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- W2107496054 abstract "ABSTRACT Evidence is presented to show that the recrystallized rocks of the Comanchean series vary from limestone to dolomites; that the faunal content has not governed the degree of dolomitization; that dolomites are distributed irregularly through the series; that unaltered limestones are present at various horizons; and that porosity is not a function of dolomitization or faunal content, but rather a function of recrystallization either with or without dolomitization." @default.
- W2107496054 created "2016-06-24" @default.
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- W2107496054 date "1931-01-01" @default.
- W2107496054 modified "2023-10-18" @default.
- W2107496054 title "Alteration of Comanchean Limestones of South Central Texas" @default.
- W2107496054 doi "https://doi.org/10.1306/d4268dc4-2b26-11d7-8648000102c1865d" @default.
- W2107496054 hasPublicationYear "1931" @default.
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