| 黄河上游地区地质灾害分布规律与区划 |
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| 引用本文： | 张春山,张业成,马寅生,胡景江,高庆昭.黄河上游地区地质灾害分布规律与区划[J].地球学报,2003,24(2):155-160. |
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| 作者姓名： | 张春山 张业成 马寅生 胡景江 高庆昭 |
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| 作者单位： | 中国地质科学院地质力学研究所，北京100081;国土资源部实物地质资料中心，河北三河065201;中国地质科学院地质力学研究所，北京100081;国土资源部实物地质资料中心，河北三河065201;国土资源部实物地质资料中心，河北三河065201 |
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| 基金项目： | 地质大调查项目“黄河上游新构造活动与地壳稳定性研究”和科技部项目“自然灾害数据库”(979250303) |
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| 摘 要： | 黄河上游地区是中国地质灾害特别发育的地区之一。主要地质灾害有：地震、崩塌、滑坡、泥石流以及水土流失、土地沙漠化、土地盐碱化、黄土湿陷、融冻等，除了直接威胁人民生命财产安全和各种工程设施安全外，还严重破坏国土资源和生态环境，是阻碍西部大开发和可持续发展的重要因素。受地质、地貌以及气候等条件控制，各地区地质灾害发育情况有很大差异，可划分为3个地质灾害类型区：以土地沙漠化、盐碱化和地震为主的北部区；以地震、崩滑流和水土流失灾害为主的中部区和以融冻为主的西南部及西北部区，3个灾害区又可进一步划分为13个亚区。
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| 关 键 词： | 黄河上游 地质灾害 分布规律 区划 |
Distribution Regularity and Regionalization of Geological Hazards in the Upper Yellow River Valley |
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| ZHANG Chun-shan,ZHANG Ye-cheng,MA Yin-sheng,HU Jing-jiang and GAO Qing-zhao.Distribution Regularity and Regionalization of Geological Hazards in the Upper Yellow River Valley[J].Acta Geoscientia Sinica,2003,24(2):155-160. |
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| Authors: | ZHANG Chun-shan ZHANG Ye-cheng MA Yin-sheng HU Jing-jiang and GAO Qing-zhao |
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| Institution: | Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Geological Information Center, MLR, Sanhe, 065201;Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Geological Information Center, MLR, Sanhe, 065201;Geological Information Center, MLR, Sanhe, 065201 |
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| Abstract: | The region of the upper Yellow River valley is one of the areas in China where geological hazards frequently occur. The geo logical hazards mainly include earthquake,collapse,landslide,mud rock flows and soil erosion, land desertification,soil salinization, moisture sedimentation of clay and freezing melt. They not only threat the safety of people's life and all kinds of engineering but also destroy the land resources and ecological environment. They are adverse factors affecting the great exploitation and continuous deve lopment of western China. Geological hazards are different from area to area because they are controlled by such factors as geology, landform and climate. Three typical regions of geological hazards can be recognized: the northern region where there mainly exist soil desertification, soil saliniztion and earthquake; the middle region where earthquake collapse, landslide, mud rock flows and soil erosion are mainly seen; the southwestern and northwestern region where freezing melt is predominant.These regions can be further divided into 13 subregions. |
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| Keywords: | upper Yellow River valley geological harzards distribution regularity regionalization |
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