The data offered here favor that the collision between the Yangtze and Cathysia blocks happened in the late Proterozoic era.
现有资料支持华夏和扬子两地块在晚元古代碰撞拼合的解释。
The regional variety of development degree and horizon shows that the turbid-water with mud is from Cathysia on the east of Zhejiang-Anhui Sea Basin.
其发育程度及其层位的区域变化规律表明，泥质浑水系来自海盆东侧的 华夏 古 陆。
The regional variety of development degree and horizon shows that the turbid-water with mud is from Cathysia on the east of Zhejiang-Anhui Sea Basin.
其发育程度及其层位的区域变化规律表明，泥质浑水系来自海盆东侧的 华夏 古 陆。
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