| 浙江中生代火山--沉积地层和构造运动 |
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| 引用本文： | 包超民,王孔忠.浙江中生代火山--沉积地层和构造运动[J].地质通报,1999,18(2). |
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| 作者姓名： | 包超民 王孔忠 |
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| 作者单位： | 浙江省地质矿产厅区域地质调查队,浙江,萧山311201 |
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| 摘 要： | 燕山运动在浙江及华南各省普遍存在，对其阶段（期）的划分尚有一些分歧。近年对浙江省岩石地层单位及构造运动不整合面进行了清理，将中生代构造运动划分为５个阶段。建议把印支运动之后至白垩纪末期的地壳运动称为广义的燕山期，而把狭义的燕山运动置于白垩纪末期。
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| 关 键 词： | 构造运动 燕山期 中生代 不整合面 |
Mesozoic volcanic-sedimentary strata and tectonic movements in Zhejiang |
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| BAO Chao-min,Wang Kong-zhong.Mesozoic volcanic-sedimentary strata and tectonic movements in Zhejiang[J].Geologcal Bulletin OF China,1999,18(2). |
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| Authors: | BAO Chao-min Wang Kong-zhong |
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| Abstract: | The Yanshan movement was prevalent in Zhejiang and various provinces of South China, but there are still some divergent views about its stages. Through purification of the lithostratigraphic units and unconformities of tectonic movements, the Mesozoic tectonic movements are divided into five stages. The authors suggest that the crustal movement after the Indosinian movement till the terminal Cretaceous is called the Yanshanian tectonic stage sensus lato, while the Yanshanian movement sensus stricto is assigned to the terminal Cretaceous. The Fujian-Zhejiang movement will continue to be used. |
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| Keywords: | tectonic movement Yanshanian Mesozoic unconformity |
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