Origin of Ancient Potash Evaporites: Clues from the Modern Nonmarine Qaidam Basin of Western China
Modern potash salt deposits and associated brines of the Qaidam Basin, western China, demonstrate that some anomalous marine evaporites may have formed from nonmarine brines instead of seawater. Qaidam Basin brines are derived from meteoric river inflow mixed with small amounts of CaCl spring inflow...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1989-09, Vol.245 (4922), p.1090-1092 |
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