Genesis of brine in South Lake of Zabuye, Tibet using stable isotopes of hydrogen and oxygen
The genesis of chemically unique brines from South Salt Lake in Zabuye is presented based on stable isotope analysis of hydrogen and oxygen. The brines that discharge to this lake were developed mainly by natural evaporation as well as transportation of fluvial water containing melted snow that introduced minerals from terrigenous deposit rather than marine deposits. Moreover, a third water component was identified formed from the interaction between a volcano and geothermal water during the Cenozoic era early in the development of the original brine of this system.
T.L.Deng
Qinghai Institute of Salt Lakes, CAS, Xining, P.R.China
国际会议
第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)
昆明
英文
297-300
2007-07-31（万方平台首次上网日期，不代表论文的发表时间）