岩溶石灰华
又称钙华。在地表由岩溶水沉积的大孔隙性次生碳酸钙。其成因是由于岩溶地区的地下水或地表水，在适宜的环境下，且往往在水动力和植物作用影响下，导致碳酸盐过饱和沉积而成。如贵州茂兰自然保护区小七孔小河沿线的大量石灰华。
90
Alias
Contributor
contributed at 2011-10-12
Classification(s)
●
Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | karst calcareous tufa |
| Chinese |
|---|
| Name | 岩溶石灰华 |
| Description | 又称钙华。在地表由岩溶水沉积的大孔隙性次生碳酸钙。其成因是由于岩溶地区的地下水或地表水，在适宜的环境下，且往往在水动力和植物作用影响下，导致碳酸盐过饱和沉积而成。如贵州茂兰自然保护区小七孔小河沿线的大量石灰华。 |
How to Cite
NNU_Group (2011). 岩溶石灰华, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/e3dff2c8-5227-4f42-ad3e-329b32c8f898
Copy
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
