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 north margin of Qaidam basin is a significant tectonic-magmatic activation belt and an endogenic metallogenic province. Its recent architectonic property is a geodome series.
柴达木盆地北缘是重要的构造-岩浆活化带和内生矿产成矿带，现今大地构造性质属地穹列。
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