High-pressure phase equilibria of a high-magnesia basalt and the genesis of primary oceanic basalts

High-P phase equilibria studies on a high-MgO basalt from the Tortuga ophiolite complex indicate that olivine + orthopyroxene + clinopyroxene + garnet are its liquidus phases at 25 kbar. The data are combined with results obtained on other tholeiitic basalt compositions, and are used to construct ps...

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Veröffentlicht in:The American mineralogist 1984-02, Vol.69 (1-2), p.1-15
Hauptverfasser: Elthon, Don, Scarfe, Christopher M
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description High-P phase equilibria studies on a high-MgO basalt from the Tortuga ophiolite complex indicate that olivine + orthopyroxene + clinopyroxene + garnet are its liquidus phases at 25 kbar. The data are combined with results obtained on other tholeiitic basalt compositions, and are used to construct pseudoliquidus phase diagrams for evaluating and predicting the nature of primary magmas and melting of the mantle at high P.
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The data are combined with results obtained on other tholeiitic basalt compositions, and are used to construct pseudoliquidus phase diagrams for evaluating and predicting the nature of primary magmas and melting of the mantle at high P.</description><identifier>ISSN: 0003-004X</identifier><identifier>EISSN: 1945-3027</identifier><language>eng</language><publisher>Mineralogical Society of America</publisher><subject>Baffin Bay ; basalts ; Betts Cove Ophiolite ; Canada ; chain silicates ; clinopyroxene ; composition ; crust ; Eastern Canada ; feldspar group ; framework silicates ; garnet ; Gorgona Island ; high pressure ; igneous and metamorphic rocks ; igneous rocks ; Lewis Hills Ophiolite ; magmas ; mantle ; nesosilicates ; Northwest Territories ; olivine ; olivine group ; Ordovician ; orthopyroxene ; orthosilicates ; oxides ; Paleozoic ; petrology ; phase equilibria ; plagioclase ; pressure ; pyroxene group ; Quebec ; silicates ; spinel ; Tortuga Ophiolite ; Ungava ; volcanic rocks ; Western Canada</subject><ispartof>The American mineralogist, 1984-02, Vol.69 (1-2), p.1-15</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom @Twickenham @GBR @United Kingdom</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785</link.rule.ids></links><search><creatorcontrib>Elthon, Don</creatorcontrib><creatorcontrib>Scarfe, Christopher M</creatorcontrib><title>High-pressure phase equilibria of a high-magnesia basalt and the genesis of primary oceanic basalts</title><title>The American mineralogist</title><description>High-P phase equilibria studies on a high-MgO basalt from the Tortuga ophiolite complex indicate that olivine + orthopyroxene + clinopyroxene + garnet are its liquidus phases at 25 kbar. The data are combined with results obtained on other tholeiitic basalt compositions, and are used to construct pseudoliquidus phase diagrams for evaluating and predicting the nature of primary magmas and melting of the mantle at high P.</description><subject>Baffin Bay</subject><subject>basalts</subject><subject>Betts Cove Ophiolite</subject><subject>Canada</subject><subject>chain silicates</subject><subject>clinopyroxene</subject><subject>composition</subject><subject>crust</subject><subject>Eastern Canada</subject><subject>feldspar group</subject><subject>framework silicates</subject><subject>garnet</subject><subject>Gorgona Island</subject><subject>high pressure</subject><subject>igneous and metamorphic rocks</subject><subject>igneous rocks</subject><subject>Lewis Hills Ophiolite</subject><subject>magmas</subject><subject>mantle</subject><subject>nesosilicates</subject><subject>Northwest Territories</subject><subject>olivine</subject><subject>olivine group</subject><subject>Ordovician</subject><subject>orthopyroxene</subject><subject>orthosilicates</subject><subject>oxides</subject><subject>Paleozoic</subject><subject>petrology</subject><subject>phase equilibria</subject><subject>plagioclase</subject><subject>pressure</subject><subject>pyroxene