element ransport
The North Q6roq syenite centre forms part of the Gardar Province of South Greenland. Extensive metasomatism, associated with the evolution of syenitic magmas, has resulted in redistribution of the rare-earth elements (REE), originally concentrated by magmatic processes, in both the syenites and surr...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.618.1743 2023-05-15T16:27:59+02:00 element ransport David A. Rae Ian M. Coulson Andrew D. Chambers The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.618.1743 http://www.minersoc.org/pages/Archive-MM/Volume_60/60-398-207.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.618.1743 http://www.minersoc.org/pages/Archive-MM/Volume_60/60-398-207.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_60/60-398-207.pdf apatite metasomatism rare-earth elements cathodoluminescence Igaliko Gardar South Greenland text ftciteseerx 2016-01-08T14:50:34Z The North Q6roq syenite centre forms part of the Gardar Province of South Greenland. Extensive metasomatism, associated with the evolution of syenitic magmas, has resulted in redistribution of the rare-earth elements (REE), originally concentrated by magmatic processes, in both the syenites and surrounding granite-gneiss and quartzite country rocks. An important host for REE is apatite which can occur irl significant quantities. Metasomatic apatites how complex, concentric, but irregular patterns of zonation, clearly seen using CL and BSE imaging. This zonation is related to successive pulses of metasomatising fluids. Electron microprobe analysis confirms the presence of significant quantities of REE in the apatites. The dominant 2+ O+ 3+ 4+ cation exchange mechanism proposed is Ca + P ~-- ~ REE + Si. In contrast o apatites from the nearby Ilfmaussaq intrusion, there is no significant Na present in the structure and exchange reactions involving Na + and REE 3+ for Ca 2+ have not occurred. Apatites from the quartzite are fluor-apatites, while those from the granite-gneiss are more Cl-rich. These differences reflect the fact that granite-gneiss apatites are original and modified by metasomatism, whereas, those in the quartzite are metasomatic n origin. REE were probably transported as carbonate, fluoride or fluor-carbonate complexes, and reflect the activity of a F-rich, CO ~-rich fluid phase. Text Greenland Igaliko Unknown Greenland |
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English |
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apatite metasomatism rare-earth elements cathodoluminescence Igaliko Gardar South Greenland |
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apatite metasomatism rare-earth elements cathodoluminescence Igaliko Gardar South Greenland David A. Rae Ian M. Coulson Andrew D. Chambers element ransport |
topic_facet |
apatite metasomatism rare-earth elements cathodoluminescence Igaliko Gardar South Greenland |
description |
The North Q6roq syenite centre forms part of the Gardar Province of South Greenland. Extensive metasomatism, associated with the evolution of syenitic magmas, has resulted in redistribution of the rare-earth elements (REE), originally concentrated by magmatic processes, in both the syenites and surrounding granite-gneiss and quartzite country rocks. An important host for REE is apatite which can occur irl significant quantities. Metasomatic apatites how complex, concentric, but irregular patterns of zonation, clearly seen using CL and BSE imaging. This zonation is related to successive pulses of metasomatising fluids. Electron microprobe analysis confirms the presence of significant quantities of REE in the apatites. The dominant 2+ O+ 3+ 4+ cation exchange mechanism proposed is Ca + P ~-- ~ REE + Si. In contrast o apatites from the nearby Ilfmaussaq intrusion, there is no significant Na present in the structure and exchange reactions involving Na + and REE 3+ for Ca 2+ have not occurred. Apatites from the quartzite are fluor-apatites, while those from the granite-gneiss are more Cl-rich. These differences reflect the fact that granite-gneiss apatites are original and modified by metasomatism, whereas, those in the quartzite are metasomatic n origin. REE were probably transported as carbonate, fluoride or fluor-carbonate complexes, and reflect the activity of a F-rich, CO ~-rich fluid phase. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David A. Rae Ian M. Coulson Andrew D. Chambers |
author_facet |
David A. Rae Ian M. Coulson Andrew D. Chambers |
author_sort |
David A. Rae |
title |
element ransport |
title_short |
element ransport |
title_full |
element ransport |
title_fullStr |
element ransport |
title_full_unstemmed |
element ransport |
title_sort |
element ransport |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.618.1743 http://www.minersoc.org/pages/Archive-MM/Volume_60/60-398-207.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Igaliko |
genre_facet |
Greenland Igaliko |
op_source |
http://www.minersoc.org/pages/Archive-MM/Volume_60/60-398-207.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.618.1743 http://www.minersoc.org/pages/Archive-MM/Volume_60/60-398-207.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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