Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites:
A composite intrusive igneous complex in the central mountain range of Queen Maud Land (Thor Range), Antarctica, displays charac-teristic features of anorogenic granites. A suite of massive intrusives and various sets of dykes and satellite intrusions are ferroan, alkalic to alkali–calcic, and weakl...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.555.2256 2023-05-15T13:38:27+02:00 Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: The Thor Range Kurt Bucher B. Ronald Frost The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.2256 http://petrology.oxfordjournals.org/content/47/3/567.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.2256 http://petrology.oxfordjournals.org/content/47/3/567.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://petrology.oxfordjournals.org/content/47/3/567.full.pdf text 2003 ftciteseerx 2016-01-08T11:44:40Z A composite intrusive igneous complex in the central mountain range of Queen Maud Land (Thor Range), Antarctica, displays charac-teristic features of anorogenic granites. A suite of massive intrusives and various sets of dykes and satellite intrusions are ferroan, alkalic to alkali–calcic, and weakly peraluminous. An early set of plutons consists of charnockitic alkali-granites; a later group of plutons comprises fayalite Qtz-syenites. Coarse mesoperthite is the dominant mineral in all rocks, quartz is abundant and plagioclase is a minor mineral. Olivine (fayalite) is the characteristic mafic mineral, but subcalcic augite and occasionally pigeonite or orthopyroxene are present. In most samples, amphibole is the dominant mafic mineral and its composition is close to end-member hastingsite. It contains high concentrations of F and Cl. Some samples contain igneous fluorite. Thermobarometry suggests a temperature of 900 25C and a pressure of 04 01GPa for the crystallization conditions Text Antarc* Antarctica Queen Maud Land Unknown Queen Maud Land ENVELOPE(12.000,12.000,-72.500,-72.500) |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
A composite intrusive igneous complex in the central mountain range of Queen Maud Land (Thor Range), Antarctica, displays charac-teristic features of anorogenic granites. A suite of massive intrusives and various sets of dykes and satellite intrusions are ferroan, alkalic to alkali–calcic, and weakly peraluminous. An early set of plutons consists of charnockitic alkali-granites; a later group of plutons comprises fayalite Qtz-syenites. Coarse mesoperthite is the dominant mineral in all rocks, quartz is abundant and plagioclase is a minor mineral. Olivine (fayalite) is the characteristic mafic mineral, but subcalcic augite and occasionally pigeonite or orthopyroxene are present. In most samples, amphibole is the dominant mafic mineral and its composition is close to end-member hastingsite. It contains high concentrations of F and Cl. Some samples contain igneous fluorite. Thermobarometry suggests a temperature of 900 25C and a pressure of 04 01GPa for the crystallization conditions |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
The Thor Range Kurt Bucher B. Ronald Frost |
spellingShingle |
The Thor Range Kurt Bucher B. Ronald Frost Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
author_facet |
The Thor Range Kurt Bucher B. Ronald Frost |
author_sort |
The Thor Range |
title |
Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
title_short |
Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
title_full |
Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
title_fullStr |
Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
title_full_unstemmed |
Fluid Transfer in High-grade Metamorphic Terrains Intruded by Anorogenic Granites: |
title_sort |
fluid transfer in high-grade metamorphic terrains intruded by anorogenic granites: |
publishDate |
2003 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.2256 http://petrology.oxfordjournals.org/content/47/3/567.full.pdf |
long_lat |
ENVELOPE(12.000,12.000,-72.500,-72.500) |
geographic |
Queen Maud Land |
geographic_facet |
Queen Maud Land |
genre |
Antarc* Antarctica Queen Maud Land |
genre_facet |
Antarc* Antarctica Queen Maud Land |
op_source |
http://petrology.oxfordjournals.org/content/47/3/567.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.2256 http://petrology.oxfordjournals.org/content/47/3/567.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766106455647191040 |