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Geochemistry and petrology of evaporites cored from a deep-sea diapir at site 546 offshore Morocco.
Published Web Locationhttps://doi.org/10.2973/dsdp.proc.79.117.1984
These evaporites are in the potash facies. The S isotope ratio suggests that the anhydrite was derived from sea-water of Permian to Scythian age.-K.A.R.
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