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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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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 |
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ftciteseerx |
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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 |
format |
Text |
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 |
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J. Gittins J. J. Fawcett J. C. Rucklidge C. K. Brooks |
author_sort |
J. Gittins |
title |
AND |
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AND |
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AND |
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title_full_unstemmed |
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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 |
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Greenland |
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East Greenland Greenland |
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East Greenland Greenland |
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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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766399377109155840 |