Volume 31 Issue 3
May  2006
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DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.
Citation: DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.

Distribution and Tectonic Background of Various Energy Resources in Ordos Basin

  • Publish Date: 2006-05-25
  • The formation process of the various energy resources coexisting system and its regional tectonic background in Ordos basin are analyzed by introducing the "metallogenic system" theory in this paper. The Mesozoic is the important transition period of the regional tectonic regime, during which the orogeny is outstanding around the basin and three rectothermal events took place in the basin. The transition of the tectonic regime induces the occurrence of various accumulating processes of the inorganic and organic fluids, for example, the organic fluid in the basin is activated by the recto-thermal events and the inorganic fluid flowing towards the basin is produced due to the orogeny. The reciprocity between the inorganic and organic fluids happens during their transporting. The existence of the organic fluid produces the redox barrier, which causes the mutation of the physicochemical parameters of the inorganic fluid and the precipitation of the uranium element at the interface. The mutation and interface effects are obvious in the formation of the various energy resources.

     

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