Cenozoic climate change as a possible cause for the rise of the Andes

2003/10/01 by Simon Lamb, Paul M. Davis, Paul Davis · 1 voice · 3 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #Geology and Paleoclimatology Research #earthquake and tectonic studies

paper · doi:10.1038/nature02049

crossref issued 2003/10/01 · crossref published 2003/10/01 · crossref published-print 2003/10/01 · openalex publication_date 2003/10/01 · crossref created 2003/10/22 · crossref deposited 2023/05/18 · openalex created_date 2025/10/10 · crossref indexed 2026/07/20 · openalex updated_date 2026/07/23

Citations

• THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES

Cited by

• Chemical Geodynamics
• The role of climate during high plateau formation. Insights from numerical experiments
• Mesozoic to Cenozoic retroarc basin evolution during changes in tectonic regime, southern Central Andes (31–33°S): Insights from zircon U-Pb geochronology
• An evaluation of factors influencing pore pressure in accretionary complexes: Implications for taper angle and wedge mechanics

Discussions

• It is possible that Andes risen to the modern highs due to change in the climate regime, which caused the change to the shallower subduction -->higher dynamic topography. An old but gold article: doi. [bsky, 6 points, 0 comments]