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Economic Geology; August 1961; v. 56; no. 5; p. 996-997
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Postdepositional alteration of sandstone minerals under acidic reducing conditions; a factor in the interpretation of sandstone texture

B. K. Holdsworth

Notes that development of secondary clay minerals from potash feldspar and other detrital minerals in the Carboniferous (Namurian) subgraywacke sandstones of southwest Derbyshire, England, may have occurred in a highly acid reducing environment such as has been postulated for postdepositional alteration of ilmenite in unconsolidated sediments.

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