向压性 meaning in Chinese

barotaxis
barotropism

The ne - strike compressional faults are not intersected with the ew ma in fault zone , but a kind of transform structure resulted from its right lateral strike slip , and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning
在青龙断裂带两侧，分布有许多北东向压性断层，它们与东西向主断裂带不是简单的切割关系，而是东西向主断裂带右行走滑活动中的分支断裂，位于青龙断裂带北东侧的辽西地区中生代逆冲推覆构造，也是青龙断裂带在右行走滑作用下，因构造方向的改变发生构造转换的结果。
Nw compressive structures are developed in indosinian epoch in which folds are predominant and companied with some small thrusts . nearly ns or nnw compressive structures are developed at the end of yanshan epoch in which it is mainly overthrusted structures and closed folded structures . large gentle anticlines and synclines are developed from the end of mesozoic to early tertiary , and antithetic sagging structures are developed in mesozoic
研究发现，本区印支期发育了以褶皱为主、局部伴有小型逆断层的北西向压性构造，燕山末期(中生代末期)发育了以逆掩构造和紧闭的褶皱构造为主的近南北向或北北西向压性构造，中生代末到第三纪早期发育了以宽缓为特征的大型背斜向斜构造，以及中生界内部的逆牵引构造。