开特米里克矿区雅丹地貌形成演化模式及形态差异研究
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成都理工大学地质灾害防治与地质环境保护国家重点实验室

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P54

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Study on Open Terme Rick Mine Landform Evolution Model and Morphological Differences
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    摘要:

    雅丹源于维吾尔语,即风蚀槽谷,主要是风的吹蚀作用结合磨蚀作用的产物。青海省开特米里克矿区雅丹地貌位于柴达木盆地西部,形成物质主要为湖相沉积物,形成原因属于以风的吹蚀作用为主的雅丹地貌类型。另外,气候的干旱、多风以及风化作用强烈为雅丹地貌的形成提供了有利条件。本文分析了开特米里克矿区雅丹体的分布规律及形态特征,以及论证了其形成条件,阐明了该矿区雅丹地貌的形成原因及演化模式。在实测的基础上,运用最小二乘法原理,验证了矿区东北部与西南部雅丹地貌形态参数长与宽的强相关性,拟合出长宽比R,并合理地分析了其形态差异的原因。

    Abstract:

    Yardangs from Uighur, namely wind troughs, the main role of wind erosion is combined with abrasive products. Qinghai open Terme Rick mining landform located in western Qaidam Basin, forming substance is mainly lacustrine sediments, which of the causes belong to the role of wind erosion. What’s more, climate dry, windy and strong weathering provided favorable conditions for the forming of yardangs. This paper analyzed the open Terme Rick mines Yardangs distribution and morphological characteristics, demonstrated its forming conditions, stating the reasons for the formation and mining landform evolution model, at last ,verified the northeast and southwest mining landform morphological parameters (the length and the width of a strong correlation between the fitting out of the aspect ratio R) On the basis of the measured by least square fitting, having a reasonable analysis of the reasons for its morphological differences.

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魏恺泓. 开特米里克矿区雅丹地貌形成演化模式及形态差异研究[J]. 科学技术与工程, 2013, 13(33): .
Wei Kai-hong. Study on Open Terme Rick Mine Landform Evolution Model and Morphological Differences[J]. Science Technology and Engineering,2013,13(33).

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  • 收稿日期:2013-05-31
  • 最后修改日期:2013-07-10
  • 录用日期:2013-07-26
  • 在线发布日期: 2013-10-22
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