Slab-derived components in the subcontinental lithospheric mantle beneath Chilean Patagonia: Geochemistry and Sr–Nd–Pb isotopes of mantle xenoliths and host basalt
Author
dc.contributor.author
Jalowitzki, Tiago
Author
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Gervasoni, Fernanda
Author
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Conceição, Rommulo V.
Author
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Orihashi, Yuji
Author
dc.contributor.author
Bertotto, Gustavo W.
Author
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Sumino, Hirochika
Author
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Schilling, Manuel E.
Author
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Nagao, Keisuke
Author
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Morata Céspedes, Diego
Author
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Sylvester, Paul
Admission date
dc.date.accessioned
2018-05-31T14:04:13Z
Available date
dc.date.available
2018-05-31T14:04:13Z
Publication date
dc.date.issued
2017
Cita de ítem
dc.identifier.citation
Lithos 292–293 (2017) 179–197
es_ES
Identifier
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https://doi.org/10.1016/j.lithos.2017.09.008
Identifier
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https://repositorio.uchile.cl/handle/2250/148383
Abstract
dc.description.abstract
In subduction zones, ultramafic xenoliths hosted in alkaline basalts can yield significant information about
the role of potential slab-derived components in the subcontinental lithospheric mantle (SCLM). Chemical and
isotopic heterogeneities in such xenoliths are usually interpreted to reflect melt extraction followed by metasomatic
re-enrichment. Here we report new whole-rock major, trace element and isotopic (Sr–Nd–Pb) data for a
Proterozoic suite of 17 anhydrous spinel-lherzolites and Eocene (new K–Ar data) host alkaline basalt found
near Coyhaique (~46°S), Aysén Region, Chile. These Patagonian nodules are located in a current back-arc
position, ~100 km east of the present day volcanic arc and ~320 km from the Chile Trench.
The mantle xenoliths consist of coarse- to medium-grained spinel-lherzolites with trace element compositions
characteristic of a subduction zone setting, such as pronounced negative Nb, Ta and Ti anomalies coupled with
significant enrichment of LILEs (e.g., U) and chalcophile elements (W, Pb and Sn).Most of themare characterized
by flat to depleted light-rare earth element (LREE) patterns (Ce/YbN = 0.6–1.1) coupled with less radiogenic
Sr–Pb (87Sr/86Sr=0.702422–0.703479; 206Pb/204Pb=18.212–18.539) and more radiogenic Nd isotopic compositions
(143Nd/144Nd = 0.512994–0.513242), similar to the depleted mantle component (DMM or PREMA).
In contrast, samples with slight LREE enrichment (Ce/YbN=1.3–1.8) show more radiogenic Sr–Pb (87Sr/86Sr=
0.703791–0.704239; 206Pb/204Pb =18.572–18.703) and less radiogenic Nd isotopic compositions (143Nd/144Nd =
0.512859–0.512934), similar to the EM-2 reservoir. These new geochemical and isotope data suggest that the
Coyhaique spinel-lherzolites are derived from a heterogeneous SCLMresulting from mixing between a depleted
mantle component and up to 10% of slab-derived components. The enriched component added to the SCLM represents
variable extents of melts of both subducted Chile Trench sediments andmodified oceanic crust throughout
the initial stages of the Farallón–Aluk ridge collision during Paleocene to Eocene time. However, based on the
tectonic evolution of southern South America, we cannot exclude the influence of long-lived subduction events
beneath south Patagonia. Although we believe that the studied samples were brought to the surface in this
geodynamic context, there is no evidence that ocean island basalt (OIB)–like melts related to the Farallón–
Aluk asthenospheric slab window affected the peridotite composition.
The host alkaline basalt is a single unit with a HIMU-like OIB signature characterized by marked positive Nb–Ta
anomalies coupledwith negative anomalies in highly incompatible and fluid-mobile elements (Rb, K, Pb, and Sr).
The compositional similarity between the HIMU-like OIB mantle source and the host basalt is also evident from
trace element ratios [(Ba–Th–K–La–Zr)/Nb] as well as by the low 87Sr/86Sri (0.703039–0.703058) and relatively
high 143Nd/144Ndi (0.512880–0.512874) and 206Pb/204Pb (19.333–19.389) isotopic ratios. The low206Pb/204Pb ratios
compared to end-member HIMU lavas (e.g., Sta. Helena and the Cook-Austral Islands) suggest that this region was modified by processes associated with a prolonged period of subduction related to the Andean orogenesis
and the recycling of several oceanic plates beneath the continent, following the Mesozoic breakup of
Gondwana or an even older subduction-related event with young recycling ages (b2 Ga).
es_ES
Patrocinador
dc.description.sponsorship
The National Council of Technological and Scientific Development –
CNPq, Brazil, JSPS KAKENHI Grant Numbers 21403012 & 15H02630 /
The Earthquake Research Institute (ERI) cooperative
research program, University of Tokyo
Slab-derived components in the subcontinental lithospheric mantle beneath Chilean Patagonia: Geochemistry and Sr–Nd–Pb isotopes of mantle xenoliths and host basalt