Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.
白音查干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底
生代发育起来的断-坳型
谷盆地的次级构造单元。
Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.
白音查干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底生代发育起来的断-坳型谷盆地的次级构造单元。
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