Sedimentary records of seismic events in a lacustrine basin of continental depression: A case study of the Triassic Yanchang Formation in the Ordos Basin, Northern China
[Display omitted] •In the Ordos Basin, the Triassic Yanchang Formation contains abundant seismites.•Ten types of seismites have been identified in the lacustrine deposits of the Ordos Basin.•The sedimentary sequence of seismites represents the periodicity of seismicity.•Seismites are of great signif...
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| Published in | Journal of Asian earth sciences Vol. 228; p. 105128 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier Ltd
01.05.2022
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| Subjects | |
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| Abstract | [Display omitted]
•In the Ordos Basin, the Triassic Yanchang Formation contains abundant seismites.•Ten types of seismites have been identified in the lacustrine deposits of the Ordos Basin.•The sedimentary sequence of seismites represents the periodicity of seismicity.•Seismites are of great significance in oil and gas exploration, sedimentology and structural geology.
Being a continental lake basin, the Ordos Basin was filled with a Triassic sedimentary succession including the Yanchang Formation in which there are widespread seismites formed via sudden seismic events. Our study focuses on types and characteristics of these seismites and concerns their sequence of the formation, genetic mechanism, and significance. The results show that the identification marks denoting the seismic sedimentary event of the Yanchang Formation include ten different types. The sedimentary sequence consists of the five units: A or F (Liquefaction homogeneous stratum), B (Micro synsedimentary fault stratum), C (Crimped deformation stratum), D (Liquefied sandstone vein), and E (Sand ball-pillow stratum) that can be further divided into five sub-types: ABCD, BCD or CD, AB, BCE or BE, and BEBE. The strong episodic activity of the boundary faults controlling the basin is the direct cause of the seismic sedimentary events. The study of seismites is helpful to understand the structural geology of Ordos Basin, the relationship between the dynamic mechanisms of the sedimentation in different reservoir sand bodies, and provide a new perspective for oil and gas exploration. |
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| AbstractList | [Display omitted]
•In the Ordos Basin, the Triassic Yanchang Formation contains abundant seismites.•Ten types of seismites have been identified in the lacustrine deposits of the Ordos Basin.•The sedimentary sequence of seismites represents the periodicity of seismicity.•Seismites are of great significance in oil and gas exploration, sedimentology and structural geology.
Being a continental lake basin, the Ordos Basin was filled with a Triassic sedimentary succession including the Yanchang Formation in which there are widespread seismites formed via sudden seismic events. Our study focuses on types and characteristics of these seismites and concerns their sequence of the formation, genetic mechanism, and significance. The results show that the identification marks denoting the seismic sedimentary event of the Yanchang Formation include ten different types. The sedimentary sequence consists of the five units: A or F (Liquefaction homogeneous stratum), B (Micro synsedimentary fault stratum), C (Crimped deformation stratum), D (Liquefied sandstone vein), and E (Sand ball-pillow stratum) that can be further divided into five sub-types: ABCD, BCD or CD, AB, BCE or BE, and BEBE. The strong episodic activity of the boundary faults controlling the basin is the direct cause of the seismic sedimentary events. The study of seismites is helpful to understand the structural geology of Ordos Basin, the relationship between the dynamic mechanisms of the sedimentation in different reservoir sand bodies, and provide a new perspective for oil and gas exploration. |
| ArticleNumber | 105128 |
| Author | Tian, Jingchun Yu, Wei Li, Jian Liang, Qingshao Wang, Feng Chen, Weizhen |
| Author_xml | – sequence: 1 givenname: Jingchun surname: Tian fullname: Tian, Jingchun organization: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China – sequence: 2 givenname: Qingshao surname: Liang fullname: Liang, Qingshao email: liangqingshao@foxmail.com organization: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China – sequence: 3 givenname: Feng surname: Wang fullname: Wang, Feng organization: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China – sequence: 4 givenname: Jian surname: Li fullname: Li, Jian organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology), Chengdu, Sichuan 610059, China – sequence: 5 givenname: Wei surname: Yu fullname: Yu, Wei organization: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China – sequence: 6 givenname: Weizhen surname: Chen fullname: Chen, Weizhen organization: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China |
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•In the Ordos Basin, the Triassic Yanchang Formation contains abundant seismites.•Ten types of seismites have been identified in the... |
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| SubjectTerms | Characteristics of seismite Genetic mechanism Ordos Basin Seismite sequence Yanchang Formation |
| Title | Sedimentary records of seismic events in a lacustrine basin of continental depression: A case study of the Triassic Yanchang Formation in the Ordos Basin, Northern China |
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