三叠纪末的印支运动结束了柴达木地块及其周缘地区的海相沉积史，使柴达木地区进入陆内盆地发育新时期。
At the end of Triassic period, the Marine sedimentation on Qaidam Massif (including its surroundings) has ended, and interior basin started to develop in Qaidam area.
柴达木盆地石炭系主要分布在柴东地区，是该盆地勘探和研究程度较低的层系之一。
It is one of the stratums which are lower degree of exploration and research in the Qaidam basin.
柴达木盆地阿尔金斜坡中段，是寻找隐蔽油气藏的有利地区之一。
The medium section of Altun slope in Qaidam basin is one of the favourable areas in the exploration of subtle petroleum reservoirs.
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