Volume 38 Issue 3
May  2013
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Article Navigation >  Earth Science  > 2013  >  38(3): 553-560
ZUO Yin-hui, MA Wei-min, DENG Yi-xun, HAO Qing-qing, LI Xin-jun, GUO Jun-mei, RAN Qing, WANG Li-rong, 2013. Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia. Earth Science, 38(3): 553-560. doi: 10.3799/dqkx.2013.055
Citation: ZUO Yin-hui, MA Wei-min, DENG Yi-xun, HAO Qing-qing, LI Xin-jun, GUO Jun-mei, RAN Qing, WANG Li-rong, 2013. Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia. Earth Science, 38(3): 553-560. doi: 10.3799/dqkx.2013.055
shu

Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia

doi: 10.3799/dqkx.2013.055
  • 1.

    Research Institute of Exploration and Development, Zhongyuan Oilfield, SINOPEC, Puyang 457001, China

  • 2.

    State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China

  • 3.

    School of Energy Resources, China University of Geosciences, Beijing 100083, China

  • 4.

    Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 100025, China

  • 5.

    Geophysical Logging Company, Zhongyuan Oilfield, SINOPEC, Puyang 457001, China

  • Received Date: 2012-02-02
  • Publish Date: 2013-05-15
    Abstract
  • The Chagan sag has the greatest potential for oil and gas exploration among other sags in the Yin'gen-Ejinaqi basin. To reveal the Mesozoic and Cenozoic thermal history and source rock thermal evolution history in the Chagan sag, the thermal history was modeled on basis of vitrinite reflectance data of 9 wells. The modeled results show the thermal gradients increased gradually from the Early Cretaceous Bayin'gebi Formation to the end of the Yin'gen Formation, and the thermal gradients reached maximum values(50-58 ℃/km) at the end of the Yingen Formation.Then the thermal gradients decreased gradually from the Late Cretaceous Wulansuhai Formation to the present day, and the thermal gradients is only 31-34 ℃/km in the present day. Meanwhile, based on the above thermal gradient data, with combination of the depositional and tectonic development history and geochemical parameters of source rocks, maturation histories of 3 sets of source rocks of 9 wells were modeled. The modeled results show the maturation histories were controlled by the palaeogeothermal, and the maturation of 3 sets of source rocks reached maximum values in the late period of the Early Cretaceous.

     

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