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- W2368509912 abstract "From Mesozoic to Cenozoic,the big mountains around Qaidam Basin were unceasingly rising and a deposit environment of high mountain and deep basin was formed,which brought abundant sources of salts.Then under extremely drought climate environment,a wide and thick stratum of salt rock was accumulated in the western basin.Based upon this,some brine samples around several representative salt mines were collected and analyzed for their hydrochemical components in order to evaluate the evolution of the brines.The results indicate that all the types of brines are chloride type and magnesium sulfate sub-type,and the oil field brines enrich valuable components of B3+ ,Li+ ,Sr2+ ,Br-and so on,and the salt lakes have abundant contents of K+.In addition,the oil field brines enrich Ca2+ ,poor Mg2+ or.However,the salt lakes and intercrystalline brines enrich Mg2+ and ,poor Ca2+.These results indicate the oil field brines developed dolomization and sulphate reduction.The shallow-layer brines approach evaporating line of Qinghai Lake,which illuminates the salt lake brines resulted from evaporation of rainfall.The hydrogen and oxygen isotopic compositions of the brines may synchronously increase in evolutional pathway,or the δ 18O value has a large positive shift whereas the δ D value has a small one.And the δ D and δ 18O values are similar with those of the spring of the front of mountain mass,and distributes in the range of metamorphosing water.Therefore,the origin of the brines in western Qaidam Basin may be ice-snow melting water or rain water,and this conclusion is consistent with the results of high ion contents of Ca2+ ,Cl-,B3+ ,Li+ ,Sr2+ ,Br-and so on." @default.
- W2368509912 created "2016-06-24" @default.
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- W2368509912 date "2007-01-01" @default.
- W2368509912 modified "2023-09-25" @default.
- W2368509912 title "Characteristics and origin of brines in western Qaidam Basin" @default.
- W2368509912 hasPublicationYear "2007" @default.
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