Compressive tectonic stress is the main stress in foreland basins in western China, where surface and subsurface structures are very complicated.
中国西部前陆盆地主要以挤压构造应力为主，地表与地下构造异常复杂。
The Mid-Late Jurassic semi-foreland basin formation and Early Yanshan compressive deformation stage;
中晚侏罗世类前陆盆地的形成和早燕山期挤压变形阶段；
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