构造运动 tectogenesis
- 两期构造运动叠加造成了车尔臣断裂系现今的构造样式。
The two period geologic movements lead to the modern Cheerchen fracture system structural patterns. - 黑孜尔断裂现今活动方式继承了新构造运动以来的运动特点。
The present motion mode of Heizir fault inherits the characteristic of new tectonic motion. - 上新世晚期的构造运动破坏了早期形成的油藏,在喀什凹陷北部地表形成油砂。
Early oil reservoir had been destroyed by the tectogencsis in Later Plioccne, and forming oilsand on the surface occurrence in northern Kashi sag.
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