Foreland basin response to middle Cretaceous thrust belt evolution, southwestern Montana, USA
Author:
Affiliation:
1. 1Earth and Environmental Sciences Department, University of Iowa, Iowa City, Iowa 52242, USA
2. 2Geosciences Department, Idaho State University, Pocatello, Idaho 83209, USA
Abstract
Publisher
Geological Society of America
Subject
Stratigraphy,Geology
Link
https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/18/6/1783/5737927/ges02521.1.pdf
Reference114 articles.
1. Kinematics of décollement folding in the Lost River Range, Idaho;Anastasio;Journal of Structural Geology,1997
2. Extra-basinal fluid infiltration, mass transfer, and volume strain during folding: Insights from the Idaho-Montana thrust belt;Anastasio;American Journal of Science,2004
3. Baar, E.E. , 2009, Determining the Regional-scale Detrital Zircon Provenance of the Middle-late Ordovician Kinnikinic (Eureka) Quartzite, East-central Idaho, US [M.S. thesis]: Washington State University, 134 p.
4. Detrital zircon record of mid-Paleozoic convergent margin activity in the northern Rocky U.S. Mountains: Implications for the Antler orogeny and early evolution of the North American Cordillera;Beranek;Lithosphere,2016
5. Timing and deformation conditions of the western Idaho shear zone, West Mountain, west-central Idaho;Braudy;Lithosphere,2017
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1. An exploratory study of “large‐n” detrital zircon geochronology of the Book Cliffs, UT via rapid (3 s/analysis) U–Pb dating;Basin Research;2024-01
2. A kinematic model linking the Sevier and Laramide belts in the Idaho-Montana fold-thrust belt, U.S. Cordillera;Geosphere;2023-10-27
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