The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.
“盆地”构造发
模式为:从晚侏罗世到白垩纪末期发
山间“盆地”开始、发展到早第三纪

盆
发
、
化为晚第三纪及第四纪地
发
阶段。
观点;若发现问题,欢迎向我们指正。


