Isotopic evolution at San Pedro -Linzor volcanic chain, Central Andes.

Year:

2015

Type of Publication:

Article

Authors:

Godoy, Benigno; Martínez, Paula; LeRoux, Petrus; Kojima, Shoji; de Silva, Shan; Morata, Diego; Parada, Miguel Angel

Journal:

Congreso Geol Soc Chile

BibTex:

@article{Benigno Godoy2015, author = "Benigno Godoy and Paula Mart{\'i}nez and Petrus LeRoux and Shoji Kojima and Shan de Silva and Diego Morata and Miguel Angel Parada", abstract = "The San Pedro –Linzor volcanic chain located in the Central Andean volcanic zone runs along the western border of the Altiplano-Puna magma body(APMB). The APMB corresponds to a partially molten upper crustal (0.7075) to San Pedro (es in the isotopic ratios would be associated with different extends of interaction between mantle-derived magmas and the APMB. Thus, erupted lavas in the SE would have assimilated more crustal material than those that evolved in the NW-most part of the volcanic chain", journal = "Congreso Geol Soc Chile", title = "{I}sotopic evolution at {S}an {P}edro -{L}inzor volcanic chain, {C}entral {A}ndes.", year = "2015", }

Abstract:

The San Pedro –Linzor volcanic chain located in the Central Andean volcanic zone runs along the western border of the Altiplano-Puna magma body(APMB). The APMB corresponds to a partially molten upper crustal (0.7075) to San Pedro (es in the isotopic ratios would be associated with different extends of interaction between mantle-derived magmas and the APMB. Thus, erupted lavas in the SE would have assimilated more crustal material than those that evolved in the NW-most part of the volcanic chain