中文摘要：

有在在盐 tectonics 和烃之间的盐层，盐 tectonics，和关系的开发的波斯湾盆的比较 Kuqa 低岬盆，盐挤入构造相对烃，这被结束。在 Kuqa 低岬盆寻找盐挤入构造和相关陷井是重要的。在 Kuqa 低岬盆构造的盐的形成的机制与 Hormuz 系列的不同，但是类似于更低的 Fars Series/Gachsaran 的形成。在烃累积由更低的 Fars Series/Gachsaran 形成的盐 tectonics 的角色启发了，作者认为在盐层下面的探索应该被强制，并且下面的陷井在在盐层更厚的地方，低岬盆将被发现的 Kuqa 的南部的部分腌层。相反，陷井应该在盐层是薄的北山前面在上面并且在盐层下面被发现。三叠纪并且侏罗记来源岩石富于有大探索的这个区域未来。

英文摘要：

Compared Kuqa foreland basin with Persian Gulf Basin in development of salt layers, salt tectonics, and the relation between salt tectonics and hydrocarbon, it is concluded that the salt diapirs are relative to hydrocarbon. Searching salt diapirs and related traps in Kuqa foreland basin is important. The forming mechanism of salt tectonic in Kuqa foreland basin is different from that of Hormuz Series, but similar to that of Lower Fars Series/Gachsaran Formation. Inspired by the role of salt tectonics of Lower Fars Series/Gaehsaran Formation in hydrocarbon accumulation, the authors considered that the exploration below salt layer should be enforced, and the traps below salt layer in the southern part of the Kuqa foreland basin would be found where salt layer is thicker. On the contrary, the traps should be found both above and below the salt layer in front of the northern mountain where salt layer is thin. The Triassic and Jurassic source rocks are rich in this area with great exploration prospective.