The giant central gas field in E′erduosi Basin is a stratigraphic gas reservoirs developed in the ancient weathered crust of carbonate rocks on the top of the Ordovician.
鄂尔多斯盆地中部大气田是发育在奥陶系顶碳酸盐岩古风化壳中的地层油气藏。
There are observation evidences for the E-W trend suture as following: (1) an ophiolitic melange belt resulted from subducted and overthrusted residual oceanic crust;
这条东西延伸的缝合带的证据是：1。残留洋壳经消减、冲断形成的蛇绿混杂带；
There are observation evidences for the E-W trend suture as following: (1) an ophiolitic melange belt resulted from subducted and overthrusted residual oceanic crust;
这条东西延伸的缝合带的证据是：1。残留洋壳经消减、冲断形成的蛇绿混杂带；
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