About: Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature

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About: Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature Goto Sponge NotDistinct Permalink

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scholarly article

Attributes	Values
rdf:type	Item
description	wetenschappelijk artikel (nl) գիտական հոդված (hy) scholarly article (en) наукова стаття, опублікована в січні 1989 (uk) article scientifique publié en 1989 (fr) im Jahr 1989 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q57855360-0D04C8BA-E421-4C9C-A8B9-D946244B05CC
publication date	1989-01-01 00:00:00Z (xsd:dateTime)
author name string	wds:Q57855360-224B5C80-CAA5-4A2E-95E5-378553A39A25 wds:Q57855360-7A41A7AC-FBFE-465A-85A1-9A7A6B5C62D6 wds:Q57855360-BD54F25C-9319-4B40-97AD-8394C70A521F wds:Q57855360-F2828CDF-2401-4C67-A4D0-D1FC7A3131FB
author name string	C.G. Ryan S.H. Sie T.H. Green D.R. Cousens
rdfs:label	Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (en) Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (nl)
skos:prefLabel	Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (en) Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (nl)
name	Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (en) Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (nl)
title	wds:Q57855360-F5611AAB-1C76-4813-BF05-72526BFEE0A1
title	Proton microprobe-determined partitioning of Nb, Ta, Zr, Sr and Y between garnet, clinopyroxene and basaltic magma at high pressure and temperature (en)
page(s)	wds:Q57855360-F7AE5A4A-3495-428A-B801-D0274940B159
page(s)	201-216
instance of	wds:Q57855360-53DEDE13-58CE-478C-ABF0-B64C91019C4F
instance of	scholarly article
main subject	wds:Q57855360-16E80B10-1A59-43D8-9C9D-C466EBBDAE79
main subject	magma
published in	wds:Q57855360-971437AF-80A8-4643-B802-3B4FDD400E5D
published in	Chemical Geology
issue	wds:Q57855360-EAB078AE-3F69-40FC-992D-64569096E8D6
volume	wds:Q57855360-DA963BE8-9C52-4AB9-A38D-69A1FB2DF9C6
issue	3-4
volume	74
DOI	wds:Q57855360-0F72C436-B94E-4F64-9F9B-1FAFA6BAD788
DOI	http://dx.doi.org/10.1016/0009-2541(89)90032-6
DOI	10.1016/0009-2541(89)90032-6
ADS bibcode	wds:Q57855360-7EF3838D-6790-4464-AD97-C6BE56CAF28D
ADS bibcode	1989ChGeo..74..201G
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q57855360
is cites work of	SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C Along-strike variation in the Aleutian Island Arc: Genesis of high Mg# andesite and implications for continental crust Incompatible trace element partitioning and residence in anhydrous spinel peridotites and websterites from the Ronda orogenic peridotite Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions Nb and Ta incorporation and fractionation in titanian pargasite and kaersutite: crystal–chemical constraints and implications for natural systems Geochemistry of lavas from Negros Arc, west central Philippines: Insights into the contribution from the subducting slab Compositional constraints on the continental lithospheric mantle from trace elements in spinel peridotite xenoliths Quantitative trace element analyses of silicate reference materials and a stainless steel using the proton microprobe Trace Element and Sr–Pb–Nd–Hf Isotope Evidence for Ancient, Fluid-Dominated Enrichment of the Source of Aldan Shield Lamproites Magmatic evolution of the area around Wadi Kariem, Central Eastern Desert, Egypt
is cites work of	wds:Q59810622-1624A56B-3638-4EF3-92DF-3BE0EF54EC6A wds:Q57854857-DF93310C-2EFB-4727-B4EC-76D4F6CC0EB6 wds:Q59790710-B1BE0D70-7AE7-4D4D-A8BC-E4F597890EF2 wds:Q107297118-B4039666-8BB3-4475-8745-745C66F917C3 wds:Q59810641-62055732-1F83-4477-A5C1-52FBF6ABBF4F wds:Q57942586-18A77C41-D314-4F2C-A946-66FF9A694369 wds:Q57799438-840411A7-5578-4A5C-A0A6-9E898CE2F141 wds:Q57890223-61B62CD2-0A7B-4587-8928-3D21B713F9A2 wds:Q57852039-54A57C55-81F6-4E4D-A576-FE199C82A848 wds:Q59083341-F89FCF54-B420-40D8-9B1B-6102E89D92DF

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