Enrichments of the mantle sources beneath the Southern Volcanic Zone (Andes) by fluids and melts derived from abraded upper continental crust

Paul Martin Holm, Nina Søager, Charlotte Thorup Dyhr, Mia Rohde Nielsen

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35 Citationer (Scopus)

Abstract

Mafic basaltic-andesitic volcanic rocks from the Andean Southern Volcanic Zone (SVZ) exhibit a northward increase in crustal components in primitive arc magmas from the Central through the Transitional and Northern SVZ segments. New elemental and Sr–Nd-high-precision Pb isotope data from the Quaternary arc volcanic centres of Maipo (NSVZ) and Infernillo and Laguna del Maule (TSVZ) are argued to reflect mainly their mantle source and its melting. For the C-T-NSVZ, we identify two types of source enrichment: one, represented by Antuco in CSVZ, but also present northward along the arc, was dominated by fluids which enriched a pre-metasomatic South Atlantic depleted MORB mantle type asthenosphere. The second enrichment was by melts having the characteristics of upper continental crust (UCC), distinctly different from Chile trench sediments. We suggest that granitic rocks entered the source mantle by means of subduction erosion in response to the northward increasingly strong coupling of the converging plates. Both types of enrichment had the same Pb isotope composition in the TSVZ with no significant component derived from the subducting oceanic crust. Pb–Sr–Nd isotopes indicate a major crustal compositional change at the southern end of the NSVZ. Modelling suggests addition of around 2 % UCC for Infernillo and 5 % for Maipo
OriginalsprogEngelsk
Artikelnummer1004
TidsskriftContributions to Mineralogy and Petrology
Vol/bind167
Antal sider27
ISSN0010-7999
DOI
StatusUdgivet - 2014

Emneord

  • Det Natur- og Biovidenskabelige Fakultet
  • Andean volcanism
  • Southern Volcanic Zone
  • Basaltic andesite
  • Pb-Sr-Nd isotopes
  • Mantle melting
  • Subduction erosion

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