Mesozoic to Cenozoic retroarc basin evolution during changes in tectonic regime, southern Central Andes (31–33°S): Insights from zircon U-Pb geochronology

2018/10/13 by Chelsea Mackaman-Lofland, Chelsea Mackaman‐Lofland, Brian K. Horton +4
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1016/j.jsames.2018.10.004

openalex publication_date 2018/10/13 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29

Citations

• Cenozoic climate change as a possible cause for the rise of the Andes
• The Neuquén Basin: an overview
• Tectono-stratigraphic evolution of the Andean Orogen between 31 and 37°S (Chile and Western Argentina)
• Ages and cooling history of the Early Cretaceous Caleu pluton: testimony of a switch from a rifted to a compressional continental margin in central Chile