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
育模式
:
侏罗世到白垩纪末
育的山间“盆地”开
、
到早第三纪断陷湖盆的
育、再演化
第三纪及第四纪地陷
育阶段。


微观图像


