Evolution of the Skaergaard magma: Evidence from crystallized melt inclusions

Evolution of the Skaergaard magma: Evidence from crystallized melt inclusions

Polymineralic aggregates composed of clinopyroxene, iron-titanium oxide minerals, apatite and accessory potassium-feldspar, biotite and amphibole are enclosed in cumulus plagioclase grains in the Middle Zone of the Skaergaard intrusion. The chemistry of the minerals in the aggregates indicates that...

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Veröffentlicht in:Contributions to mineralogy and petrology 1995-07, Vol.120 (3-4), p.265
Hauptverfasser: Hanghoj, Karen, Rosing, Minik T, Brooks, C Kent
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Aggregates
Chemical elements
Chemistry
Geology
Mineralogy
Minerals
Petrology
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creator Hanghoj, Karen
Rosing, Minik T
Brooks, C Kent
description Polymineralic aggregates composed of clinopyroxene, iron-titanium oxide minerals, apatite and accessory potassium-feldspar, biotite and amphibole are enclosed in cumulus plagioclase grains in the Middle Zone of the Skaergaard intrusion. The chemistry of the minerals in the aggregates indicates that they represent inclusions of the contemporaneous melt of the Skaergaard intrusion.
doi_str_mv 10.1007/s004100050074
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subjects Aggregates
Chemical elements
Chemistry
Geology
Mineralogy
Minerals
Petrology
title Evolution of the Skaergaard magma: Evidence from crystallized melt inclusions
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