| 新疆阿合奇地区木兹杜克过渡带的薄皮构造 |
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| 引用本文： | 张新勇. 新疆阿合奇地区木兹杜克过渡带的薄皮构造[J]. 地质与勘探, 2014, 50(Z1): 1308-1313 |
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| 作者姓名： | 张新勇 |
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| 作者单位： | 长安大学地球科学与资源学院，陕西西安； 中国人民武装警察部队黄金第七支队，山东烟台 |
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| 基金项目： | 中国地质调查局地质调查项目（编号：1212011120495；编号：1212011220661）资助 |
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| 摘 要： | 新疆阿合奇地区木兹杜克过渡带位于塔里木西北边缘的柯坪前陆盆地，是典型的薄皮构造，其主滑脱面为寒武纪阿瓦塔格组膏泥层，盖层变形强烈。该薄皮构造带是长期、多期、至今仍在活动的产物，受区域构造影响，木兹杜克过渡带的变形由北向南发展，盖层中存在不整合面和多个次级滑脱面，具有横向分带垂向分层的特点。
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| 关 键 词： | 木兹杜克过渡带?? 薄皮构造? ?新疆阿合奇 |
| 收稿时间： | 2014-03-28 |
| 修稿时间： | 2014-09-16 |
Thin-skinned structure in the Muziduke transition zone of the Aheqi region, Xinjiang |
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| Zhang Xin-yong. Thin-skinned structure in the Muziduke transition zone of the Aheqi region, Xinjiang[J]. Geology and Prospecting, 2014, 50(Z1): 1308-1313 |
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| Authors: | Zhang Xin-yong |
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| Affiliation: | School of Earth Sciences and Resources, Chang'an University, Xi'an, Shanxi; The 7th Gold Detachment of Chinese Armed Police Force, Yantai, Shandong |
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| Abstract: | The Muziduke transition zone is located in the Keping foreland basin, northwestern margin of Tarim, Xinjiang. It is a typical thin-skinned structure with the primary detachment plane composed of paste mud in Cambrian Awatage Formation and strong deformation in the cover. This thin-skinned structure belt is the product of the long-term and multi-phase tectonic movement that is still ongoing at present. Affected by the regional tectonics, the deformation in the Muziduke transition zone has spread from north to south. Unconformity and multiple secondary detachment planes exist in the cover, which exhibit characteristics of lateral zonation and vertical layering. |
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