华南(研究区)由杨子地块东南部和华夏地块组成。
South China (studying area) is composed of the Cathaysian block and the southeastern part of Yangtze block.
近期一些文献中的华夏地块的内涵已经不是原来的华夏古陆。
Some intension of the term Cathaysian block in the recent magazines is not that of the original Cathaysian old land.
江西萍乡地区位于扬子地块和华夏地块两大构造单元对接带的西段。
Pingxiang area Jiangxi Province is in the western part of the junction between Yangzi and Huaxia Block.
该裂碰带是在新晚元古代以后，华夏地块发生裂解、闭合过程中形成的，是使本区前寒武系地层产生变质、混合岩化和花岗岩化的主导因素。
This splitting and collision zone is formed in the Process of splitting and closing of Huaxia massif 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 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 data offered here favor that the collision between the Yangtze and Cathysia blocks happened in the late Proterozoic era.
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