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A lithic description and gamma-ray log of a classic outcrop section provide a basis for correlation with subsurface units.
Excerpt from Stratigraphy of the Chattanooga Shale (Upper Devonian and Lower Mississippian) In Vicinity of Big Stone Gap, Wise County, Virginia Composition, maximum grain size, and lamination were examined in 30 thin sections of the exposed rocks. Quartz and feldspar, clay, coarse micaceous minerals, organic matter, pyrite, chert, and rock fragments were recognized in decreasing abundance. Coarsest grains of quartz and feldspar range in size from fine sand to silt. Two types of lamination recognized in thin section are distinct silt laminae and distinct organic laminae. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.