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Regional chemical diversity, crustal and mantle sources and evolution of central Andean Puna plateau ignimbrites
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“The similarity between the 87 Sr/ 86 Sr ratios of the Rosario River (0.715; Garcia et al., 2020) and the ratios of rocks from the Pairique volcanic complex (~0.716;Kay et al., 2010) represent an additional evidence of the strong relation between the hydrothermal fluid circulation to the north and the main source of recharge of the Salar de Olaroz.”
From Chemical and isotopic features of Li-rich brines from the Salar de Olaroz, Central Andes of NW Argentina (2020) · cites this paper as Kay et al., 2010
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Metadata
- Authors
- Kay, S. M., Coira, B. L., Caffe, P. J., & Chen, C.-H.
- Affiliations
- Cornell University (US)
- Consejo Nacional de Investigaciones Científicas y Técnicas (AR)
- Institute of Earth Sciences, Academia Sinica (TW)
- Corresponding author
- Kay, Suzanne Mahlburg
- Venue
- Journal of Volcanology and Geothermal Research
- Publisher
- Elsevier BV
- Published
- 2010-12
- Volume
- 198
- Issue
- 1-2
- Pages
- 81-111
- ISSN
- 0377-0273 (ISSN-L)
- OpenAlex
- W2049575148
- Cited by
- 193
- References
- 117
- Citations by year
- 2026: 17 · 2025: 10 · 2024: 3 · 2023: 19 · 2022: 16 · 2021: 15 · 2020: 13 · 2019: 16 · 2018: 12 · 2017: 9 · 2016: 16 · 2015: 13 · 2014: 11 · 2013: 15 · 2012: 6
- FWCI
- 6.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Volcanology and Geothermal Research (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Tectonic Studies in Latin America
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Keywords
- Altiplano-Puna plateau, rhyodacite, crustal magma source, mantle-derived magma, crustal contamination, fractional crystallization, Sr-Nd isotopes, oxygen isotopes, trace element geochemistry, rare earth elements, crustal thickening
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