Apatite fission track analysis of tectono−thermal history in the Xiushui area, southern Songliao Basin

CHEN Shuwang; SUN Shouliang; ZHANG Tao; Kohn Barry P; Gleadow Andrew; LIU Yan; Chung Ling; LI Yongfei; DING Qiuhong

doi:10.12029/gc20210407001

2025 Vol. 52, No. 3

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CHEN Shuwang, SUN Shouliang, ZHANG Tao, Kohn Barry P, Gleadow Andrew, LIU Yan, Chung Ling, LI Yongfei, DING Qiuhong. 2025. Apatite fission track analysis of tectono−thermal history in the Xiushui area, southern Songliao Basin[J]. Geology in China, 52(3): 1055-1068. doi: 10.12029/gc20210407001

Citation:

CHEN Shuwang, SUN Shouliang, ZHANG Tao, Kohn Barry P, Gleadow Andrew, LIU Yan, Chung Ling, LI Yongfei, DING Qiuhong. 2025. Apatite fission track analysis of tectono−thermal history in the Xiushui area, southern Songliao Basin[J]. Geology in China, 52(3): 1055-1068. doi: 10.12029/gc20210407001

Apatite fission track analysis of tectono−thermal history in the Xiushui area, southern Songliao Basin

1.
Shenyang Center, China Geological Survey, Shenyang 110032, Liaoning, China
2.
School of Earth Sciences, The University of Melbourne, Melbourne 3010, Victoria, Australia
3.
College of Resources and Environment, Yangtze University, Wuhan 430100, Hubei, China

Fund Project: Supported by National Natural Science of China (No.41790451) and the projects of China Geological Survey (No.DD20190098, No.DD20190097).

More Information

Author Bio: CHEN Shuwang, male, born in 1964, professor, engaged in basic geological survey of oil and gas; E-mail: sycswgeology@163.com
Corresponding author: SUN Shouliang, male, born in 1982, senior engineer, engaged in petroleum geological exploration and research; E-mail: sunsolar@qq.com.

Received Date: 07 April 2021

Revised Date: 30 December 2021

Publish Date: 25 May 2025

Abstract

Abstract

This paper is the result of oil−gas geological survey engineering.
Objective
The tectono−thermal history of the Cretaceous fault basins in the Songliao peripheral area had not been well explored. The Xiushui Basin is a new exploration area with high hydrocarbon potential in the southern part of the Songliao peripheral area. The reconstruction of the burial and thermal history of the Xiushui Basin has become an important issue for hydrocarbon exploration in this area.
Methods
Based on five samples from Well LFD1 in the Xiushui Basin, burial and thermal history as well as hydrocarbon source rock evolution history of the Xiushui Basin were studied using apatite fission track methods.
Results
The Xiushui Basin reached its maximum burial depth in the late Early Cretaceous, and then uplift continued and denudated about 2000 m. The terrestrial heat flow value increased linearly with time during the initial subsidence period, reaching the maximum value of about 100.5 mW/m² at ~120 Ma, and then experienced a three−stage cooling process, i.e., rapid cooling, then slow cooling, and finally rapid cooling. The heat flow pattern is similar to and comparable with the adjacent Zhangqiang Depression and the Songliao Basin.
Conclusions
The reconstruction results of the burial and thermal history of Well LFD1 indicate that the hydrocarbon source rocks of the third member of the Yixian Formation entered the oil generation window at ~90 Ma, and thereafter, due to the uplift and cooling of the formation, the thermal evolution of the source rock ceased, thus remain unchanged to date.
- burial history /
- thermal history /
- apatite fission track /
- Xiushui Basin /
- southern Songliao Basin /
- oil−gas geological survey enginnering

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References

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