basin karst

基本解釋

The Wenshan basin is karst faulted basin, the main rock is carbonate, clay and clastic.
文山盆地屬于巖溶斷陷盆地，研究區(qū)基巖主要為碳酸鹽巖、粘土巖與碎屑巖。
In Guanghua basin karst collapse is mainly due to excessively pumping groundwater, mining or heavy rains;
巖溶塌陷主要是由于過量抽取地下水或礦山疏干排水、地下采空、暴雨觸發(fā)；
There are two systems in Guanzhong basin, karst thermal water system on the north of Wei river faults and large deep faults thermal water system on the south of Wei river faults.
其中渭河以南地熱系統又分為盆地中部“凈熱水”亞系統與秦嶺山前混合熱水亞系統。