The main reservoir spaces in Archean are mainly tensional,steeply dipped fractures oriented in NE and NW directions and micro-cracks formed in the middle or the Late Mesozoic.

 
  • 茨榆坨潛山儲集空間主要是裂縫和微裂隙,太古界儲層主要發(fā)育北東向和北西向兩組裂縫,以高角度張性裂縫為主,形成于中生代中、晚期;
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