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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 38 (1968)No. 2. (June), Pages 516-529

Clay Mineralogy of Pluvial Lake Sediments, Southern High Plains, Texas

W. T. Parry, C. C. Reeves, Jr.

ABSTRACT

Lacustrine sediments Previous HitfromNext Hit six pluvial lake basins on the southern High Plains, Texas contain illite, montmorillonite, interstratified illite-montmorillonite, kaolinite, glauconitic mica, and in two basins, sepiolite. Sepiolite, illite-montmorillonite, and glauconitic mica are authigenic; some of the montmorillonite is derived Previous HitfromNext Hit volcanic ash, but most of the lacustrine clay is detrital and representative of ancient soils of the Llano Estacado. Increase in kaolinite and montmorillonite with depth and corresponding decrease in illite is indicative of a Pleistocene pluvial period antedating Tahoka Clay time (14,000 to 22,000 years B. P.). Lacustrine strata of post-Tahoka age, formed in a closed lake environment, consist of illite, illite-montmorillonite, montmorillonite, sepiolite with gypsum, sodium sulfate, glauconitic mica, and dolomite.


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