| 试论陆内型造山作用──以秦岭-大别山造山带为例 |
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| 引用本文： | 赵宗溥. 试论陆内型造山作用──以秦岭-大别山造山带为例[J]. 地质科学, 1995, 0(1): 19 |
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| 作者姓名： | 赵宗溥 |
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| 作者单位： | 中国科学院地质研究所 |
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| 摘 要： | 板块构造学说的大陆碰撞作用和槽台学说的地槽回返作用不能解释秦岭-大别山造山带的成因机制。壳幔拆离构造导致陆内A型俯冲是陆内型造山作用的成因机制。
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| 关 键 词： | 秦岭-大别山造山带 大陆碰撞造山带 陆内A型俯冲-壳幔拆离构造 陆内型造山作用 |
| 修稿时间： | 1994-03-22; |
AN INTRACONTINENTAL-TYPE OROGENY──Evidence from Qinling-Dabie Orogenic Belt,China |
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| Zhao Zongpu. AN INTRACONTINENTAL-TYPE OROGENY──Evidence from Qinling-Dabie Orogenic Belt,China[J]. Chinese Journal of Geology, 1995, 0(1): 19 |
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| Authors: | Zhao Zongpu |
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| Affiliation: | Istitute of Geology, Chinese Academy of Sciences, Beijing, 100029 |
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| Abstract: | his paper mainly demonstrates that the causal mechanism of Qinling-Dabie Orogenic Belt could not be explained both by continental collision of plate-tectonics theory and by geosyncline inversion of the geosyncline-platfrom theory. Moreover,the author proposes that the crust-mantle detachment lead to the A-type subdution can interprete the causal mechanism of the Qinling-Dabie Orogenic Belt. |
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| Keywords: | Qinling-Dabie Orogenic Belt Continental Collision A-type subduction Crustal-mantle detachment Intracontinental-type Orogeny |
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