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Journal articles on the topic 'Sequence stratigrapy'

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Published: 18 May 2024

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1

Firmansyah, Yusi, Dhehave Riaviandhi, and Reza Muhammad Ganjar Gani. "Sikuen Stratigrafi Formasi Talang Akar Lapangan “Dr”, Sub–Cekungan Jambi,Cekungan Sumatera Selatan." Bulletin of Scientific Contribution 14, no. 3 (2017): 263. http://dx.doi.org/10.24198/bsc.vol14.yr2016.art10970.

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The area of this study include to PT. Energi Mega Persada Tbk work area. The area of this study is located in Jambi Sub - Basin, South Sumatera Basin. This study is emphasized to examine the sequence stratigraphy of Talang Akar Formation. The data that is used in this study include core, mudlog, 3D seismic, well log, and palynomorf fossil. The result of those data analysis and data correlation are lithofacies, electrofacies, depositional environment, and stratigrahys sequences of Talang Akar Formation. From data analysis, the facies’ that develop in Talang Akar Formation are A, B, C, D, E, F,

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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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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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4

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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5

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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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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Yu, Ying Hua, Hong Qi Yuan, and Zi Xue Guo. "Sedimentary Characteristics in Zhalainuoer Group in Cano Depression Hailaer Basin." Advanced Materials Research 652-654 (January 2013): 2515–19. http://dx.doi.org/10.4028/www.scientific.net/amr.652-654.2515.

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Based on the theory of sequence stratigraphy, sequence stratigraphy framework of is established in this paper by comprehensively search of core, logging and 3-D seismic data. Zhalainuoer group in Cano Depression is divided into 5 3rd-order sequences: Sq1、Sq2、Sq3、Sq4、Sq5 from down to up. Based on the division and comparison of sequence formation, the sedimentary facies and the depositional system are proposed to study in the paper, and the main depositional systems are detailed explained. The distribution of these depositional systems is controlled by the sequence framework.

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Kwetche, Paul Gustave Fowe, Marie Joseph Ntamak-Nida, Adrien Lamire Djomeni Nitcheu, et al. "Facies Analysis and Sequence Stratigraphy of Missole Outcrops: N’Kapa Formation of the South-Eastern Edge of Douala Sub-Basin (Cameroon)." Earth Science Research 7, no. 1 (2017): 35. http://dx.doi.org/10.5539/esr.v7n1p35.

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Missole facies description and sequence stratigraphy analysis allow a new proposal of depositional environments of the Douala sub-basin eastern part. The sediments of Missole outcrops (N’kapa Formation) correspond to fluvial/tidal channel to shallow shelf deposits with in some place embayment deposits within a warm and semi-arid climate. Integrated sedimentologic, palynologic and mineralogical data document a comprehensive sequence stratigraphy of this part of the Douala sub-basin. Five facies associations occur: (1) facies association I is characterized by Floodplain deposits; (2) facies asso

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9

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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10

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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11

Ahler, Steven R. "Stratigraphy and Radiocarbon Chronology of Modoc Rock Shelter, Illinois." American Antiquity 58, no. 3 (1993): 462–89. http://dx.doi.org/10.2307/282107.

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Excavations at Modoc Rock Shelter, Illinois (11R5), between 1952 and 1956 documented the antiquity and cultural sequence of the Archaic period in the midcontinental United States. Some researchers questioned the site's stratigraphic integrity because of apparent inconsistencies between the radiocarbon assays and associated artifacts. Excavations in 1980, 1984, and 1987 documented stratigraphic sequences and produced assays of over 40 additional radiocarbon samples from controlled stratigraphic contexts. This report describes the stratigraphic sequences at Modoc Rock Shelter and presents critic

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12

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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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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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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16

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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17

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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18

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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19

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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20

Haddad, Sabah Noori Saleem, and Momtaz Ahmed Amin. "Mid-Turonian–early Campanian sequence stratigraphy of northeast Iraq." GeoArabia 12, no. 2 (2007): 135–76. http://dx.doi.org/10.2113/geoarabia1202135.

