This paper describes the halokinesis of the salt tectonics of Kucha Depression with the analysis of seismic and geological data.
以盐构造解析的方法，综合地震与地质资料分析，在盐构造成因要素剖析的基础上探讨库车坳陷盐构造动力学特征。
A model summarizing the relationships of salt tectonics, fluid flow, and hydrocarbon migration and accumulation is proposed based on it.
在此基础上文中概括了盐构造、流体流动及油气运移和聚集相互关系的模式。
The Formation of the salt tectonics in the Kuqa foreland fold belt may be controlled by compression, gravitational gliding and gravitational spreading.
库车前陆褶皱带盐构造的形成可能受挤压作用、重力滑动和重力扩展作用多重控制。
So the concepts of "salt-mud bed" and "salt mud tectonics" are proposed in this paper.
针对这一特点，提出了盐-泥层和盐-泥构造的概念。
The salt-related tectonics in the Qiangtang basin mainly formed in late Jurassic and was further patterned during Cenozoic.
羌塘盆地盐相关构造形成于侏罗纪末并在新生代进一步定型。
The salt-related tectonics in the Qiangtang basin mainly formed in late Jurassic and was further patterned during Cenozoic.
羌塘盆地盐相关构造形成于侏罗纪末并在新生代进一步定型。
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