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Volume 22 Issue 3
Jun.  2011
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曹强, 叶加仁, 陆俊泽, 黄胜兵, 唐大卿. Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0187-4
Citation: 曹强, 叶加仁, 陆俊泽, 黄胜兵, 唐大卿. Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0187-4

Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China

doi: 10.1007/s12583-011-0187-4
  • Received Date: 2018-07-15
  • Rev Recd Date: 2018-07-15
  • Publish Date: 2018-07-15
  • The Yitong (伊通) basin is a Late Mesozoic and Cenozoic continental sedimentary basin in Northeast China. On the basis of well tests and seismic data, we use the 2D modeling technique to rebuild the pressure evolution and hydrocarbon migration in the Moliqing (莫里青) fault depression of the Yitong basin. Based on the modeling results, four conclusions are drawn as follows. (1) The Eocene Shuangyang (双阳) Formation within the Moliqing fault depression had entirely undergone three epi-sodic cycles of pressure accumulation and release in geological history, and the three tectonic move-ments since the Middle Eocene played important roles in the episodic changes of excess pressure. (2) The present formation pressure distribution is characterized by normal pressure in almost the entire fault depression with some residual overpressure...
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China

doi: 10.1007/s12583-011-0187-4

Abstract: The Yitong (伊通) basin is a Late Mesozoic and Cenozoic continental sedimentary basin in Northeast China. On the basis of well tests and seismic data, we use the 2D modeling technique to rebuild the pressure evolution and hydrocarbon migration in the Moliqing (莫里青) fault depression of the Yitong basin. Based on the modeling results, four conclusions are drawn as follows. (1) The Eocene Shuangyang (双阳) Formation within the Moliqing fault depression had entirely undergone three epi-sodic cycles of pressure accumulation and release in geological history, and the three tectonic move-ments since the Middle Eocene played important roles in the episodic changes of excess pressure. (2) The present formation pressure distribution is characterized by normal pressure in almost the entire fault depression with some residual overpressure...

曹强, 叶加仁, 陆俊泽, 黄胜兵, 唐大卿. Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0187-4
Citation: 曹强, 叶加仁, 陆俊泽, 黄胜兵, 唐大卿. Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression, Yitong Basin, Northeast China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0187-4

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