| 陶湾群的变形特征 |
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| 引用本文： | 胡健民,张维吉. 陶湾群的变形特征[J]. 地球科学与环境学报, 1988, 0(2) |
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| 作者姓名： | 胡健民 张维吉 |
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| 摘 要： | 石门断裂到铁炉子断裂之间的广大区域是华北地台与秦岭褶皱造山带的过渡带,陶湾群分布于该带近造山带一侧的最前缘。特殊的构造环境决定了陶湾群的构造变形史是以推覆构造与平卧褶皱组合十分发育为特点。这种构造环境也是导致陶湾群变形较之其北侧寒武系及元古宇变形更为复杂的根本原因。
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| 关 键 词： | 陶湾群 构造变形 秦岭褶皱造山带 |
DEFORMATIONAI FEATURES OF THE TAOWAN GROUP |
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| Hu Jianmin Zhang Weiji. DEFORMATIONAI FEATURES OF THE TAOWAN GROUP[J]. Journal of Earth Sciences and Environment, 1988, 0(2) |
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| Authors: | Hu Jianmin Zhang Weiji |
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| Affiliation: | Xi'an College of Geology |
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| Abstract: | The region between the Shimen Fault and the Tieluzi Fault is a transitional belt of the north China Platform and the Qinling Oroginic Belt. The Taowan Group is distributed along the forest margin of this transitional belt. It is the tectonic environment that determines the deformational features of the Taowan Group. The tectonic history of this area is characterized by a combination of thrust structures and recumbent folds.For this reason the Taowa Group has many more complex deforational features that of the nearly Cambrian and Proterozoic rocks. |
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