UNIGE document Scientific Article
previous document  unige:29473  next document
add to browser collection

Assimilation of the plutonic roots of the Andean arc controls variations in U-series disequilibria at Volcan Llaima, Chile

Bourdon, B.
Koornneef, J.M.
Langmuir, C.H.
Aciego, S.
Published in Earth and Planetary Science Letters. 2011, vol. 303, no. 1-2, p. 37-47
Abstract U-series disequilibria provide important constraints on the processes and time scales of melt production, differentiation, and transport in subduction settings. Such constraints, which are essential for understanding the chemical evolution of the continental crust, are conventionally based on the assumption that the U-series disequilibria measured in mafic lavas are produced during mantle metasomatism and melting, and that intracrustal differentiation and assimilation have limited impacts. Here we show that mantle-derived U-series disequilibria in mafic lavas erupted at Volcán Llaima, Chile are significantly diminished by assimilation of plutonic rocks forming Llaima's subvolcanic basement. This contamination process is extremely subtle in terms of “classical” indicators of crustal assimilation like Sr, Nd or Pb isotopes because it is a manifestation of assimilative recycling of the plutonic roots of the arc. This process results in variations in U-series disequilibria and incompatible trace element ratios that are significant compared to regional and global variability in arc magmas. Furthermore, it yields linear correlations between U-series excesses and incompatible trace element ratios that are generally interpreted as slab-fluid indicators and chronometers, or tracers of sediment recycling in subduction zone. Cannibalization of ancestral magmas by ascending melts warrants careful evaluation when considering the components and chemical fluxes in subduction zones. Linear arrays defined by activity ratios of U-series nuclides with different half-lives may be the most reliable indicators of assimilative recycling of ancestral intrusive magmas.
Keywords U-seriesAssimilationArc magmatismBasaltic andesite
Full text
Research group Physical Volcanology and Geological Risk
(ISO format)
REUBI, Olivier et al. Assimilation of the plutonic roots of the Andean arc controls variations in U-series disequilibria at Volcan Llaima, Chile. In: Earth and Planetary Science Letters, 2011, vol. 303, n° 1-2, p. 37-47. doi: 10.1016/j.epsl.2010.12.018 https://archive-ouverte.unige.ch/unige:29473

456 hits

0 download


Deposited on : 2013-08-28

Export document
Format :
Citation style :