陆相断陷湖盆迁移型层序构型及意义：以珠Ⅰ坳陷古近系文昌组为例

朱红涛; 李森; 刘浩冉; 舒誉; 梅廉夫; 杨香华

doi:10.3799/dqkx.2016.028

Volume 41 Issue 3

Mar. 2016

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Article Navigation > Earth Science > 2016 > 41(3): 361-372

Zhu Hongtao, Li Sen, Liu Haoran, Shu Yu, Mei Lianfu, Yang Xianghua, 2016. The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin. Earth Science, 41(3): 361-372. doi: 10.3799/dqkx.2016.028

Citation:

Zhu Hongtao, Li Sen, Liu Haoran, Shu Yu, Mei Lianfu, Yang Xianghua, 2016. The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin. Earth Science, 41(3): 361-372. doi: 10.3799/dqkx.2016.028

Citation:

Zhu Hongtao, Li Sen, Liu Haoran, Shu Yu, Mei Lianfu, Yang Xianghua, 2016. The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin. Earth Science, 41(3): 361-372. doi: 10.3799/dqkx.2016.028

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The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin

doi: 10.3799/dqkx.2016.028

Zhu Hongtao^{1,2
,},
Li Sen^1,2,
Liu Haoran^1,2,
Shu Yu³,
Mei Lianfu^1,2,
Yang Xianghua^1,2

1.
Key Laboratory of Tectonics and Petroleum Resources, China University of Geoscien, 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: 2015-10-11
Publish Date: 2016-03-15

Abstract

Abstract

Compared with the sequences of marine basins, sequence stratigraphic architecture of non-marine basins is characterized by multi-variation and uncertainty. Migrated sequence stratigraphic architecture is one non-normal type in the evolution of continental lacustrine rift basin, which is rare documented. Based on the sequence stratigraphic units analysis of Paleogene Wenchang Formation of Huizhou and Enping sags, Zhu Ⅰ Depression, Pearl River Mouth Basin, this paper defined the concept of migrated sequence stratigraphic architecture and divided into autogenic and allogenic migration. Autogenic migrated sequences are mainly controlled by horizontal displacement of low-angle syndepositional normal fault, whereas allogenic migrated sequences are controlled by the different tectonic activation episodes of boundary fault on both sides of the basin. In other words, autogenic and allogenic migrated sequences are controlled by one and two syndepositional boundary fault, respectively. During the lateral migration of sequences, reservoirs and source rocks controlled by sequence stratigraphic units at multiple scales also migrate and stack laterally. This helps the high-efficient configuration of hydrocarbon accumulation factors (e.g., source rock, reservoir, and seal) to generate reservoir combination with multiple blocks and multiple strata.
- Migrated sequence stratigraphic architecture,
- autogenic migration,
- allogenic migration,
- hydrocarbons,
- Zhu Ⅰ depression,
- Wenchang Formation.

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References(60)

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The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin

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