盐泉
2.Canadians have long revered SaltSpring as a pristine refuge for the eccentric and creative.
4.During the deposition period of Taoshuyuan Formation from Eocene to Oligocene Miocene developed almost one thousand meter thick plaster salt rock, whose most component is anhydrite, in the Yanmuxi Shenquan region of the west of Taibei depression.
5.It is estimated for Xinancun spring basin of the southeast of·Shanxi Province by environ-mental isotopic method that the ages of karst ground water from Middle Ordovician andCambrian-Ordovician aquifers are 80 and 84 years,their reserves 2.57×10 ̄(10)and 3.15×10 ̄(10)m ̄3,respectively,The coefficient of infiltration is 0.21 in the recharge areas of carbonaterock regions.

