The Devonian-Mississippian and Kinderhookian-Osagean boundaries in the East-Central United States are paracontinuities
By: by James E. Conkin and Barbara M. Conkin.
Contributors: Conkin, Barbara M., joint author.
Edition: 1st ed.
Series: University of Louisville studies in paleontology and stratigraphy ;; no. 4
Publisher: University of Louisville
Published: 1975
Place of publication: Louisville, Ky
Language: eng
Number of pages: 54
Subjects: Geology, Stratigraphic -- Mississippian.; Geology, Stratigraphic -- Devonian.; Geology -- Middle West.
Notes: Bibliography: p. 27-28.