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Charles A. Sandberg, Raymond C. Gutschick, J.G. Johnson, Forrest G. Poole & William J. Sando

Middle Devonian to Late Mississippian event stratigraphy of Overthrust Belt region, Western United States

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Annexes

Résumé

Vingt phénomènes eustatiques et épeirogéniques datés principalement par conodontes du Dévonien moyen au début du Mississippien supérieur dans les régions du Grand Bassin, des Montagnes Rocheuses et dans la ceinture charriée, sont résumés et discutés brièvement.

Abstract

Twenty eustatic and epeirogenic events mainly dated by conodonts are distinguished between the Middle Devonian and the lower Upper Mississippian in Great Basin, in Rocky Mountains and in the Overthrust belt regions.  (Abstracted by the editors).

To cite this article

Charles A. Sandberg, Raymond C. Gutschick, J.G. Johnson, Forrest G. Poole & William J. Sando, «Middle Devonian to Late Mississippian event stratigraphy of Overthrust Belt region, Western United States», Annales de la Société géologique de Belgique [En ligne], Volume 109 (1986), Fascicule 1 (Late Devonian events around the Old Red Continent), 205-207 URL : https://popups.ulg.ac.be/0037-9395/index.php?id=2479.

About: Charles A. Sandberg

U.S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225.

About: Raymond C. Gutschick

U.S. Geological Survey and Department of Earth Sciences, University of Notre Dame, Notre Dame, Indiana 46556.

About: J.G. Johnson

Department of Geology, Oregon State University, Corvallis, Oregon 97331.

About: Forrest G. Poole

U.S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225.

About: William J. Sando

U.S. Geological Survey, E-318 U.S. National Museum, Washington, D.C. 20560.