Depositional agent and biological action in the east part of the South China epicontinental sea are chiefly controlled by the land upliffting of its southeastern edge since theMaokouan Stage.
华南陆表海沉积与生物的发育深受其东南边缘茅口期以来隆起成陆的影响。
Depositional agent and biological action in the east part of the South China epicontinental sea are chiefly controlled by the land upliffting of its southeastern edge since theMaokouan Stage.
华南陆表海沉积与生物的发育深受其东南边缘茅口期以来隆起成陆的影响。
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