Conodont Biostratigraphy in Middle Osagean to Upper Chesterian Strata, North-Central Oklahoma, U.S.A.
<p> The informally known “Mississippian Limestone” stratigraphic interval in north-central Oklahoma, U.S.A. bears no chronostratigraphic markers and has no formally established biostratigraphic framework to date. Conodonts collected from four “Mississippian Limest...
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| Language: | EN |
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Oklahoma State University
2018
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| Online Access: | http://pqdtopen.proquest.com/#viewpdf?dispub=10690774 |