| 华夏古陆晚前寒武纪的活动痕迹 |
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| 引用本文： | 邓家瑞,张志平.华夏古陆晚前寒武纪的活动痕迹[J].地质调查与研究,1998,21(2):1. |
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| 作者姓名： | 邓家瑞 张志平 |
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| 作者单位： | 华东地质学院!江西临川，344000，华东地质学院!江西临川，344000 |
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| 摘 要： | 通过对前寒武纪建造、构造的综合分析研究认为：中元古代晚期浙西-赣东北地区是华夏古陆的活动陆缘；武陵运动是华南一次最重要的造山运动，华夏古陆与扬子地块沿赣东北断裂带发生碰撞，形成了统一的“华南古大陆”。
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| 关 键 词： | 活动陆缘 晚前寒武纪 华夏古陆 |
| 修稿时间： | 1998－03－20 |
THE ACTIVE TRACE OF LATE PRECAMBRIAN IN CATHAYSIA |
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| Deng Jiarui,Zhang Zhipin.THE ACTIVE TRACE OF LATE PRECAMBRIAN IN CATHAYSIA[J].Geological Survey and Research,1998,21(2):1. |
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| Authors: | Deng Jiarui Zhang Zhipin |
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| Abstract: | Through comprehensive analysis and studies on the Precambrian formations and Structures, it is suggested the western Zhejiang-Northeastern Jiangxi region was just the activeContiental margin of the Cathaysia during the late stage of middle Proterozoic. Wuling movement Is the most important orogengy in southern China, which lead to the collision of cathaysia with Yangtze block along the northeastern jiangxi fault belt, resulting in the formation of the united South China old land. |
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| Keywords: | active continental margin Precambrian cathaysis |
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