S. L. Dorobek
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View article: Subsidence across the Antler foreland of Montana and Idaho: Tectonic versus eustatic effects
Subsidence across the Antler foreland of Montana and Idaho: Tectonic versus eustatic effects Open
Devonian and Mississippian sedimentary rocks of western Montana and east-central Idaho were deposited on a cratonic platform that faced a deep basin to the west. The deep basin in Idaho was a northern extension of the Antler foredeep and f…