摘要
寿阳盆地比西部的太原盆地高276m,有″山顶之盆″之称,因地势较高,气候寒冷,又有″冷寿阳″之称。该盆地为新生代断陷盆地,构造条件复杂,具有差异性与继承性的活动特点。其独特的地理条件及地质构造条件,使盆地内奥灰岩溶不断向深处发育,导致岩溶地下水水位埋深达430～550m,具特深水位特征。
The elevation of Shouyang basin is 276m higher than Taiyuan basin in the west, so there is a saying of “a basin on mountain top”. Because of its high relief, the weather there is very cold, thus people called the place “cold Shouyang”. The basin is a Cenozoic faulted basin, differential and posthumous movements made the basin a complex structural setting. The unique geographical and geological structure made the Ordovician limestone kant developing toward to depth ceaselessly, tiros the reason caused the karstic groundwater level there as deed as 430-550m.
出处
《中国煤田地质》
2005年第5期55-57,共3页
Coal Geology of China
关键词
特深水位
成因探讨
新构造运动
寿阳盆地
extra-deep water table
discussion on origin
neotectonism
Shouyang Basin
