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- W993934118 abstract "This chapter describes the different aspects of the clay minerals in the thin loess of the Ohio River basin in the U.S.A. The Ohio River basin occupies about 261,500 km2 above the mouth of the Wabash River in southwestern Indiana and is emplaced eastward across the geologic structure, the Cincinnati arch. Eastward from the mouth of the Wabash River to near Cincinnati, Ohio, successively older bedrock is crossed from Pennsylvanian clastic rocks and coal measures, to Mississippian carbonate rocks, Devonian shales, Silurian limestones, and Ordovician carbonate, and clastic rocks. Wisconsin loess covers a large part of the uplands in the Ohio drainage basin and is >5 inches thick just east of the Wabash River valley in southwestern Indiana and also western Kentucky. Excluding near-surface horizon effects caused by agricultural liming such as high Ca, base saturation, and pH, the chemical properties of the profile are independent of lithologic stratification. It is found that extractable Ca and Mg and base saturation decrease to minimum values across the textural contact and then increase with depth." @default.
- W993934118 created "2016-06-24" @default.
- W993934118 creator A5044237794 @default.
- W993934118 date "1983-01-01" @default.
- W993934118 modified "2023-09-27" @default.
- W993934118 title "Clay Minerals in Thin Loess, Ohio River Basin, U.S.A." @default.
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- W993934118 doi "https://doi.org/10.1016/s0070-4571(08)70790-8" @default.
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