钾盐矿床成矿条件研究若干进展
王春连1, 刘成林1*,*, 王立成1, 张林兵2

Reviews on Potash Deposit Metallogenic Conditions
Wang Chunlian1, Liu Chenglin1, Wang Licheng1, Zhang Linbing2
图2 裂谷盆地成钾示意图 [ 62 ] 1.石盐；2.钾盐；3.砂砾岩；4.粉砂；5.玄武岩；6.深循环卤水（起源于卤水-矿物反应）；7.地层建造水被驱动上涌；8.岩浆分异热液流体；9.地表盐泉（来自深循环水、建造水的上升排泄）；10.冲洪积物。
Fig.6 Schematic diagram shows that how potash salts formed in rift basin [ 62 ] 1.halite； 2.potash ；3.sandy conglomerates ；4. siltstones； 5.basalts； 6. deep cycle brineoriginated from brine-minerals reaction ；7.upwelling formation water derived by magma；8.magmatic differentiation hydrothermal fluids；9.surface salt springs come from discharge of the deep cycle water and formation water ；10.alluvial deposits