山西太原盆地是我国北方典型的大型新生代断陷盆地。
Taiyuan basin is a representative large-scale Cenozoic rift basin in Shanxi Province, northern China.
以一系列断陷盆地为主体的断陷盆地带是山西的地震构造带和未来地震的主要危险区。
The belt which a series of faulted basins are main body is the seismotectonic belt and the main risk region of the future earthquakes in Shanxi.
这些特点不同于山西断陷带其它诸盆地局部小区域应力场的特点。
These features are different from the features of the locally small regional stress fields of other basins in Shanxi rift zone.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
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