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茂县牟托泉群水文地质条件及成因分析
引用本文:陈盟,吴勇,高东东.茂县牟托泉群水文地质条件及成因分析[J].地下水,2011(6):104-105,121.
作者姓名:陈盟  吴勇  高东东
作者单位:成都理工大学地质灾害防治与地质环境保护国家专业实验室
基金项目:地质灾害防治与地质环境保护国家重点实验室自主研究课题(SKLGP2009Z006)
摘    要:牟托村位于茂县最南端,是山间河谷阶地地貌、洪积扇地貌及泥石流侵蚀地貌综合作用而成,分布有带状泉群,通过水文地质调查工作,结合Piper图和指印图探讨分析了该泉的成因,认为该泉是一个受多向补给的下降泉.泉水的补给来源是牟托沟上游的补给和基岩裂隙水及孔隙水的侧向补给.

关 键 词:牟托  泉群  水文地质条件  Piper图  指印图

Analysis on Hydrogeological Condition & Its Forming Causes of the Moutuo Springs Area
CHEN Meng,WU Yong,Gao Dong-dong.Analysis on Hydrogeological Condition & Its Forming Causes of the Moutuo Springs Area[J].Groundwater,2011(6):104-105,121.
Authors:CHEN Meng  WU Yong  Gao Dong-dong
Institution:(National Professional Laboratory of geological disaster prevention and of Environmental protection,Chengdu university of technology Chengdu 610059,Sichuan)
Abstract:Moutuo village is located in the southern most part of Mao County,It is synthetically aroused by intermountain valley landform,alluvial fan landform and debris flow erosion landform zonal springs are found in the zone,combined with hydrogeological survey,we explored the causes of the springs with Piper Map and Fingerprint Map,then we found that this is a gravity springs by multiway recharge of upstream of Moutuo ditch and lateral supply of bedrock fissure water and pore water.
Keywords:Moutuo Springs  Hydrogeological condition  Piper Map and  Fingerprint Map
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