Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China)
Based on core, well-logging and seismic data, the gravity flow characteristics and sedimentary model of the 1st member of the Tengger formation in the eastern steep slope belt of the Sai-4 tectonic belt in the Saihantala depression (Erlian Basin, China) have been systematically studied; further, the...
Main Authors: | , , , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
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SAGE Publishing
2023-07-01
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Series: | Energy Exploration & Exploitation |
Online Access: | https://doi.org/10.1177/01445987231164243 |
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author | Zhiping Zhang Hongyan Ren Hongfeng Zhou Youliang Ji Wanglin Wu Yong Zhou Lin Tang Ruijing Guo Dongji Yang Chuanmeng Pang Jia Sun Shanshan Guo Chenxi Gao Zhengtao Ma Xiaoyu Liu |
author_facet | Zhiping Zhang Hongyan Ren Hongfeng Zhou Youliang Ji Wanglin Wu Yong Zhou Lin Tang Ruijing Guo Dongji Yang Chuanmeng Pang Jia Sun Shanshan Guo Chenxi Gao Zhengtao Ma Xiaoyu Liu |
author_sort | Zhiping Zhang |
collection | DOAJ |
description | Based on core, well-logging and seismic data, the gravity flow characteristics and sedimentary model of the 1st member of the Tengger formation in the eastern steep slope belt of the Sai-4 tectonic belt in the Saihantala depression (Erlian Basin, China) have been systematically studied; further, the sublacustrine fan sedimentary model in the study area has been established. The main types of gravity flow identified in the study area are sandy debris flow deposits and turbidity flow deposition. Affected by paleo-geomorphology, provenance and other factors, sublacustrine fans in the eastern steep slope zone are formed by gravity flows from different periods. The sublacustrine fan is divided into three subfacies: inner-fan, mid-fan and outer-fan. The subfacies can be subdivided into six types of microfacies: main channel, levee of main channel, distributary channel, inter-channel, levee of distributary channel and terminals. The formation of the sublacustrine fan is caused by steep slopes and triggered by earthquakes. The sedimentary model of the sublacustrine fan and its sedimentary characteristics provide a foundation for exploring and developing oil and gas in the study area. |
first_indexed | 2024-03-13T03:06:27Z |
format | Article |
id | doaj.art-24bb19ac8c5448259bf3a29fe0dbdd82 |
institution | Directory Open Access Journal |
issn | 0144-5987 2048-4054 |
language | English |
last_indexed | 2024-03-13T03:06:27Z |
publishDate | 2023-07-01 |
publisher | SAGE Publishing |
record_format | Article |
series | Energy Exploration & Exploitation |
spelling | doaj.art-24bb19ac8c5448259bf3a29fe0dbdd822023-06-26T21:34:23ZengSAGE PublishingEnergy Exploration & Exploitation0144-59872048-40542023-07-014110.1177/01445987231164243Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China)Zhiping Zhang0Hongyan Ren1Hongfeng Zhou2Youliang Ji3Wanglin Wu4Yong Zhou5Lin Tang6Ruijing Guo7Dongji Yang8Chuanmeng Pang9Jia Sun10Shanshan Guo11Chenxi Gao12Zhengtao Ma13Xiaoyu Liu14 Institute of Geology, Erlian Branch, North China Oilfield Company, China National Petroleum Corporation, Renqiu, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China Institute of Geology, Erlian Branch, North China Oilfield Company, China National Petroleum Corporation, Renqiu, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China Institute of Geology, Erlian Branch, North China Oilfield Company, China National Petroleum Corporation, Renqiu, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, China State Key Laboratory of Petroleum Resources and Exploration, , Beijing, ChinaBased on core, well-logging and seismic data, the gravity flow characteristics and sedimentary model of the 1st member of the Tengger formation in the eastern steep slope belt of the Sai-4 tectonic belt in the Saihantala depression (Erlian Basin, China) have been systematically studied; further, the sublacustrine fan sedimentary model in the study area has been established. The main types of gravity flow identified in the study area are sandy debris flow deposits and turbidity flow deposition. Affected by paleo-geomorphology, provenance and other factors, sublacustrine fans in the eastern steep slope zone are formed by gravity flows from different periods. The sublacustrine fan is divided into three subfacies: inner-fan, mid-fan and outer-fan. The subfacies can be subdivided into six types of microfacies: main channel, levee of main channel, distributary channel, inter-channel, levee of distributary channel and terminals. The formation of the sublacustrine fan is caused by steep slopes and triggered by earthquakes. The sedimentary model of the sublacustrine fan and its sedimentary characteristics provide a foundation for exploring and developing oil and gas in the study area.https://doi.org/10.1177/01445987231164243 |
spellingShingle | Zhiping Zhang Hongyan Ren Hongfeng Zhou Youliang Ji Wanglin Wu Yong Zhou Lin Tang Ruijing Guo Dongji Yang Chuanmeng Pang Jia Sun Shanshan Guo Chenxi Gao Zhengtao Ma Xiaoyu Liu Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) Energy Exploration & Exploitation |
title | Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) |
title_full | Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) |
title_fullStr | Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) |
title_full_unstemmed | Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) |
title_short | Gravity flow sedimentary characteristics and sedimentary model of the 1 member of the Tengger formation in Saihantala depression (Erlian Basin, China) |
title_sort | gravity flow sedimentary characteristics and sedimentary model of the 1 member of the tengger formation in saihantala depression erlian basin china |
url | https://doi.org/10.1177/01445987231164243 |
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