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ABSTRACT A sequence stratigraphic and tectonic model for the mid-Turonian-early Campanian carbonate sequence in North Iraq was constructed based on subsurface lithologic, thin-section and well-log analyses of ten boreholes. The studied sequence is represented by the Gulneri, Kometan and Mushorah formations in the eastern sector (seven wells) and their correlative Khasib, Tanuma, Sa’adi and lower part of the Hartha formations in the western sector of the study area (three wells). Three second-order sequences (from oldest to youngest A, B and C) were identified. Sequence A consists of two third-

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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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22

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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23

Amiewalan, F. O., and E. O. Bamigboye. "Sequence Stratigraphy of Well DX, Gongola Sub-Basin, Upper Benue Trough, Nigeria." Journal of Applied Sciences and Environmental Management 23, no. 10 (2019): 1855–60. http://dx.doi.org/10.4314/jasem.v23i10.14.

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: Biostratigraphic study of Well DX has yielded Cretaceous miospores and dinoflagellates cysts which heightened the recognition of sequence boundaries (SB), Maximum Flooding Surfaces (MFS) and associated Systems Tracts. Five maximum flooding surfaces between 95.6 Ma and 89.0 Ma, four sequence boundaries between 96.4 Ma and 93.0 Ma and threedepositional sequences were identified with varying average thicknesses of sediments interpreted from the gamma ray log and biostratigraphic data. The threedepositional sequences interpreted are -depositional sequence I (96.4 Ma - 95.4 Ma) (8240 ft. - 8120 f

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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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25

Daneshian, Jahanbakhsh, Zahra Saleh, Rudy Swennen, and Hossein Mosaddegh. "Porosity development in central Alborz Upper Jurassic deposits (N-Iran): sequence stratigraphy, diagenesis and mechanical stratigraphy." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 300, no. 2 (2021): 117–43. http://dx.doi.org/10.1127/njgpa/2021/0975.

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Ouda, Khaled, Mohammed Massoud, and Mohammed Tammam. "Stratigraphy of the Miocene sequence of the northern Red Sea." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 215, no. 1 (2000): 125–76. http://dx.doi.org/10.1127/njgpa/215/2000/125.

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27

Hadlari, Thomas, and Robert H. Rainbird. "Tectonic accommodation and alluvial sequence stratigraphy of a Paleoproterozoic continental rift, Baker Lake Basin, Canada." Stratigraphy 3, no. 4 (2006): 263–83. http://dx.doi.org/10.29041/strat.03.4.02.

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A model, based upon pre-existing formulations, is presented here for alluvial sequence stratigraphy and applied to the non-marine, Paleoproterozoic Baker Lake Basin. Discharge and sediment supply are considered boundary conditions, subject to feedback effects. Primary control on alluvial facies changes is attributed to the gradient of the alluvial plain. This gradient is determined by the “graded profile", a topographic profile defined by a graded stream linking a sediment source region to a subaqueous basin. It is argued that coupled source uplift and basin subsidence provide feedback on sedi

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Wescott, William A., William N. Krebs, John C. Dolson, Salah A. Karamat, and Dag Nummedal. "Rift Basin Sequence Stratigraphy: Some Examples from the Gulf Of Suez." GeoArabia 1, no. 2 (1996): 343–58. http://dx.doi.org/10.2113/geoarabia0102343.

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ABSTRACT Unconformity-bounded sequences within the Miocene strata of the Suez Rift reflect a complex interplay between tectonism and sea level fluctuations. Analyses of Miocene outcrops along the Sinai margin of the Gulf of Suez provide new insights into the sequence stratigraphy of this basin. The Miocene strata can be subdivided into seven major sequences separated by biostratigraphically defined time breaks. These lacunae represent depositional sequence boundaries, transgressive surfaces and condensed sections. These basinwide time breaks were related to major tectonic events from rift init

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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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Shaffer, Bernard L., Jory A. Pacht, and Bruce E. Bowen. "Aspects of Gulf Coast late Neogene sequence stratigraphy." Paleontological Society Special Publications 6 (1992): 268. http://dx.doi.org/10.1017/s2475262200008285.

