涠西南凹陷一号断裂陡坡带扇体沉积展布特征及主控因素

姜平; 秦春雨; 杨希冰; 何杰; 陆江; 赵彦璞; 罗碧华

doi:10.3799/dqkx.2018.369

Volume 45 Issue 2

Feb. 2020

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Article Navigation > Earth Science > 2020 > 45(2): 534-546

Jiang Ping, Qin Chunyu, Yang Xibing, He Jie, Lu Jiang, Zhao Yanpu, Luo Bihua, 2020. Sedimentary Architecture, Distribution Features and Genesis of Steep Slope Fan in Upper Liushagang Formation, Weixi'nan Sag. Earth Science, 45(2): 534-546. doi: 10.3799/dqkx.2018.369

Citation:

Jiang Ping, Qin Chunyu, Yang Xibing, He Jie, Lu Jiang, Zhao Yanpu, Luo Bihua, 2020. Sedimentary Architecture, Distribution Features and Genesis of Steep Slope Fan in Upper Liushagang Formation, Weixi'nan Sag. Earth Science, 45(2): 534-546. doi: 10.3799/dqkx.2018.369

Citation:

Jiang Ping, Qin Chunyu, Yang Xibing, He Jie, Lu Jiang, Zhao Yanpu, Luo Bihua, 2020. Sedimentary Architecture, Distribution Features and Genesis of Steep Slope Fan in Upper Liushagang Formation, Weixi'nan Sag. Earth Science, 45(2): 534-546. doi: 10.3799/dqkx.2018.369

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Sedimentary Architecture, Distribution Features and Genesis of Steep Slope Fan in Upper Liushagang Formation, Weixi'nan Sag

doi: 10.3799/dqkx.2018.369

Jiang Ping^{1
,
,},
Qin Chunyu^{2
,
,},
Yang Xibing¹,
He Jie²,
Lu Jiang¹,
Zhao Yanpu²,
Luo Bihua¹

1.
Zhanjiang Branch of CNOOC Co. Ltd., Zhanjiang 524057, China
2.
Faculty of Earth Resources, China Unoversity of Geosciences, Wuhan 430074, China

Received Date: 2018-12-22
Publish Date: 2020-02-15

Abstract

Abstract

Using high quality 3D seismic data, combining analyses of light and heavy minerals, core observation and sand grain size distributions, sedimentary architecture and distribution features of steep slope fan in Upper Liushagang Formation of Weixi'nan Sag have been investigated in this study. These features vary along the NO.1 border fault:In the western part of steep slope belt, large-scale incised valleys developed, producing large-scale sub-lacustrine fans, which are characterized by thick beds of debris flow deposits; While in the middle part, small-scale channelized turbidite sub-lacustrine fans dominated; In eastern part, a series of small-scale symmetrical fans were located along the border fault, with sparse valleys present. Lateral variations of sediment supply, geomorphology and subsidence rate induced by multiple stages of border fault activity are considered the controlling factors:Fault slope in western part feeds coarser sediments from larger drainages. Meanwhile, large-scale incised valleys and complex morphology allow the growth of larger, asymmetrical fan lobes; On the other hand, fault slopes in the middle and eastern part with planar style and ramp-flat structure, respectively, provide a limited supply to multiple small fans.
- border fault,
- Weixi'nan sag,
- fan distribution,
- controlling factors,
- paleogeomorphology,
- oil-gas geology

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References(49)

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