Abnormal high pressure is found from Neogene to Jurassic in Leughu-Nanbaxian strnctural belt in the northern margin of Qaidam basin, and mostly occurs in undercompaction shale.

 
  • 摘要柴北缘冷湖-南八仙构造带从新近系到侏罗系普遍存在异常高压,且通常发育在欠压实泥岩中。
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