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Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho

Open-File Report 2012-1100

By:
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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.

Additional Publication Details

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
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
Number of Pages:
9
Country:
United States
State:
Idaho
Other Geospatial:
Black Pine Mountains
Online Only (Y/N):
Y
Additional Online Files(Y/N):
Y