Titlebook: Evaporites; A Geological Compend John K. Warren Book 2016Latest edition Springer International Publishing Switzerland 2016 Economic Geology

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https://doi.org/10.1007/978-3-642-34252-3rface (primary salts) or in the shallow subsurface (secondary salts). Today, bedded accumulations of primary potash evaporites are a relatively rare occurrence. Extremely high solubility of most potash salts means they accumulate in highly restricted, some would say highly continental, modern deposi

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Effective Transport Properties,y greenschist phase, little or nothing of the original sedimentary mineral phase remains with the possible exception of anhydrite (Table 14.1; Spear 1993). Consider “the before and after” situation as a sequence of evaporite-entraining sediments passes into the metamorphic realm. Under a likely “bef

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Patrick G. Grimes,Richard J. Bellows,M. Zahnent and entrapment in subsurface settings ranging from the burial diagenetic through to the metamorphic and igneous realms. Within this framework, this chapter explores relationships between evaporites and lower temperature ore deposits, where ore is defined as a mineral, or an aggregate of minerals

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Sabkhas, Saline Mudflats and Pans,abkhas) and saline pans. These two settings encompass that part of the hydrological spectrum dominated by capillary and ephemeral at-surface brine hydrologies. Climatically, these settings tend to occur in arid deserts (K?ppen zone: BW) in both coastal and continental interior arid settings where sa