Dynamic topography control on Patagonian relief evolution as inferred from low temperature thermochronology

2013/02/01 by Benjamin Guillaume, Cécile Gautheron, Thibaud Simon-Labric +6 · 3 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #Geology and Paleoclimatology Research #earthquake and tectonic studies

paper · doi:10.1016/j.epsl.2012.12.036

crossref issued 2013/02/01 · crossref published 2013/02/01 · crossref published-print 2013/02/01 · openalex publication_date 2013/02/01 · crossref created 2013/02/21 · crossref deposited 2020/07/22 · openalex created_date 2025/10/10 · crossref indexed 2026/07/15 · openalex updated_date 2026/07/29

Citations

• Subduction of the Chile Ridge: Upper mantle structure and flow
• Glaciation as a destructive and constructive control on mountain building
• Late Cenozoic tectonics of the Southern Chile Trench
• Geologically current plate motions
• Neogene kinematic history of Nazca–Antarctic–Phoenix slab windows beneath Patagonia and the Antarctic Peninsula

Cited by

• Constraints on the Neogene growth of the central Patagonian Andes at the latitude of the Chile triple junction (45–47°S) using U/Pb geochronology in synorogenic strata
• Miocene [wikipedia]
• Patagonia [wikipedia]