Southern Patagonian plateau basalts and deformation: Backarc testimony of ridge collisions
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The Chile triple junction at ∼46° S delimits the surface tip of the asthenospheric window, which opened during the last ∼16 Myr from south to north.
“The Chile triple junction (CTJ) at ∼ 46° S delimits the surface tip of the asthenospheric window, which opened during the last ∼ 16 Myr from south to north (Ramos and Kay, 1992;Breitsprecher and Thorkelson, 2009).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Ramos and Kay, 1992
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Paleomagnetism and 40Ar/39Ar Chronology of Lavas from Meseta del Lago Buenos Aires, Patagonia
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Self-citation
- Authors
- Ramos, V. A., & Kay, S. M.
- Affiliations
- Cornell University (US)
- Venue
- Tectonophysics
- Publisher
- Elsevier BV
- Published
- 1992-04
- Volume
- 205
- Issue
- 1-3
- Pages
- 261-282
- ISSN
- 0040-1951 (ISSN-L)
- OpenAlex
- W1987166327
- Cited by
- 317
- References
- 41
- Citations by year
- 2026: 6 · 2025: 9 · 2024: 15 · 2023: 12 · 2022: 14 · 2021: 16 · 2020: 10 · 2019: 15 · 2018: 16 · 2017: 8 · 2016: 9 · 2015: 9 · 2014: 10 · 2013: 11 · 2012: 7
- FWCI
- 3.11
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Tectonophysics (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Tectonic Studies in Latin America
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Keywords
- slab window, continental crust contamination, continental margin
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