The area had undergone such evolution stages as passive borderland basining, squeerze-retrograde nose-like swelling, cratonic inner sagging. intracratonic basining and para-foreland basin.
克拉通内凹;克拉通内坳盆地发展和类前陆盆地发展。
The area had undergone such evolution stages as passive borderland basining, squeerze-retrograde nose-like swelling, cratonic inner sagging. intracratonic basining and para-foreland basin.
克拉通内凹;克拉通内坳盆地发展和类前陆盆地发展。
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