渤海湾盆地饶阳凹陷沙一下亚段古湖泊环境与烃源岩发育模式

殷杰; 王权; 郝芳; 郭柳汐; 邹华耀

doi:10.3799/dqkx.2017.098

Volume 42 Issue 7

Jul. 2017

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Article Navigation > Earth Science > 2017 > 42(7): 1209-1222

Yin Jie, Wang Quan, Hao Fang, Guo Liuxi, Zou Huayao, 2017. Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin. Earth Science, 42(7): 1209-1222. doi: 10.3799/dqkx.2017.098

Citation:

Yin Jie, Wang Quan, Hao Fang, Guo Liuxi, Zou Huayao, 2017. Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin. Earth Science, 42(7): 1209-1222. doi: 10.3799/dqkx.2017.098

Citation:

Yin Jie, Wang Quan, Hao Fang, Guo Liuxi, Zou Huayao, 2017. Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin. Earth Science, 42(7): 1209-1222. doi: 10.3799/dqkx.2017.098

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Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin

doi: 10.3799/dqkx.2017.098

Yin Jie^1
,,
Wang Quan²,
Hao Fang^3,4,
Guo Liuxi²,
Zou Huayao^{1
,
,}

1.
College of Geosciences, China University of Petroleum, Beijing 102249, China
2.
Exploration and Development Research Institute of PetroChina Huabei Oilfield Company, Renqiu 062552, China
3.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
4.
China University of Petroleum, Qingdao 266580, China

Received Date: 2017-01-04
Publish Date: 2017-07-15

Abstract

Abstract

Despite successful studies on source rocks of Raoyang sag, existing studies on the ancient lake environment during lower submember of Sha1 source rocks development period are not systematic, an important factor controlling the geochemical characteristics and temporal and spatial distribution of source rocks, is often ignored.In this study, samples of source rocks in the lower submember of Sha1 were analyzed with palaeontological material, organic geochemistry, trace element and isotopic geochemistry to reveal the paleolake environment including the paleoclimate, water depth, salinity, organic matter preservation and productivity, and to construct depositional model for high-quality source rocks of the lower submember of Sha1.Results show that the high-quality source rocks mainly formed in the transgressive system tracts period.Meantime, the climate was in the transition from arid to humid, and the water depth of the paleolake was about 2-14 meters, wave base depth was 7.5 meters.Paleosalinity parameters such as Sr/Ba and B/Ga indicate the lower submember of Sha1 belonged to the saline environment due to the effect of water evaporation.High salinity was favorable to stable halocline formation, resulting in the bottom water in an anoxic condition for the preservation of organic matter.And the stable carbon isotope and nutrient elements distribution characteristics display that the surface water had high initial productivity in the stage of the lower submember of Sha1.Such paleolake environment caused wide distribution of strong reducing salt water semi-deep lake organic facies, beneficial to the growth of high-quality hydrocarbon source rocks.
- Raoyang sag,
- the lower submember of Sha1,
- paleolake,
- high-quality source rock,
- development model,
- petroleum geology

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References(91)

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Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin

doi: 10.3799/dqkx.2017.098

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