382 6 archive 4 disk0/00/00/03/82 2006-09-14 2008-07-18 09:42:57 2008-07-16 15:45:29 article show Dima.Kamenetsky@utas.edu.au Kamenetsky VS Elburg MA Arculus RJ Thomas R pub 260100 restricted NULL Island-arc magmas; Picrites; Olivine; Clinoenstatite; Magmatic inclusions; Xenocrysts; Mantle (15/4 SvA) fixed initials, added DOI and URL; restricted access as is an Elsevier journal and pub version cannot be used. Unravelling the origin of different components contributing to subduction-related magmas is a prerequisite to understanding the sources and processes involved in their origins. Mafic, high-Ca subduction-related magmas from geographically-diverse areas (Indonesia, Solomon Islands, Kamchatka, Valu Fa Ridge) contain two populations of olivine crystals, of which only the high-Ca population (CaO = 0.3-0.5 wt.%) crystallized from the melt that dominantly contributed to the whole rock composition. Forsterite-rich (Fo90-94), low-Ca (CaO < 0.15 wt.%), high-Ni (NiO > 0.3 wt.%) olivine crystals, which constitute 16-37 vol.% of total olivine population, are generally interpreted as mantle or lithospheric xenocrysts. However, in these samples, the olivine shape and chemical zoning, the composition of included minerals (orthopyroxene, clinoenstatite and Cr-spinel) and presence of melt inclusions, are indications that these crystals are phenocrysts from a mafic magma with high silica and low calcium contents. The coexistence of contrasting magmas (mafic high-Ca silica-poor versus low-Ca silica-rich) within a number of arc systems and their mixing may not be a rare event, and should be taken into account when developing models of arc petrogenesis. 2006-10 published Chemical Geology 233 3-4 346-357 10.1016/j.chemgeo.2006.03.010 University of Tasmania UNSPECIFIED TRUE http://dx.doi.org/10.1016/j.chemgeo.2006.03.010 710 1 382 1 application/pdf en staffonly cc_utas

CG-lowCa-olivine.pdf

CG-lowCa-olivine.pdf 1188040 http://eprints.utas.edu.au/382/1/CG-lowCa-olivine.pdf