摘要
Potash deposits and various types of breccia-bearing argillaceous roeksalts and their surfacial salt-dissolved rocks are found in the Lower Tertiary strata in JiangehengMengla area, Yunnan Province. Distinct sedimentary cycles have been noticed for the potassium salt-bearing formations. These rocks are essentially mud stones cemented by salt minerals formed in stagnant, reducing environment in continental sabkhas. The potash deposits and potassium-bearing strata in this region are of marine origins as evidenced by dominant chlorides and high contents of Br and Rb in salt minerals.Methods for further prospecting efforts are also suggested.
Potash deposits and various types of breccia-bearing argillaceous rocksalts and theirsurfacial salt-dissolved rocks are found in the Lower Tertiary strata in Jiangcheng-Mengla area,Yunnan Province.Distinct sedimentary cycles have been noticed for thepotassium salt-bearing formations.These rocks are essentially mud stones cemented bysalt minerals formed in stagnant,reducing environment in continental sabkhas.Thepotash deposits and potassium-bearing strata in this region are of marine origins asevidenced by dominant chlorides and high contents of Br and Rb in salt minerals.Mcthods for further prospecting efforts are also suggested.
出处
《地球化学》
CAS
1982年第2期143-154,共12页
Geochimica