| 贵州的多级剥夷面 |
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| 引用本文： | 秦守荣,张慧,王天华.贵州的多级剥夷面[J].贵州地质,2002,19(2):86-92. |
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| 作者姓名： | 秦守荣 张慧 王天华 |
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| 作者单位： | 贵州省地质调查院,贵州,贵阳,550005 |
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| 基金项目： | 1 :2 5万安顺幅区调 (修测 )项目成果 项目编号 2 0 0 113 0 0 0 0 68。 |
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| 摘 要： | 简要论述剥胰面的基本概念及工作方法。以图切地质地貌剖面为基础，结合区域地质地貌特征，划分了贵州区域性多级剥夷面及地文期。认定贵州新构造运动的主要形式是间歇性持续上升，总体西高东低的地势为历次溯源侵蚀夷平范围渐次缩小而成。
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| 关 键 词： | 剥夷面 贵州 新构造运动 地文期 识别 划分 |
| 文章编号： | 1000-5943(2002)02-0086-07 |
| 修稿时间： | 2002年2月7日 |
Multi-grade Planation Surface of Denudation in Guizhou |
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| QIN Shou-rong,ZHANG Hui,WANG Tian-hua.Multi-grade Planation Surface of Denudation in Guizhou[J].Guizhou Geology,2002,19(2):86-92. |
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| Authors: | QIN Shou-rong ZHANG Hui WANG Tian-hua |
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| Abstract: | This paper generalizes the basic concept and the work process on the planation surface of denudation, and classifies the muti-grade planation surface of denudation and physiographic stage of Guizhou in light of the profile of geomorphy and the feature of regional geomorphy. The major process of neotectonic movement of Guizhou is continuous lift in interval, and the whole topography of high west and low east has developed in all previous gradual range-reduction of retrogressive planation surface of denudation. |
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| Keywords: | multi-grade planation surface of denudation Guizhou |
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