In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.
在中国东部早第三纪沉积演化过程中曾周期性地发生过侵,从而形成了具有特征的岩类型、古生。
In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.
在中国东部早第三纪沉积演化过程中曾周期性地发生过侵,从而形成了具有特征的岩类型、古生。
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