group</subject><subject>Quebec</subject><subject>silicates</subject><subject>spinel</subject><subject>Tortuga Ophiolite</subject><subject>Ungava</subject><subject>volcanic rocks</subject><subject>Western Canada</subject><issn>0003-004X</issn><issn>1945-3027</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotkE1LxDAYhIMoWFf_Q-4SyGebHGVRV1jwouCtvE3ftlm6bU1axH9vi8scBoaHGZgrkgmnDVNcFtck45wrxrn-uiV3KZ04l1IZlxF_CG3HpogpLRHp1EFCit9L6EMVA9CxoUC7jTlDO2BaowoS9DOFoaZzh7TFLU4bOcVwhvhLR48wBH8h0z25aaBP-HDxHfl8ef7YH9jx_fVt_3RkIIWcmRCVh9rVzhaV0YVA00hlEU2uvdHGWm6NyCWvHdeiQCEabzWuvFoFSqgdefzvbXFMPuDg8WeMfV2exiUO63IpnM1Lvv0i1R-SPVUd</recordid><startdate>198402</startdate><enddate>198402</enddate><creator>Elthon, Don</creator><creator>Scarfe, Christopher M</creator><general>Mineralogical Society of America</general><scope/></search><sort><creationdate>198402</creationdate><title>High-pressure phase equilibria of a high-magnesia basalt and the genesis of primary oceanic basalts</title><author>Elthon, Don ; Scarfe, Christopher M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a212t-11bcad9d987b5471e5f238ee564c545880851620d90417e11fc84e9d93939a313</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>Baffin Bay</topic><topic>basalts</topic><topic>Betts Cove Ophiolite</topic><topic>Canada</topic><topic>chain silicates</topic><topic>clinopyroxene</topic><topic>composition</topic><topic>crust</topic><topic>Eastern Canada</topic><topic>feldspar group</topic><topic>framework silicates</topic><topic>garnet</topic><topic>Gorgona Island</topic><topic>high pressure</topic><topic>igneous and metamorphic rocks</topic><topic>igneous rocks</topic><topic>Lewis Hills Ophiolite</topic><topic>magmas</topic><topic>mantle</topic><topic>nesosilicates</topic><topic>Northwest Territories</topic><topic>olivine</topic><topic>olivine group</topic><topic>Ordovician</topic><topic>orthopyroxene</topic><topic>orthosilicates</topic><topic>oxides</topic><topic>Paleozoic</topic><topic>petrology</topic><topic>phase equilibria</topic><topic>plagioclase</topic><topic>pressure</topic><topic>pyroxene group</topic><topic>Quebec</topic><topic>silicates</topic><topic>spinel</topic><topic>Tortuga Ophiolite</topic><topic>Ungava</topic><topic>volcanic rocks</topic><topic>Western Canada</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Elthon, Don</creatorcontrib><creatorcontrib>Scarfe, Christopher M</creatorcontrib><jtitle>The American mineralogist</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Elthon, Don</au><au>Scarfe, Christopher M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>High-pressure phase equilibria of a high-magnesia basalt and the genesis of primary oceanic basalts</atitle><jtitle>The American mineralogist</jtitle><date>1984-02</date><risdate>1984</risdate><volume>69</volume><issue>1-2</issue><spage>1</spage><epage>15</epage><pages>1-15</pages><issn>0003-004X</issn><eissn>1945-3027</eissn><abstract>High-P phase equilibria studies on a high-MgO basalt from the Tortuga ophiolite complex indicate that olivine + orthopyroxene + clinopyroxene + garnet are its liquidus phases at 25 kbar. The data are combined with results obtained on other tholeiitic basalt compositions, and are used to construct pseudoliquidus phase diagrams for evaluating and predicting the nature of primary magmas and melting of the mantle at high P.</abstract><pub>Mineralogical Society of America</pub><tpages>15</tpages></addata></record>
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subjects Baffin Bay
basalts
Betts Cove Ophiolite
Canada
chain silicates
clinopyroxene
composition
crust
Eastern Canada
feldspar group
framework silicates
garnet
Gorgona Island
high pressure
igneous and metamorphic rocks
igneous rocks
Lewis Hills Ophiolite
magmas
mantle
nesosilicates
Northwest Territories
olivine
olivine group
Ordovician
orthopyroxene
orthosilicates
oxides
Paleozoic
petrology
phase equilibria
plagioclase
pressure
pyroxene group
Quebec
silicates
spinel
Tortuga Ophiolite
Ungava
volcanic rocks
Western Canada
title High-pressure phase equilibria of a high-magnesia basalt and the genesis of primary oceanic basalts
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