银额盆地苏红图坳陷西部中生界烃源岩热演化史恢复

祁凯; 任战利; 崔军平; 陈志鹏; 任文波

doi:10.3799/dqkx.2018.594

Volume 43 Issue 6

Jun. 2018

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Qi Kai, Ren Zhanli, Cui Junping, Chen Zhipeng, Ren Wenbo, 2018. Thermal History Reconstruction of Mesozoic Source Rocks in Western of Suhongtu Depression, Inner Mongolia, Northern China. Earth Science, 43(6): 1957-1971. doi: 10.3799/dqkx.2018.594

Citation:

Qi Kai, Ren Zhanli, Cui Junping, Chen Zhipeng, Ren Wenbo, 2018. Thermal History Reconstruction of Mesozoic Source Rocks in Western of Suhongtu Depression, Inner Mongolia, Northern China. Earth Science, 43(6): 1957-1971. doi: 10.3799/dqkx.2018.594

Citation:

Qi Kai, Ren Zhanli, Cui Junping, Chen Zhipeng, Ren Wenbo, 2018. Thermal History Reconstruction of Mesozoic Source Rocks in Western of Suhongtu Depression, Inner Mongolia, Northern China. Earth Science, 43(6): 1957-1971. doi: 10.3799/dqkx.2018.594

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Thermal History Reconstruction of Mesozoic Source Rocks in Western of Suhongtu Depression, Inner Mongolia, Northern China

doi: 10.3799/dqkx.2018.594

Qi Kai^1
,,
Ren Zhanli^{1,2
,
,},
Cui Junping^1,2,
Chen Zhipeng¹,
Ren Wenbo¹

1.
Department of Geology, Northwest University, Xi'an 710069, China
2.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China

Received Date: 2018-01-04
Publish Date: 2018-06-15

Abstract

Abstract

Suhongtu depression, located in the northeastern of Yin'e basin (Yingen-Ejinaqi basin), is a Mesozoic faulting-subsiding basin with large oil and gas resources. 75 vitrinite reflectance data from 7 wells in the study area are used to analyze the degree of thermal evolution of Mesozoic source rocks. The thermal evolution degree of source rocks in Yingen Formation is in immature to low mature stage. The vitrinite reflectance (Ro) data distribute in 0.6%-1.2% at the bottom of Suhongtu Formation, and they are generally greater than 1.1% at the bottom of Bayingebi Formation in the center of the sag. The results of Mesozoic and Cenozoic thermal history show that the present-day geothermal gradient is 34 ℃/km, and approximately 40.6-46.7 ℃/km in Late Cretaceous. The temperature gradient was 40-42 ℃/km (135-110 Ma) and increased to 46-50 ℃/km (110-103 Ma). Especially, during the deposition period of Yingen Formation (100-95 Ma), the geothermal gradient reached the maximum at about 48-53 ℃/km. From the beginning of Wulansuhai Formation, the geothermal gradient gradually increased to 40-46 ℃/km (92-80 Ma) and decreased to a present-day value of 34 ℃/km (80-0 Ma) ultimately. The higher geothermal field has played an important role in controlling oil and gas generation and accumulation since the Early Cretaceous, and the source rocks have reached the maximum thermal evolution stage at the end of the sedimentary period of the Wulansuhai Formation.
- thermal history reconstruction,
- thermal evolution of source rock,
- vitrinite reflectance,
- Mesozoic-Cenozoic,
- Yin'e basin,
- petroleum geology,
- tectonics

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References(62)

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Thermal History Reconstruction of Mesozoic Source Rocks in Western of Suhongtu Depression, Inner Mongolia, Northern China

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