georefid:2007-088652SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1007/s00410-006-0135-yThe formation of SiO (sub 2) -rich melts within the deep oceanic crust by hydrous partial melting of gabbros2007-01-01publicationgeorefid:2007-088652
doi:10.1007/s00410-006-0135-y
Koepke, JuergenLeibniz Universitaet Hannover, Institut fuer Mineralogie, Hannover, Federal Republic of GermanyauthorBerndt, JasperWestfaelische Wilhelms-Universitaet, Federal Republic of GermanyauthorFeig, Sandrin T.authorHoltz, FrancoisauthorSpringer International, Heidelberg - New York, InternationalpublisherdocumentHardcopyContributions to Mineralogy and Petrology153 (1)67-84completedIgneous and metamorphic petrologyanatexisbasaltschemical compositioncrustdioritesenrichmentexperimental studiesfeldspar groupframework silicatesgabbrosgeochemistryhydrationigneous rocksimmiscibilityintrusionsmagmatismmajor elementsmeltsmid-ocean ridge basaltsmineral compositionOcean Drilling Programoceanic crustODP Site 735ophiolitepartial meltingpetrologyplagioclaseplagiograniteplate tectonicsplutonic rockspressuresea-floor spreadingshallow depthsilicasilicate meltssilicatessiliceous compositionspreading centersstockstexturestholeiitic compositionvolcanic rocksurn:org.iodp:exp:118:site:735
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urnlargerWorkCitationcampaignEnglishgeoscientificInformation57.155757.1618-32.4327-32.4318