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- W177689377 abstract "Optical and electron petrography were used to test if differences of mineral textures in tonsteins offer any evidence of the alteration history of their volcanic precursors. A suspect tonstein from the Mississippian Sample fm. In Crawford County, IN, and true tonsteins from the Pennsylvanian Breathitt Fm. in Leslie County, KY; Cretaceous Adaville Fm. in Lincoln County, WY; and the Cretaceous Williams Fork Fm. in Moffat and Routt Counties, CO were studied. Optical petrography showed lack of silt or sand in the Indiana clay, minor silt/fine-sand in the Kentucky clay, and lack of mica in both. The Indiana clay is very fine grained and has a strong preferred orientation, whereas the Kentucky clay matrix is also very fine grained but is isotropic. Abundant, angular, quartzofeldspathic, medium sand abounds in the western clays. Very large kaolinite verms up to 0.5 mm in length dominate the western clays. Each large kaolinite contains evenly spaced interlayers of relict biotite extending exactly the width of each verm. Kaolinite in the western clays shows strong compactional strain including undulose extinction, kink bands, and shearing along the basal plane. Compactional fabrics show all of the samples to have altered from their parent material before significant burial." @default.
- W177689377 created "2016-06-24" @default.
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- W177689377 date "1993-03-01" @default.
- W177689377 modified "2023-09-24" @default.
- W177689377 title "Kaolinization in examples of Carboniferous and Cretaceous tonsteins" @default.
- W177689377 hasPublicationYear "1993" @default.
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