| 长江下游地区中生代构造活动与岩浆作用 |
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| 引用本文： | 翁世劼,孔庆寿.长江下游地区中生代构造活动与岩浆作用[J].地球学报,1981,3(1):1-20. |
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| 作者姓名： | 翁世劼 孔庆寿 |
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| 作者单位： | 南京地质矿产研究所;南京地质矿产研究所 |
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| 摘 要： | <正> 一、地质发育概况 长江下游地区在地质发育进程中历经了多次构造旋回,经受多期构造作用的迭加和改造。（一）前寒武纪；（二）古生代；（三）中生代。
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MESOZOIC TECTONISM AND MAGMATISM OF THE LOWER YANGTZE VALLEY |
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| WENG Shi-jie and KONG Qing-shou.MESOZOIC TECTONISM AND MAGMATISM OF THE LOWER YANGTZE VALLEY[J].Acta Geoscientia Sinica,1981,3(1):1-20. |
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| Authors: | WENG Shi-jie and KONG Qing-shou |
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| Institution: | Nanjing Institute of Geology and Mineral Resources, Chinese Academy ot Geological Sciences;Nanjing Institute of Geology and Mineral Resources, Chinese Academy ot Geological Sciences |
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| Abstract: | Based on the regional paleogeography, tectonic history and magmaticactivity, this paper deals with the Mesozoic tectonism and magmatism of thelower Yangtze Valley, and also discusses the relation between the mechanismand evolution of continental volcanism. After the beginning of Mesozoic time, the platform block of the lowerYangtze Valley was disintegrated. Under the influence of the northwardmovement of the Pacific Plate, a series of left-lateral deep faults were formed in the eastern part of Chinese continent. |
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