| 论陆内造山作用和陆内造山带 |
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| 引用本文： | 杨志华,李勇,苏生瑞,周义.论陆内造山作用和陆内造山带[J].矿物岩石,2001,21(3):169-172. |
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| 作者姓名： | 杨志华 李勇 苏生瑞 周义 |
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| 作者单位： | 长安大学地球科学学院,陕西,西安,710054 |
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| 基金项目： | 地质矿产部秦巴 ( 85 -0 1-0 18)，国家自然基金 ( 4 92 72 136 )，国家计委 ( 96 -30 -4 3)，国家科委 ( 96 -914 -0 1-0 4)等项目资助 |
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| 摘 要： | 中国大陆造山带按属性特征可以划分为三种类型和三个发展阶段，板块构造体制下的洋盆或过渡性洋盆转化造山带以后的板内沉积盆地与造山带的转化，是中国大陆岩石圈划时代的造山作用，形成最重要的造山带，那种只那造山带限制在洋盆俯冲碰撞阶段与中国造山带的实际相差甚远。
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| 关 键 词： | 大陆造山带 陆内造山作用 陆内造山带 板块构造 抽拉构造 中国 |
| 文章编号： | 1001-6872(2001)03-0169-04 |
| 修稿时间： | 2001年5月18日 |
ON THE INTRACONTINENTAL OROGENIC PROCESS AND INTRACONTINENTAL OROGENIC BELT |
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| YANG Zhi,hua,LI Yong,SU Sheng,rui,ZHOU Yi.ON THE INTRACONTINENTAL OROGENIC PROCESS AND INTRACONTINENTAL OROGENIC BELT[J].Journal of Mineralogy and Petrology,2001,21(3):169-172. |
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| Authors: | YANG Zhi hua LI Yong SU Sheng rui ZHOU Yi |
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| Abstract: | The orogenic belts in China may be classified into three types and three developing stages according to their characteristics. The transformation of sedimentary basin into orogenic belt after the transformation of oceanic basin or transitional oceanic basin into orogenic belt in plate tectonic system was the epoch making orogenic process of the continental lithosphere of China,which produced the most important orogenic belts in China. The idea that the orogenic process is limited to subduction and collision of oceanic basin is far from what has happened in the orogenic belt of China. |
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| Keywords: | Continental orogenic belt intracontinental orogenic process intracontinental orogenic belt plate tectonics drawing out tectonics China |
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