[1]李俊,刘金峰,莫多闻.河北平原地裂缝的分布规律及成因初探[J].水土保持研究,2003,10(03):62-65,116.
　LI Jun,LIU Jin-feng,MO Duo-wen.Distribution and Origin of the Rifts in Hebei Plain[J].Research of Soil and Water Conservation,2003,10(03):62-65,116.
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河北平原地裂缝的分布规律及成因初探

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 10 期数: 2003年03期 页码: 62-65,116 栏目: 出版日期: 1900-01-01
Title:
Distribution and Origin of the Rifts in Hebei Plain
作者:
李俊1, 刘金峰2, 莫多闻1
1. 北京大学环境学院, 北京, 100871;
2. 河北地质学院, 石家庄, 050031
Author(s):
LI Jun1, LIU Jin-feng2, MO Duo-wen1
1. College of Environmental Sciences, Peking University, Beijing, 100871, China;
2. Hebei University of Geology, Shijiazhuang, 050031, China
关键词:
地裂缝; 构造运动; 地震; 地下水动态
Keywords:
rift; tectonic movement; earthquake; groundwater regime
分类号:
P694
摘要:
以丰富的资料,阐述了河北平原地裂缝的发展现状、形态特征、时空分布规律.通过分析地裂缝与地形地貌、土体岩性、降水、地表水、地下水动态、构造运动的关系,初步揭示了地裂缝的成因是以构造运动、地震为主导因素,水的活动为诱发因素,地形地貌、土体岩性为影响因素.
Abstract:
The morphological characteristics and space time distribution of the rifts in the Hebei Plain were discussed.The relations between the rifts and the landforms,lithology,precipitation,surface water,groundwater regime,earthquake,and tectonic movement were analyzed.It can be found that the tectonic movement and earthquake is the controlling factor,the water’s movement is the inducing factor,the land form and lithology have also played an influencing role in the development of the rift.

参考文献/References:

[1] 王景明.地裂缝与其灾害的理论与应用[M].西安:陕西科学技术出版社,2000.112-119.
[2] 刘金峰.任丘地区井孔注水和地震活动与地裂缝关系[J].河北地质学院学报,1995,18(6):574.
[3] 河北省环境地质图说明书,河北省环境水文地质总站(1990).

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备注/Memo

收稿日期:2003-4-25。
基金项目:国家自然科学基金(批准号:40271013);教育部高等学校博士学科点专项科研基金(批准号:99000149)资助.
作者简介:李俊(1979- ),女,硕士生,地貌与第四纪地质学专业.

更新日期/Last Update: 1900-01-01