2019Petroleum Science and TechnologyRequires access

Source of Chang 10 crude oil in Zhidan area, Ordos Basin, China

Zhanxi Chen, Shijia Chen, Zhenglu Xiao, Meimei Han, Wen Qiu

Open publisher page 6 citations

Abstract

Numerous studies on the oil source of Chang 10 reservoir in the Zhidan area were undertaken until now, but still have no definite conclusion. Based on the comparisons and analyses of geochemical parameters between Chang 7 to Chang 9 source rocks and Chang 10 crude oil, it is found that the forming environments of the crude oil in the Chang 10 member are similar to Chang 7 and Chang 9 source rocks, as they occur both in weak reduction environments. C30 hopane(C30H), Ts, C30 rearranged hopane(C30*), Ts/C30H and C30*/C30H range of two types of crude oil in the Chang 10 member are similar to those of Chang 7 and Chang 9 source rocks, respectively. The results show that the crude oil in the Chang 10 member is a mixed product of Chang 7 and Chang 9 source rocks.

About this research paper

What this paper is about

Numerous studies on the oil source of Chang 10 reservoir in the Zhidan area were undertaken until now, but still have no definite conclusion. Based on the comparisons and analyses of geochemical parameters between Chang 7 to Chang 9 source rocks and Chang 10 crude oil, it is found that the forming environments of the crude oil in the Chang 10 member are similar to Chang 7 and Chang 9 source rocks, as they occur both in weak reduction environments. C30 hopane(C30H), Ts, C30 rearranged hopane(C30*), Ts/C30H and C30*/C30H range of two types of crude oil in the Chang 10 member are similar to those of Chang 7 and Chang 9 source rocks, respectively. The results show that the crude oil in the Chang 10 member is a mixed product of Chang 7 and Chang 9 source rocks.

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Available abstract

Numerous studies on the oil source of Chang 10 reservoir in the Zhidan area were undertaken until now, but still have no definite conclusion. Based on the comparisons and analyses of geochemical parameters between Chang 7 to Chang 9 source rocks and Chang 10 crude oil, it is found that the forming environments of the crude oil in the Chang 10 member are similar to Chang 7 and Chang 9 source rocks, as they occur both in weak reduction environments. C30 hopane(C30H), Ts, C30 rearranged hopane(C30*), Ts/C30H and C30*/C30H range of two types of crude oil in the Chang 10 member are similar to those of Chang 7 and Chang 9 source rocks, respectively. The results show that the crude oil in the Chang 10 member is a mixed product of Chang 7 and Chang 9 source rocks.

Key concepts: Source rock, Hopanoids, Crude oil, Geochemistry, Geology, Structural basin, Light crude oil, Mineralogy

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