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The Late Pliocene mafic lavas from the Camusú Aike volcanic field (∼50°S, Argentina): Evidence for geochemical variability in slab window magmatism

✍ Scribed by M. D'Orazio; F. Innocenti; P. Manetti; M.J. Haller; G. Di Vincenzo; S. Tonarini


Book ID
116695564
Publisher
Elsevier Science
Year
2005
Tongue
English
Weight
947 KB
Volume
18
Category
Article
ISSN
0895-9811

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