This study begins to fill this gap by testing whether spatial skills predict success on a sequence stratigraphic interpretation task. Students in this study (N = 78) were enrolled in undergraduate or graduate stratigraphy-focused courses at three U.S. state universities. Students completed (1) a sequence stratigraphic interpretation task with a sequence stratigraphic diagram a

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Parvin, Afroza, and ASM Woobaidullah. "Incorporation of Sequence Stratigraphy in Gas Reservoir Correlation: A Case Study." Journal of the Asiatic Society of Bangladesh, Science 45, no. 2 (2019): 209–16. http://dx.doi.org/10.3329/jasbs.v45i2.46594.

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The application of sequence stratigraphy to resolve the miscorrelation between different genetic units in reservoir characterization in a gas field of Surma Basin is dealt with. Interpretation of available seismic and wireline logs (gamma ray, resistivity, density and neutron porosity) give the sequence stratigraphic correlation of reservoir sands. The reservoirs geometry, its extent, seal architecture and trapping styles have been revealed better with this correlation. There is juxtaposition of two reservoir sands, namely A1 and A2. A1 is located at older highstand sand, whereas A2 is in the

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Qayyum, Farrukh, Octavian Catuneanu, and Crépin Eric Bouanga. "Sequence stratigraphy of a mixed siliciclastic-carbonate setting, Scotian Shelf, Canada." Interpretation 3, no. 2 (2015): SN21—SN37. http://dx.doi.org/10.1190/int-2014-0129.1.

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During the Jurassic Period, a large-scale carbonate bank (Abenaki Formation) and a siliciclastic (Sable) delta coexisted in North America. Conventionally, carbonate systems (in situ) are separated from siliciclastic systems (transported) because of their contrasting origin. However, we developed a case study to show that the basic principles of sequence stratigraphy remain applicable. We integrated the results obtained from a regional 2D study and a detailed follow-up study using 3D seismic data of the Scotian Shelf, Canada. The results were integrated with the prepared Wheeler diagrams, and a

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Courville, P., and P. Y. Collin. "Taphonomic sequences—A new tool for sequence stratigraphy." Geology 30, no. 6 (2002): 511. http://dx.doi.org/10.1130/0091-7613(2002)030<0511:tsantf>2.0.co;2.

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Brett, Carlton E., Patrick I. McLauglin, and Gordon C. Baird. "Eo-Ulrichian to Neo-Ulrichian views: The renaissance of "layer-cake stratigraphy"." Stratigraphy 4, no. 2-3 (2007): 201–15. http://dx.doi.org/10.29041/strat.04.2.14.

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Classical notions of “layer-cake stratigraphy" have been denigrated as representing an antiquated “Neptunian" view of the geologic record with the American paleontologist-stratigrapher E.O. Ulrich vilified as its quintessential advocate. Some of the extreme “layer-cake" interpretations of E.O. Ulrich are demonstrably incorrect, especially where applied in marginal marine and terrestrial settings. However, close scrutiny of Ulrich’s work suggests that the bulk was correct and demonstrated considerable insight for the time. Subsequent development of facies concepts revolutionized geologists’ vie

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Krayenbuehl, Thomas, Nadeem Balushi, and Stephane Gesbert. "Novel geometric classification of 3D seismic and its application to the Habshan clinoforms of Western Oman." Leading Edge 40, no. 3 (2021): 186–92. http://dx.doi.org/10.1190/tle40030186.1.

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The principles and benefits of seismic sequence stratigraphy have withstood the test of time, but the application of seismic sequence stratigraphy is still carried out mostly manually. Several tool kits have been developed to semiautomatically extract dense stacks of horizons from seismic data, but they stop short of exploiting the full potential of seismo-stratigraphic models. We introduce novel geometric seismic attributes that associate relative geologic age models with seismic geomorphological models. We propose that a relative sea level curve can be derived from the models. The approach i

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Catuneanu, Octavian. "Scale in sequence stratigraphy." Marine and Petroleum Geology 106 (August 2019): 128–59. http://dx.doi.org/10.1016/j.marpetgeo.2019.04.026.

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Catuneanu, Octavian. "Model-independent sequence stratigraphy." Earth-Science Reviews 188 (January 2019): 312–88. http://dx.doi.org/10.1016/j.earscirev.2018.09.017.

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Scott, R. W. "Are seismic/depositional sequences chronostratigraphic units?" Paleontological Society Special Publications 6 (1992): 264. http://dx.doi.org/10.1017/s2475262200008248.

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Sequence Stratigraphic Analysis is claimed to be a “new globally valid system of stratigraphy … a precise methodology to subdivide, correlate and map sedimentary rocks” (Vail et al., 1991, p. 622). Sequence stratigraphic units, such as depositional sequences, depositional systems tracts, and parasequences, are time-equivalent rocks of specific durations controlled by cyclical changes in sediment supply related to eustasy. These units are bounded by regionally extensive unconformities with erosion beneath and onlapping strata above, or by physical surfaces separating either different patterns o

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Seidov, Vaqif M., and Lala N. Khalilova. "Sequence stratıgraphıc analysıs of the Galmaz field based on well loggıng data." Journal of Geology, Geography and Geoecology 32, no. 2 (2023): 360–70. http://dx.doi.org/10.15421/112333.

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   It is known that over 90% of oil, gas and gas condensate in Azerbaijan is produced from Productive Series (PS) of the Early Pliocene. In this respect, the detailed study of Pro- ductive Series deposits and their evolution conditions has a special value. Currently in most sedimentary basins of the world the latest highly informative methods of stratigraphic analysis are applied and one of these methods is sequence-stratigraphy, which is used in this study. The application of the concept of sequence stratigraphy enables an in-depth analysis of the study area to be conducted

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