What Is Evaporite Karst? Why Can Rock Salt and Gypsum Form Caves, Subsidence and Sinkholes?
USGS explanation of caves, subsidence and sinkholes produced by dissolution of highly soluble halite and gypsum.
USGS explanation of caves, subsidence and sinkholes produced by dissolution of highly soluble halite and gypsum.
The geochemical logic behind enrichment of K, Mg, Li and other elements in residual brines after halite precipitation.
How near-surface evaporation, temperature and brine movement control halite, gypsum and carnallite precipitation in saline systems.
A USGS strontium-isotope test of whether Castile Formation evaporites were derived mainly from seawater or strongly mixed continental waters.
The development of the thick dolomite, gypsum/anhydrite, halite and potash succession in the southwestern US Permian Basin.
How USGS interpretations of Castile and Salado evaporites explain gypsum and halite forming under different hydrologic conditions.
Why thick rock-salt and gypsum successions generally require repeated replenishment rather than a single isolated sea drying once.
An explanation of the typical gypsum/anhydrite, halite and sylvite-potash precipitation sequence in marine evaporite systems.
A synthesis of modern, Silurian, Permian, Cretaceous and Neoproterozoic halite studies explaining why halite is a powerful archive of paleoseawater chemistry.
Testing fluid-inclusion analytical methods with laboratory-grown halite in NaCl-KCl-MgCl2-CaCl2 brine systems.