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Relevant bibliographies by topics / Sequence stratigrapy

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Journal articles

Academic literature on the topic 'Sequence stratigrapy'

Author: Grafiati

Published: 18 May 2024

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Journal articles on the topic "Sequence stratigrapy"

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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2

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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3

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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6

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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7

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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8

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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