| 松潘黄龙水循环及钙华景观成因研究 |
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| 引用本文： | 郭建强,彭东,杨俊义.松潘黄龙水循环及钙华景观成因研究[J].四川地质学报,2002,22(1):21-26. |
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| 作者姓名： | 郭建强 彭东 杨俊义 |
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| 作者单位： | 四川省地勘局区调队,四川双流,610213 |
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| 摘 要： | 通过对松潘黄龙风景名胜区主景区黄龙寺沟运用水均衡原理和水化学系统分析，并结合天然同位表示综技术，初步查明了黄龙水循环规律，确立黄龙钙华的源泉为转花泉，其源泉来源于大气降水，并经深循环补给。进而阐明了钙华的形成与演化，建立了黄龙水循环模式，用于保护和合理开发松潘黄龙自然景观资料，使之可持续利用。
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| 关 键 词： | 同位素示踪 水循环 钙华成因 松潘黄龙 |
| 文章编号： | 1006-0995(2002)01-0021-06 |
| 修稿时间： | 2001年10月8日 |
A STUDY OF WATER CIRCULATION AND GENESIS OF TRAVERTINE LANDSCAPE IN HUANGLONG |
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| Abstract: | Water circulation regularities in the Huanglong Temple Valley as main spot of the Huanglong scenic spots are found out by means of water equilibrium principle and hydrochemical survey.Source of the Huanglong traverting is Zhuanhua Spring which is derived from meteoric water.Formation and evolution of the Huanglong travertine are expounded.A model for water circulation in Huanglong is established in order to protection and reasonable developmentof natural landcape in Huanglong. |
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| Keywords: | isotopic tracer water circulation genesis of travertine Huanglong Songpan |
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