AND

ABSTRACT. Black, opaque grains of a spinel whose composition is (Mg2TiO4) 85.8, (MgFe204) 0.4 (FeFe204) 13.8 (mole %) coexist with a MgA1204 spinel and geikielite in a periclase-forsterite marble that has been thermally metamorphosed against an alkalic ultra-mafic intrusion of Caledonian age in the...

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Main Authors: J. Gittins, J. J. Fawcett, J. C. Rucklidge, C. K. Brooks
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.1703
http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.604.1703 2023-05-15T16:03:41+02:00 AND J. Gittins J. J. Fawcett J. C. Rucklidge C. K. Brooks The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.1703 http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.1703 http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf text ftciteseerx 2016-01-08T14:10:26Z ABSTRACT. Black, opaque grains of a spinel whose composition is (Mg2TiO4) 85.8, (MgFe204) 0.4 (FeFe204) 13.8 (mole %) coexist with a MgA1204 spinel and geikielite in a periclase-forsterite marble that has been thermally metamorphosed against an alkalic ultra-mafic intrusion of Caledonian age in the Kangerdlugs-suaq region of East Greenland. The spinel appears to be the closest recorded approach to the end-member Mg2TiO 4 among natural rocks, and to be part of a solid-solution series extending across the join Mg2TiO4-MgFe204-FeFe204, the existence of which has not previously been reported. The composition ofthe series appears to be controlled by thefo2 that prevails during metamorphism. THE compound Mg2TiO4 is a recognized end- Text East Greenland Greenland Unknown Greenland
institution Open Polar
collection Unknown
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language English
description ABSTRACT. Black, opaque grains of a spinel whose composition is (Mg2TiO4) 85.8, (MgFe204) 0.4 (FeFe204) 13.8 (mole %) coexist with a MgA1204 spinel and geikielite in a periclase-forsterite marble that has been thermally metamorphosed against an alkalic ultra-mafic intrusion of Caledonian age in the Kangerdlugs-suaq region of East Greenland. The spinel appears to be the closest recorded approach to the end-member Mg2TiO 4 among natural rocks, and to be part of a solid-solution series extending across the join Mg2TiO4-MgFe204-FeFe204, the existence of which has not previously been reported. The composition ofthe series appears to be controlled by thefo2 that prevails during metamorphism. THE compound Mg2TiO4 is a recognized end-
author2 The Pennsylvania State University CiteSeerX Archives
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author J. Gittins
J. J. Fawcett
J. C. Rucklidge
C. K. Brooks
spellingShingle J. Gittins
J. J. Fawcett
J. C. Rucklidge
C. K. Brooks
AND
author_facet J. Gittins
J. J. Fawcett
J. C. Rucklidge
C. K. Brooks
author_sort J. Gittins
title AND
title_short AND
title_full AND
title_fullStr AND
title_full_unstemmed AND
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url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.1703
http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf
geographic Greenland
geographic_facet Greenland
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genre_facet East Greenland
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op_source http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.1703
http://www.minersoc.org/pages/Archive-MM/Volume_45/45-337-135.pdf
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