Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho
Open-File Report
2012-1100
By: Fred J. Smith Jr. and Bruce R. Wardlaw
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Abstract
The 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.
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho |
| Series title | Open-File Report |
| Series number | 2012-1100 |
| DOI | 10.3133/ofr20121100 |
| Year Published | 2012 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Publisher location | Reston, VA |
| Description | iv, 5 p.; XLS Download of Table 1 |
| First page | i |
| Last page | 5 |
| Country | United States |
| State | Idaho |
| Other Geospatial | Black Pine Mountains |
| Online Only (Y/N) | Y |
| Additional Online Files (Y/N) | Y |