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

Smith, Fred J., Jr.; Wardlaw, Bruce R.

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.

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USGS Numbered Series

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70038626

Citation Author:

Smith, Fred J., Jr.; Wardlaw, Bruce R.

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English

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iv, 5 p.; XLS Download of Table 1

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U.S. Geological Survey

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Open-File Report

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OFR

Citation Series Number:

2012-1100

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Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho; 2012; OFR; 2012-1100; Smith, Fred J., Jr.; Wardlaw, Bruce R.

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2012

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citation/reference

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Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho; 2012; OFR; 2012-1100; Smith, Fred J., Jr.; Wardlaw, Bruce R.