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With its vast well and seismic data base, coupled with expanded sedimentary and biostratigraphic cycles that apparently were driven by glacial eustacy, the Gulf Coast offshore region provides a unique opportunity to develop and test sequence models. Virtually every major oil company and a number of academic institutions are currently engaged in some form of sequence analysis.Regional studies incorporating biostratigraphic analyses of more than 120 wells integrated with a seismic grid exceeding 24,000 line smiles, have shown the Gulf Coast to be an unstable prograding margin, and that character

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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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Moghaddam, H. V., and H. Torabi. "Biofacies and sequence stratigraphy of the Oligocene succession, Central Basin, Iran." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2004, no. 6 (2004): 321–34. http://dx.doi.org/10.1127/njgpm/2004/2004/321.

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33

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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35

Abbasi, Samira, Saeid Pourmorad, Ashutosh Mohanty, Shakura Jahan, and Nilanchal Patel. "Sedimentological Studies of Marine Oil Fields in Order to Reduce Drilling Risk and Environmental Pollution: A Case Study of South of Iran." BOHR International Journal of Civil Engineering and Environmental Science 1, no. 2 (2022): 50–61. http://dx.doi.org/10.54646/bijcees.006.

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Detailed studies of sedimentology and petrology of oil ﬁelds, especially oil ﬁelds located in the seas, play a very important role in reducing the risk of danger, increasing harvest, and reducing the amount of environmental pollution. The South Pars gas ﬁeld in the waters of the Persian Gulf on the joint border line of Iran and Qatar and on the south coast of Iran has been used as a comprehensive model for this type of study. In these studies, the sedimentary environment and sequential stratigraphy of the Scorpion and Sarvak Formations in the South Pars gas ﬁeld in wells 1 and 3 have been inve

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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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Abbasi, Samira, Saeid Pourmorad, Ashutosh Mohanty та Shakura Jahan. "Sedimentological studies of marine oil ﬁelds in order to reduce drilling risk and environmental pollution: a case study of South of Iran". BOHR International Journal of Civil Engineering and Environmental Science 1, № 2 (2023): 50–62. http://dx.doi.org/10.54646/bijcees.2023.06.

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Detailed studies of sedimentology and petrology of oil fields, especially oil fields located in the seas, play avery important role in reducing the risk of danger, increasing harvest, and reducing the amount of environmentalpollution. The South Pars gas field in the waters of the Persian Gulf on the joint border line of Iran and Qatar andon the south coast of Iran has been used as a comprehensive model for this type of study. In these studies, thesedimentary environment and sequential stratigraphy of the Scorpion and Sarvak Formations in the South Parsgas field in wells 1 and 3 have been inves

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38

Smith, Greg C., and Robert G. Cowley. "THE TECTONO-STRATIGRAPHY AND PETROLEUM POTENTIAL OF THE NORTHERN ABROLHOS SUB BASIN, WESTERN AUSTRALIA." APPEA Journal 27, no. 1 (1987): 112. http://dx.doi.org/10.1071/aj86012.

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The Abrolhos Sub-basin lies offshore in Western Australia to the west of Geraldton and has geological affinities with the northern Perth Basin and the southern Carnarvon Basin. Both of these basins contain commercial petroleum accumulations, whereas the Abrolhos Sub-basin is a frontier area which is largely unexplored. A moderate seismic coverage of the sub-basin now exists but only two wells have been drilled, both of which were dry.Four main tectono-stratigraphic sequences are recognisable above Precambrian basement:Lower Palaeozoic Pre Rift SequenceCarboniferous-Permian Synrift/Rift Sequenc

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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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40

Liu, Jin Shui, Ming Zhang, Jin Liang Zhang, Chun Yan Wang, and Peng Hui Zhang. "Tectonic Evolution and Sequence Filling of Paleocene in Lishui Sag, East China Sea Shelf Basin." Advanced Materials Research 807-809 (September 2013): 2244–48. http://dx.doi.org/10.4028/www.scientific.net/amr.807-809.2244.

