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Geologie & Mijnbouw
AbstractThe Late Permian Zechstein carbonates in the Southern Permian Basin were deposited under marine conditions. The carbonates form part of a largely progradational infill, with a gradual northward facies shift. The paleogeography of the Zechstein carbonate deposits has been reviewed recently on the base of well data, cores and publications. This has resulted in three updated maps of the carbonate units. These maps reflect the increase in knowledge of the palaeogeography of the Zechstein asdoi:10.1017/s0016774600021545 fatcat:eihrpe47o5dtpolhpzuiabiq4a