South-to-north pyroxenite–peridotite source variation correlated with an OIB-type to arc-type enrichment of magmas from the Payenia backarc of the Andean Southern Volcanic Zone (SVZ)

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

OriginalsprogEngelsk
TidsskriftContributions to Mineralogy and Petrology
Vol/bind172
Udgave nummer1
Antal sider25
ISSN0010-7999
DOI
StatusUdgivet - 2017

ID: 170405423