Open-File Report 2012–1100
AbstractThe Black Pine Mountains, southeastern Cassia County, Idaho, consist of southern and northern blocks separated by a northeast-trending, high-angle fault. Differences in conodont color alteration values distinguish the two blocks. The southern block has significantly higher organic maturation levels than the northern block and is interpreted to have been thrust northeastward adjacent to the northern block. |
First posted June 1, 2012 For additional information contact: Part or all of this report is presented in Portable Document Format (PDF); the latest version of Adobe Reader or similar software is required to view it. Download the latest version of Adobe Reader, free of charge. |
Smith, J.F., Jr., and Wardlaw, B.R., 2012, Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho: U.S. Geological Survey Open-File Report 2012–1100, 5 p., available only at http://pubs.usgs.gov/of/2012/1100.
Abstract
Introduction
Geology
Conodont Color Alteration Indices in the Black Pine Mountains
Interpretation
Summary
References Cited