Evidence for an arid to semi-arid climate during deposition of the Cambrian system in central Texas, U.S.A
作者： Henry S. Chafetz
DOI: 10.1016/0031-0182(80)90050-4
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摘要: Abstract Petrographic evidence indicates that an arid to semi-arid climate existed in central Texas, U.S.A., during accumulation of the Cambrian System. This interpretation is supported by presence ventifacts, quartz with frosted surfaces, fresh well-rounded feldspars, paucity clay material, and situ transported calcitized evaporites.
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