Oil & Gas Geology ›› 1988, Vol. 9 ›› Issue (4): 356-362.doi: 10.11743/ogg19880407

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HIGH-CONDUCT ORIGIN AND ENVIRONMENT OF THE HIGH CONDUCTIVE MUDSTONES IN DAINAN FORMATION,GAOYOU DEPRESSION

Xue Liangqing   

  1. Scientific Research Institute of Petroleum Exploration and Development, Beijing
  • Received:1987-06-26 Online:1988-12-25 Published:2012-01-16

Abstract:

The high conductivity of high conductive mudstone is mainly caused by sali-nity difference, and has less relation with the chemical composition and claymineral of mudstones.The deposition of the mudstone is not a simpleprocess of the lake enlargement, but a process of enlarging-contracting andreenlarg-recontracting.In the meantime, the depth of water and the nature ofmediums were changed correspondingly.This shows the control actions of ancientclimate and direct runoff under the stable structural background.