珠江口盆地惠州凹陷迁移型层序特征及其意义

刘浩冉; 朱红涛; 施和生; 舒誉; 付鑫; 刘依梦

doi:10.3799/dqkx.2015.068

Volume 40 Issue 5

May 2015

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Article Navigation > Earth Science > 2015 > 40(5): 840-850

Liu Haoran, Zhu Hongtao, Shi Hesheng, Shu Yu, Fu Xin, Liu Yimeng, 2015. Migrated Sequence Stratigraphic Architecture and Its Geological Significance in Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(5): 840-850. doi: 10.3799/dqkx.2015.068

Citation:

Liu Haoran, Zhu Hongtao, Shi Hesheng, Shu Yu, Fu Xin, Liu Yimeng, 2015. Migrated Sequence Stratigraphic Architecture and Its Geological Significance in Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(5): 840-850. doi: 10.3799/dqkx.2015.068

Citation:

Liu Haoran, Zhu Hongtao, Shi Hesheng, Shu Yu, Fu Xin, Liu Yimeng, 2015. Migrated Sequence Stratigraphic Architecture and Its Geological Significance in Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(5): 840-850. doi: 10.3799/dqkx.2015.068

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Migrated Sequence Stratigraphic Architecture and Its Geological Significance in Huizhou Depression, Pearl River Mouth Basin

doi: 10.3799/dqkx.2015.068

Liu Haoran^{1, 2
,},
Zhu Hongtao^{1, 2
,
,},
Shi Hesheng³,
Shu Yu³,
Fu Xin^{1, 2},
Liu Yimeng^{1, 2}

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
China National Offshore Oil Corporation Limited-Shenzhen, Guangzhou 510240, China

Received Date: 2014-10-27
Publish Date: 2015-05-15

Abstract

Abstract

Migrated sequence stratigraphic architecture represents a special type in continental lacustrine rift basin. However, its characteristics and main controlling factors are unclear yet. Lower Wenchang Formation (PSQ1-PSQ4) is mainly distributed at south of Huizhou depression, while upper Wenchang Formation (PSQ5-PSQ7) is distributed at northern part. It is found in this study that sequences in Wenchang Formation migrate from southeast to northwest across Huizhou depression. Migration of sequence is generally caused by different stages of episodic tectonic activity. In rifted stage IA, tectonic activities of southern depression strengthen largely and sequences configuration show as Type T, which mostly develops lower Wenchang Formation. However, as for rifted stage IB, northern tectonic activities become stronger, which results in migration of depocenter and subsidence center from north to south. And sequences configuration show as Type H which mainly develops upper Wenchang Formation. Moreover, migration of sequence stratigraphic unit generates multi-block along the direction of migration and also a combination of multi-stage oil and gas reservoirs, which are all of great potential for exploration.
- migrated sequence stratigraphic architecture,
- episodic tectonic activity,
- Wenchang Formation,
- Huizhou depression,
- petroleum geology,
- stratigraphy

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References(66)

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Migrated Sequence Stratigraphic Architecture and Its Geological Significance in Huizhou Depression, Pearl River Mouth Basin

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