摘要
根据遥感影像信息特征,湘西北地区有向、向和近向类新构造2000.TMNEENNESN3带,各新构造带岩溶发育阶段,分别相当于中年期、青年期和幼年期。岩溶发育各阶段表现出不同的岩溶地貌、流水地貌和岩溶水文地质特征,反映了新构造运动由强烈活动→趋向稳定平静的过程。
Based on features of the newest remote sensing image, there are 3 sets of neotectonics zones in Westnorthern Hunan, i.e. NEE strike, NNE strike and SN strike, the karst development stages in the each neotectonics zone match respectively with the middle-aged period, young-aged period and chidhood-aged period. Every stage of karst growth shows the difference characteristics of karst geomorphology, running water geomorphology and kart hydrogeology, they reflect the process of neotectonics movement from strong action to near stablilty.
出处
《湖南地质》
2001年第3期225-229,共5页
Hunan Geology
基金
"西南岩溶石山地区地下水资源勘查与生态环境地质调查"项目的部分成果。
