Miocene Growth of the Patagonian Andes Revealed by Sedimentary Provenance of the Río Guillermo Formation, Magallanes-Austral Basin, Chile and Argentina (51°30’S)

Joel S Leonard, Arizona State University, School of Earth and Space Exploration, Tempe, United States and Julie C Fosdick, University of Connecticut, Department of Geography, Groton, CT, United States
Back to: Sedimentary Basin Records of Convergent Orogenic Systems I