干旱区生态环境知识资源中心(Arid): Characteristics and deposition models of the paleocene source rocks in the Lishui Sag, east China sea shelf basin: Evidences from organic and inorganic geochemistry

Arid

DOI	10.1016/j.petrol.2021.108342
	Characteristics and deposition models of the paleocene source rocks in the Lishui Sag, east China sea shelf basin: Evidences from organic and inorganic geochemistry
	Lei, Chuang; Yin, Shiyan; Ye, Jiaren; Wu, Jingfu; Wang, Zhaosheng; Gao, Bin
通讯作者	Ye, JR (corresponding author), China Univ Geosci Wuhan, Key Lab Tecton & Petr Resources, Minist Educ, Wuhan 430074, Peoples R China.
来源期刊	JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
ISSN	0920-4105
EISSN	1873-4715
出版年	2021
卷号	200
英文摘要	The Lishui Sag, situated at the East China Sea Shelf Basin, is regarded as one of the most prospecting oil exploration zones. Low exploration in this region requires detailed identification of source rocks to enhance further oil and gas exploration. Three potential source rocks, including the Paleocene Yueguifeng (E(1)y), Lingfeng (E(1)l) and Mingyuefeng (E(1)m) Formations, were investigated by integrating organic and inorganic geochemistry to estimate hydrocarbon generation potential, and to document original organic matter input and deposition environments. Two deposition models for source rocks were established considering tectonic subsidence and climate variation. The result shows that the E(1)y mudstones are dominated by high TOC content, oil/gas-prone kerogen at moderate maturity stage with relatively high hydrocarbon generation potential, whereas E(1)l and E(1)m mudstones are dominated by low TOC content, gas-prone kerogen at low to moderate maturity stage with low hydrocarbon generation potential, and coals with high hydrocarbon generation potential. The original organic matter input and deposition environment are obviously different among these three potential source rocks and are controlled by the coupling of tectonic subsidence and climate variation. Insufficient material supply lead mudstone deposition in a hemi-deep/deep lake during the E(1)y period, resulting in inefficient water mixing and stable water column stratification (high Gammacerane Indexs). The weak water inflow supplied minor oxygen and terrigenous organic matter to the lake due to arid-hot climate, as indicated by low Pr/Ph, C-19 T/C23T, C-20 T/C23T and C(24)Tet/C26T ratios, low Oleanane Indexs, and high C-35 Homohopane Indexs and V/Ni ratios. Water algae, including pediastrums and chlorellas, which contributed to the development of high-quality source rocks, could be efficiently preserved in dysoxic condition. High subsidence rate together with sufficient sediment supply during the transgression in the E(1)l and E(1)m periods developed a coastal marine or paralic environment. The alternated climate brought unstable water inflow against stable water column stratification (low Gammacerane Indexs). Strong water inflow due to warm-humid climate provides abundant terrigenous organic matter and oxygen to the lake as indicated by high Pr/Ph, C-19 T/C23T, C-20 T/C23T and C(24)Tet/C26T ratios, high Oleanane Indexs, low C-35 Homohopane Indexs and V/Ni ratios, and rich C-29 steranes. Algal might be preferentially oxidized and degraded in aerobic conditions. Thus, mudstone is regarded as general-quality source rocks but coal is regarded as high-quality source rocks. Weak water inflow under arid-hot climate provided subtle aquatic and terrigenous organic matter to the lake, resulting in poor-quality source rocks.
英文关键词	Organic matter input Deposition environment Source rock deposition model Lishui sag East China Sea shelf basin
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000628819200038
WOS类目	Energy & Fuels ; Engineering, Petroleum
WOS研究方向	Energy & Fuels ; Engineering
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/368831
作者单位	[Lei, Chuang; Yin, Shiyan; Wang, Zhaosheng; Gao, Bin] North China Univ Sci & Technol, Coll Min Engn, Tangshan 063210, Peoples R China; [Yin, Shiyan; Ye, Jiaren] China Univ Geosci Wuhan, Key Lab Tecton & Petr Resources, Minist Educ, Wuhan 430074, Peoples R China; [Wu, Jingfu] CNOOC Res Inst Ltd, Beijing 100028, Peoples R China
推荐引用方式 GB/T 7714	Lei, Chuang,Yin, Shiyan,Ye, Jiaren,et al. Characteristics and deposition models of the paleocene source rocks in the Lishui Sag, east China sea shelf basin: Evidences from organic and inorganic geochemistry[J],2021,200.
APA	Lei, Chuang,Yin, Shiyan,Ye, Jiaren,Wu, Jingfu,Wang, Zhaosheng,&Gao, Bin.(2021).Characteristics and deposition models of the paleocene source rocks in the Lishui Sag, east China sea shelf basin: Evidences from organic and inorganic geochemistry.JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING,200.
MLA	Lei, Chuang,et al."Characteristics and deposition models of the paleocene source rocks in the Lishui Sag, east China sea shelf basin: Evidences from organic and inorganic geochemistry".JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING 200(2021).