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The Lishui sag located at Southwest of the East China Sea Shelf Basin. It had undergone the four stages of syn-rift processes in Late Cretaceous to Paleocene: initial rift stage, main rift stage, stable rift stage and decline stage. The tectonic evolution has control effect on the development of sequence stratigraphy and the sediments distribution. Three second-order sequences, five third-order sequences and twelve system tracts are distinguished. Different sedimentary facies recognized in the Lishui sag.

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41

Idrissi, Assia, Mohamed Saadi, Yassir Astati, Ali Bouayachi, and Kawtar Benyas. "Mapping of Genetic Sequences of the Cambrian Series in the Jbel Saghro Massif, Eastern Anti-Atlas, Morocco: Implications for Eustatic and Tectonic Controls." Iraqi Geological Journal 55, no. 1D (2022): 1–20. http://dx.doi.org/10.46717/igj.55.1d.1ms-2022-04-17.

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In this paper, a sedimentological and sequence stratigraphy analysis was performed on Lower and Middle Cambrian deposits of Jbel Saghro, Eastern Anti-Atlas. The field data analysis and the application of sequence stratigraphy concepts were used to classify sedimentary processes and depositional environment, and to define the Lower to Middle Cambrian basin’s detailed geometry. The Cambrian sedimentation of northeastern Saghro indicates a deltaic environment, which is composed of two depositional sequences. These sequences are made of a transgressive system-tract with retrograding sediments and

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Simmons, Michael D., Peter R. Sharland, David M. Casey, Roger B. Davies, and Owen E. Sutcliffe. "Arabian Plate sequence stratigraphy: Potential implications for global chronostratigraphy." GeoArabia 12, no. 4 (2007): 101–30. http://dx.doi.org/10.2113/geoarabia1204101.

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ABSTRACT The ability to recognise and correlate third-order depositional sequences across Arabia and between Arabia and other plates indicates that these sequences are driven by synchronous eustatic sea-level change. This is of value in providing guidance for the definitions of stages, which are the fundamental units of chronostratigraphy. Each Phanerozoic stage requires a Global Stratotype Section and Point (GSSP), which is a location and specific bedding plane where the base of each stage is defined. This definition is tied to an event in the rock record useful for correlation. Progress in d

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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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Barker, G. W. W. "From Classification to Interpretation: Libyan Prehistory, 1969–1989." Libyan Studies 20 (January 1989): 31–43. http://dx.doi.org/10.1017/s0263718900006579.

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In the 15 years following the Second World War, the available data on the prehistory of North Africa were summarised in a series of major syntheses (notably Alimen 1955; Balout 1955; Ford-Johnston 1959; and Vaufrey 1955). With stratified sequences few and far between, radiometric techniques of absolute dating still at the developmental stage, and little detailed information on palaeoenvironments, it was inevitable that the emphasis of all these studies was on the description and classification of the archaeological record, and its organisation into regional cultural sequences. As far as Libya

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Arifin, Lukman, and Tommy Naibaho. "STRUKTUR GEOLOGI DI PERAIRAN PULAU BUTON SELATAN." JURNAL GEOLOGI KELAUTAN 13, no. 3 (2016): 143. http://dx.doi.org/10.32693/jgk.13.3.2015.269.

