18O16O isotope geochemistry of silicic lava flows erupted from Volcán Ollagüe, Andean Central Volcanic Zone

1995/07/01 by T. C. Feeley, T.C. Feeley, Z. D. Sharp +1 · 3 citations
Computer Science · Earth and Planetary Sciences · #Andesite #Basalt #Basaltic andesite #Geochemistry #Geochemistry and Geologic Mapping #Geological and Geochemical Analysis #Geology #Lava #Magma #Petrology #Silicic #Volcanic rock #Volcano #earthquake and tectonic studies

paper · doi:10.1016/0012-821x(95)00094-s

crossref issued 1995/07/01 · crossref published 1995/07/01 · crossref published-print 1995/07/01 · openalex publication_date 1995/07/01 · crossref created 2002/07/25 · crossref deposited 2019/04/24 · openalex created_date 2025/10/10 · crossref indexed 2026/01/08 · openalex updated_date 2026/06/22

Citations

• The volcanic and magmatic evolution of Volcán Ollagüe, a high-K, late quaternary stratovolcano in the Andean Central Volcanic Zone
• Crustal contributions to arc magmatism in the Andes of Central Chile
• Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization
• Uplift of the Central Andean Plateau and bending of the Bolivian Orocline

Cited by

• Faulting-assisted lateral collapses and influence on shallow magma feeding system at Ollagüe volcano (Central Volcanic Zone, Chile-Bolivia Andes)
• Low-pressure evolution of arc magmas in thickened crust: The San Pedro–Linzor volcanic chain, Central Andes, Northern Chile
• Ollagüe [wikipedia]