Article ID Journal Published Year Pages File Type
9529286 Chemical Geology 2005 8 Pages PDF
Abstract
The observed 17O-anomalous gypsum deposit in the mid-Gering ash bed is most likely the result of a series of extreme dry fogs that resulted in an intense pulse of atmospheric sulfate deposition to a semiarid playa setting.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Sulfate in modern playa settings and in ash beds in hyperarid deserts: implication for the origin of 17O-anomalous sulfate in an Oligocene ash bed
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