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Thermal Maturity Patterns CAI and Ro in the Ordovician and Devonian Rocks of the Appalachian Basin in New York State

The classic study by Epstein and others (1977), using conodont alteration index (CAI) isograds, is the established standard for evaluating thermal maturity patterns of lower...
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Thermal Maturity Patterns CAI and Ro in the Ordovician and Devonian Rocks of the Appalachian Basin in Pennsylvania

The objective of this study is to enhance existing thermal maturity maps in Pennsylvania by establishing: 1) new subsurface CAI data points for the Ordovician and Devonian and...
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Thermal Maturity Patterns CAI and Ro in Upper Ordovician and Devonian Rocks of the Appalachian Basin A Major Revision of USGS Map I–917–E Using New Subsurface Collections

The conodont color alteration index (CAI) introduced by Epstein and others (1977) and Harris and others (1978) is an important criterion for estimating the thermal maturity of...
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