| 中国和哈萨克斯坦阿尔泰大地构造及地壳演化 |
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| 引用本文： | 李天德,В.Н.波里扬斯基.中国和哈萨克斯坦阿尔泰大地构造及地壳演化[J].新疆地质,2001,19(1):27-32. |
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| 作者姓名： | 李天德 В.Н.波里扬斯基 |
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| 作者单位： | 1. 新疆维吾尔自治区地质矿产勘查开发局地质矿产研究所,
2. 哈萨克斯坦科学院地质研究所阿尔泰分部, |
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| 基金项目： | 国家305项目（8590206）资助 |
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| 摘 要： | 中国和哈萨克斯坦阿尔泰位于西伯利亚板块西南边缘，阿尔泰褶皱系与斋桑－北准噶尔褶皱系的接合部位，分为霍尔宗－丘伊－哈纳斯、冲乎尔－青河、别洛乌巴－南阿尔泰、矿区阿尔泰和东卡尔巴－富蕴、二台6个构造建造带，14个构造建造亚带。区内地壳演化可分为太古宙－元古宙古陆壳形成阶段、早古生代被动陆缘壳壳增生阶段、晚古生代陆壳拉张破坏和挤压重建（增生）阶段及中－新生代相对稳定的大陆发展阶段。
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| 关 键 词： | 阿尔泰褶皱系 大地构造 地壳演化 中国 哈萨克斯坦 有色金属成矿带 构造建造带 |
| 文章编号： | 1000-8845(2001)01-027-06 |
| 修稿时间： | 2000年11月8日 |
TECTONICS AND CRUSTAL
EVOLUTION OF ALTAI IN CHINA AND KAZAKHSTAN |
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| LI Tian-de,B.H.Poliyangsiji.TECTONICS AND CRUSTAL
EVOLUTION OF ALTAI IN CHINA AND KAZAKHSTAN[J].Xinjiang Geology,2001,19(1):27-32. |
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| Authors: | LI Tian-de BHPoliyangsiji |
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| Institution: | LI Tian-de1,B.H.Poliyangsiji 2 |
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| Abstract: | Altai in China and Kazakhstan is located at the southwestern margin of Siberia plate, where Altai fold system and Zhaisang-North Jungger fold system join together. The tectonic units are divided as follows, the 1st grade units for fold region, the sub-1st grade units for fold system, the 2nd grade units for tectono-formation belt which roughly corresponds with fold belt, central uplift belt or central crystalline belt or simply-called belt. The 3rd grade units roughly correspond with anticlinoria, synclinoria, combination of above two, and faulted blocks. These are simlpy called sub-belts. Four tectono-formation sub-belts are divided in the area. The tectonic framework of the area formed through repeated extensions and compressions. Four key stages are divided, i.e., Archean-Proterozoic formation of paleo-continental crust, Early Paleozoic accretion of passive continental margin, Late Paleozoic extension-compression of continental crust, and Meso-Cenozoic relatively stable development. |
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| Keywords: | Altai of Sino-Kazakhstan geotectonics Altai fold system Zhaisang-North Jungger fold system tectono-formation belt Archean-Proterozoic Early Paleozoic Late Paleozoic |
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