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- W1973757907 abstract "Gypsum is the most common sulfate mineral that occurs on the earth's surface or in the shallow subsurface, whereas anhydrite occurs in relatively deeper subsurface settings. Anhydrite is described here from the Lockport Formation (Middle Silurian) of New York. This occurrence is unusual as the anhydrite is present on the surface in a temperate climatic zone where the regional rainfall averages ∼80 cm per year. The anhydrite is of nodular form and has an incomplete rind composed of megaquartz. Petrographic characteristics and megafeatures indicate that formation of the nodule followed shortly after dolomitization. Growth of the nodule probably took place in an open space. Overall sequence of events is indicated to be: dolomitization → dissolution of gypsum → precipitation of anhydrite → partial silicification of the nodule surface." @default.
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- W1973757907 date "1981-07-01" @default.
- W1973757907 modified "2023-10-16" @default.
- W1973757907 title "An unusual occurrence of surficial anhydrite in a moist temperate zone: Example from the lockport formation (Middle Silurian) of New York" @default.
- W1973757907 cites W2069144490 @default.
- W1973757907 doi "https://doi.org/10.1016/0037-0738(81)90003-8" @default.
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