Oil & Gas Geology ›› 1988, Vol. 9 ›› Issue (4): 356-362.doi: 10.11743/ogg19880407
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Xue Liangqing
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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.
Xue Liangqing. HIGH-CONDUCT ORIGIN AND ENVIRONMENT OF THE HIGH CONDUCTIVE MUDSTONES IN DAINAN FORMATION,GAOYOU DEPRESSION[J]. Oil & Gas Geology, 1988, 9(4): 356-362.
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URL: http://ogg.pepris.com/EN/10.11743/ogg19880407
http://ogg.pepris.com/EN/Y1988/V9/I4/356