These evidences prove that the Early and Middle Triassic paralic and lacustrine features had already been inactive in the Middle and Late Triassic Ordos basin.
表明中晚三叠世鄂尔多斯盆地已经结束早中三叠世近海湖泊的性质。
The Carboniferous Formation of paralic facies in the north margin of Qaidam Basin was drilled in the Gaqiu-1 Well for the first time.
在柴达木盆地北缘，尕丘1井首次钻遇了石炭系海陆交互相地层。
The Carboniferous Formation of paralic facies in the north margin of Qaidam Basin was drilled in the Gaqiu-1 Well for the first time.
在柴达木盆地北缘，尕丘1井首次钻遇了石炭系海陆交互相地层。
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