Ashley Stanton-Yonge
Pontificia Universidad Católica de Chile, Santiago
Activity
2015
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COMPARING FORWARD MODEL TECTONIC BOUNDARY CONDITIONS IN AN OBLIQUELY-CONVERGENT MARGIN: A CASE STUDY FROM THE SOUTHERN ANDES
T318 Strike Slip Fault Systems Transfer Stress Inboard from the Subduction Zone Margin Leading to Basin Subsidence and Orogensis, Are Conduits for Magmatism, and Are Responsible for Far-Traveled Terrane Translation (Posters)Wednesday, 4 November 20159:00 AM - 6:30 PMExhibit Hall