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Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica; constraints from melt...

Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica; constraints from melt...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2493590053

Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica; constraints from melt inclusions and thermodynamic modeling

About this item

Full title

Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica; constraints from melt inclusions and thermodynamic modeling

Publisher

Washington: Mineralogical Society of America

Journal title

The American mineralogist, 2018-04, Vol.103 (4), p.610-622

Language

English

Formats

Publication information

Publisher

Washington: Mineralogical Society of America

More information

Scope and Contents

Contents

In the Pan-African belt of the Dronning Maud Land, Antarctica, crystallized melt inclusions (nanogranitoids) occur in garnet from ultramafic granulites. The granulites contain the peak assemblage pargasite+garnet+clinopyroxene with rare relict orthopyroxene and biotite, and retrograde symplectites at contacts between garnet and amphibole. Garnet co...

Alternative Titles

Full title

Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica; constraints from melt inclusions and thermodynamic modeling

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2493590053

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2493590053

Other Identifiers

ISSN

0003-004X

E-ISSN

1945-3027

DOI

10.2138/am-2018-6214

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