摘要
黄龙景区因拥有钙华源泉、彩池、滩流、瀑布等景观而享誉世界,其钙华景观的稳定性也为世人所关注。文章通过对与钙华景观形成密切相关的地质环境,特别是水循环系统动态变化及区域钙华景观成长演化历史的研究,认为黄龙钙华景观现状稳定性较好,但正处于缓慢的、反复的衰退过程,只要采取适当的措施可以延缓其衰退。
The Huanglong scenic spot is world-famous, which includes travertine source spring, colored ponds, sinter flow beaches and waterfalls, etc. The stability of the travertine landscape attracts more and more attention. An investigation of geo-environment related to the formation of the travertine landscape, especially the dynamic changes in water circulation system and the development of the landscape was carried out. The results indicate that the Huangl reoccurring ong travertine landscape is stable at present, but it is in its gradual decline stage and this decline is a procedure. The decline could be controlled if propert protection measures are taken.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
2008年第1期107-111,116,共6页
Hydrogeology & Engineering Geology
基金
四川省发展和改革委员会([2004]161号)资助
关键词
黄龙
钙华景观
演化趋势
衰退
Huanglong
travertine landscape
evolution trend
decline
