Petrography, diagenesis and depositional model for potash deposits of north central Iran, and use of Bromine geochemistry as a prospecting tool
2003
The worldwide sea-level fluctuations during the Pyrenean Orogeny caused substantial regressions in the north of Central Iran during the Eocene-Oligocene time. These orogenic activities shaped shallow marginal marine basins in some regions, which were sites for subsequent evaporite deposition.
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