Paleogene topographic and climatic evolution of the Northern Rocky Mountains from integrated sedimentary and isotopic data

Author:

Schwartz Theresa M.1,Methner Katharina2,Mulch Andreas23,Graham Stephan A.4,Chamberlain C. Page4

Affiliation:

1. Geology & Geological Engineering Department, Colorado School of Mines, 1516 Illinois Street, Golden, Colorado 80403, USA

2. Senckenberg Biodiversity and Climate Research Centre, Georg-Voigt-Straße 14-16, 60325 Frankfurt am Main, Germany

3. Institute of Geosciences, Goethe University Frankfurt, Altenhöferallee 1, 60438 Frankfurt am Main, Germany

4. Department of Geological Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA

Publisher

Geological Society of America

Subject

Geology

Reference144 articles.

1. Cordilleran metamorphic core complexes—From Arizona to southern Canada;Armstrong;Annual Review of Earth and Planetary Sciences,1982

2. Tertiary Sedimentary Facies, Depositional Environments, and Structure, Jefferson Basin, Southwest Montana [M.S. thesis];Axelrod,1984

3. The Oligocene Haynes Creek Flora of Eastern Idaho;Axelrod,1998

4. Biostratigraphy and magnetostratigraphy of the mid-Miocene Railroad Canyon sequence, Montana and Idaho, and age of the mid-Tertiary unconformity west of the continental divide;Barnosky;Journal of Vertebrate Paleontology,2007

5. Prelude to the Anthropocene: Two new North American Land Mammal Ages (NALMAs);Barnosky;The Anthropocene Review,2014

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