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Penelitian geofisika dengan metode seismik pantul dangkal dilakukan di perairan Pulau Buton bagian selatan. Tujuan dari penelitian adalah untuk mengetahui kondisi geologi di bawah permukaan dasar laut. Dari data rekaman seismik diinterpretasikan bahwa stratigrafi seismik dibagi menjadi dua runtunan yaitu runtunan A dan B. Bila disebandingkan dengan geologi daratnya maka runtunan A termasuk dalam Formasi Wapulaka yang berumur Tersier dan runtunan B termasuk Formasi Sampolakosa yang berumur Kuater. Data rekaman tersebut juga menunjukkan adanya beberapa struktur geologi seperti sesar, lipatan, da

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Gonzalez, Wilma B. Aleman, Jean M. Self-Trail, W. Burleigh Harris, Jessica Pierson Moore, and Kathleen M. Farrell. "Depositional sequence stratigraphy of Turonian to Santonian sediments, Cape Fear arch, North Carolina Coastal Plain, USA." Stratigraphy 16, no. 1 (2020): 293–314. http://dx.doi.org/10.29041/strat.17.4.293-314.

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ABSTRACT: A new sequence stratigraphic framework for Turonian to Santonian (94-84 Ma) sediments is established using data from the USGS Kure Beach and Elizabethtown cores collected from the Atlantic Coastal Plain of North Carolina (NC). These sediments represent some of the oldest marine units deposited on the southeastern Atlantic Coastal Plain and record the early development of a clastic wedge atop crystalline basement. Sediments were deposited as transitional marginal-marine to marine units in a complex interplay of fluvial, estuarine, and shelf environments. Repetitive lithologies and min

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Rudolph, Kurt W., William J. Devlin, and Jeff P. Crabaugh. "Upper Cretaceous Sequence Stratigraphy of the Rock Springs Uplift, Wyoming." Mountain Geologist 52, no. 3 (2015): 13–157. http://dx.doi.org/10.31582/rmag.mg.52.3.13.

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Three scales of sedimentary cyclicity are observed in the Campanian to Maastrichtian-aged strata of southwestern Wyoming based on sedimentary stacking patterns, facies successions, paleontological data and geometric criteria from outcrop, and subsurface data. The largest scale of sequence stratigraphic interpretation is of 10-15 million years duration per cycle and is designated as second order. Second-order cyclicity is represented by profound sequence boundaries and maximum-flooding surfaces that are related to regional tectono-subsidence drivers. The 2nd-order sequence boundaries at the bas

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Moore Jr., Theodore C., David K. Rea, Larry A. Mayer, C. F. Michael Lewis, and David M. Dobson. "Seismic stratigraphy of Lake Huron – Georgian Bay and postglacial lake level history." Canadian Journal of Earth Sciences 31, no. 11 (1994): 1606–17. http://dx.doi.org/10.1139/e94-142.

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Five seismic reflectors in the basinal sedimentary section have been identified as representing erosional surfaces in shoaler regions of the lake basins and can be traced throughout most of the study area. The reflectors representing these erosional surfaces, and their conformable equivalents in the deep lake basins, are caused by intervals of coarser grain size in the sediments and are thought to represent lowering of lake levels prior to, and following, the Main Algonquin highstand (about 10.2 – 11.0 ka). These reflectors are used to define seismic sequences in the postglacial sedimentary fi

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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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Amiewalan, F. O., and F. A. Lucas. "Sequence Stratigraphic Interpretation of FX-1 and FX-2 wells, Onshore Western Niger Delta, Nigeria." Journal of Applied Sciences and Environmental Management 24, no. 2 (2020): 303–11. http://dx.doi.org/10.4314/jasem.v24i2.17.

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The area of study is a portion of the Greater Ughelli Depobelt in Niger Delta Basin. The main aim of the paper is to interpret the sequence stratigraphy of FX-1 and FX-2 wells by employing data sets from biostratigraphic data and well logs. Standard laboratory techniques were used for data treatment while computer software such as Petrel and StrataBugs were used for data simulation, processing, integration and interpretation. Sedimentology, interpreted gamma ray and resistivity well logs integrated with biostratigraphic data were utilized to define the candidate maximum flooding surfaces and s

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