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• W1163976455 abstract "This chapter discusses the marginal marine halite. The arrangement of dissolution cavities, patches of clear halite, and areas of chevron halite within the rock layers testifies to a history of repeated episodes of dissolution and precipitation. Shearman proposed that the vertically-oriented dissolution cavities were created during flooding events by the downward percolation of dilute waters into the halite bed and that the evaporative reconcentration of these waters, which followed, precipitated the diagenetic clear halite cement in the brine-filled dissolution cavities. Thus, the halite rock layers, similar to many ancient examples, were the product of a long period of reworking of salt pan halite and groundwater brine diagenesis. The recent halite rock disappeared from the sediment record in early 1983. Its disappearance was due to dissolution by brackish waters that flooded much of the supratidal flat when unusually high amounts of rain fell in Baja California. Although a hard halite-rock layer made up of several halite depositional units (saline pan cycles) was present for many years on the high flats beneath a protective cover of supratidal muds and additional saline deposits, the flooding events of 1983 were too great and eventually led to its dissolution." @default.
• W1163976455 created "2016-06-24" @default.
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• W1163976455 date "1991-01-01" @default.
• W1163976455 modified "2023-10-02" @default.
• W1163976455 title "Chaper 1 Marginal Marine Halite: Sabkhas and Salinas" @default.
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• W1163976455 doi "https://doi.org/10.1016/s0070-4571(08)70259-0" @default.
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