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Geochemistry of late Cenozoic lavas on Kunashir Island, Kurile Arc
Author(s) -
Martynov Alexey Y.,
Kimura JunIchi,
Martynov Yuri A.,
Rybin Alexsander V.
Publication year - 2010
Publication title -
island arc
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.554
H-Index - 58
eISSN - 1440-1738
pISSN - 1038-4871
DOI - 10.1111/j.1440-1738.2009.00684.x
Subject(s) - geology , geochemistry , basalt , island arc , crust , volcanic rock , mantle (geology) , isotope geochemistry , rhyolite , radiogenic nuclide , trace element , oceanic crust , subduction , volcano , isotope , paleontology , tectonics , physics , quantum mechanics
Middle Miocene to Quaternary lavas on Kunashir Island in the southern zone of the Kurile Arc were examined for major, trace, and Sr–Nd–Pb isotope compositions. The lavas range from basalt through to rhyolite and the mafic lavas show typical oceanic island arc signatures without significant crustal or sub‐continental lithosphere contamination. The lavas exhibit across‐arc variation, with increasingly greater fluid‐immobile incompatible element contents from the volcanic front to the rear‐arc; this pattern, however, does not apply to some other incompatible elements such as B, Sb, and halogens. All Sr–Nd–Pb isotope compositions reflect a depleted source with Indian Ocean mantle domain characteristics. The Nd and Pb isotope ratios are radiogenic in the volcanic front, whereas Sr isotope ratios are less radiogenic. These Nd isotope ratios covary with incompatible element ratios such as Th/Nd and Nb/Zr, indicating involvement of a slab‐derived sediment component by addition of melt or supercritical fluid capable of mobilizing these high field‐strength elements and rare earth elements from the slab. Fluid mobile elements, such as Ba, are also elevated in all basalt suites, suggesting involvement of slab fluid derived from altered oceanic crust. The Kurile Arc lavas are thus affected both by slab sediment and altered basaltic crust components. This magma plumbing system has been continuously active from the Middle Miocene to the present.