Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history
The compositions of 17 orthopyroxenes from granulites facies rocks of the Wilson Terrane (Ross Orogen), determined by microprobe analysis, are consistent with a metamorphic origin. Three groups may be distinguished : a) orthopyroxenes with high Al2O3 content (2.85-5.33 weight%) and X(Mg) = 0.46-0.60...
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ftunivsiena:oai:usiena-air.unisi.it:11365/41585 2024-04-21T07:51:54+00:00 Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history TRIBAUDINO, M. TALARICO, F. M. Tribaudino, M. Talarico, F. M. 1992 STAMPA http://hdl.handle.net/11365/41585 https://doi.org/10.1127/ejm/4/3/0453 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:A1992HW81500004 volume:4 issue:3 firstpage:453 lastpage:463 numberofpages:11 journal:EUROPEAN JOURNAL OF MINERALOGY http://hdl.handle.net/11365/41585 doi:10.1127/ejm/4/3/0453 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0026452878 ORTHO-PYROXENE GRANULITE CRYSTAL CHEMISTRY COOLING HISTORY ANTARCTICA info:eu-repo/semantics/article 1992 ftunivsiena https://doi.org/10.1127/ejm/4/3/0453 2024-03-28T00:44:46Z The compositions of 17 orthopyroxenes from granulites facies rocks of the Wilson Terrane (Ross Orogen), determined by microprobe analysis, are consistent with a metamorphic origin. Three groups may be distinguished : a) orthopyroxenes with high Al2O3 content (2.85-5.33 weight%) and X(Mg) = 0.46-0.60, from garnet-cordierite granulites b) orthopyroxenes with low Al2O3 (less than 0.9 wt%) and X(Mg) = 0.49-0.62, from enderbites c) orthopyroxenes with very low Al2O3 (less than 0.4 wt%) and X(Mg) = 0.70, from two-pyroxene mafic granulites. These differences do not reflect different metamorphic conditions, but are due to local mineral assemblages. Zoning occurs in few orthopyroxenes from garnet-cordierite and mafic granulites, in both cases due to a retro-grade evolution. The crystal chemistry and site populations of two Al-rich and one Al-poor specimen were determined by X-ray single crystal diffraction. The most relevant structural differences are the decrease in M1 and M2 polyhedral dimensions, and an increase in TB, both induced by Al. The high degree of Fe2+-Mg order (k(D) between 0.017 and 0.023) is coherent with slow cooling. Closure temperatures of the ordering process are between 214-degrees and 243-degrees-C, with cooling rates in the range expected for a regional metamorphic terrane. Article in Journal/Newspaper Antarc* Antarctica Victoria Land Università degli Studi di Siena: USiena air European Journal of Mineralogy 4 3 453 464 |
institution |
Open Polar |
collection |
Università degli Studi di Siena: USiena air |
op_collection_id |
ftunivsiena |
language |
English |
topic |
ORTHO-PYROXENE GRANULITE CRYSTAL CHEMISTRY COOLING HISTORY ANTARCTICA |
spellingShingle |
ORTHO-PYROXENE GRANULITE CRYSTAL CHEMISTRY COOLING HISTORY ANTARCTICA TRIBAUDINO, M. TALARICO, F. M. Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
topic_facet |
ORTHO-PYROXENE GRANULITE CRYSTAL CHEMISTRY COOLING HISTORY ANTARCTICA |
description |
The compositions of 17 orthopyroxenes from granulites facies rocks of the Wilson Terrane (Ross Orogen), determined by microprobe analysis, are consistent with a metamorphic origin. Three groups may be distinguished : a) orthopyroxenes with high Al2O3 content (2.85-5.33 weight%) and X(Mg) = 0.46-0.60, from garnet-cordierite granulites b) orthopyroxenes with low Al2O3 (less than 0.9 wt%) and X(Mg) = 0.49-0.62, from enderbites c) orthopyroxenes with very low Al2O3 (less than 0.4 wt%) and X(Mg) = 0.70, from two-pyroxene mafic granulites. These differences do not reflect different metamorphic conditions, but are due to local mineral assemblages. Zoning occurs in few orthopyroxenes from garnet-cordierite and mafic granulites, in both cases due to a retro-grade evolution. The crystal chemistry and site populations of two Al-rich and one Al-poor specimen were determined by X-ray single crystal diffraction. The most relevant structural differences are the decrease in M1 and M2 polyhedral dimensions, and an increase in TB, both induced by Al. The high degree of Fe2+-Mg order (k(D) between 0.017 and 0.023) is coherent with slow cooling. Closure temperatures of the ordering process are between 214-degrees and 243-degrees-C, with cooling rates in the range expected for a regional metamorphic terrane. |
author2 |
Tribaudino, M. Talarico, F. M. |
format |
Article in Journal/Newspaper |
author |
TRIBAUDINO, M. TALARICO, F. M. |
author_facet |
TRIBAUDINO, M. TALARICO, F. M. |
author_sort |
TRIBAUDINO, M. |
title |
Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
title_short |
Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
title_full |
Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
title_fullStr |
Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
title_full_unstemmed |
Orthopyroxenes from granulite rocks of the Wilson Terrane (Victoria Land, Antarctica): crystal chemistry and cooling history |
title_sort |
orthopyroxenes from granulite rocks of the wilson terrane (victoria land, antarctica): crystal chemistry and cooling history |
publishDate |
1992 |
url |
http://hdl.handle.net/11365/41585 https://doi.org/10.1127/ejm/4/3/0453 |
genre |
Antarc* Antarctica Victoria Land |
genre_facet |
Antarc* Antarctica Victoria Land |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:A1992HW81500004 volume:4 issue:3 firstpage:453 lastpage:463 numberofpages:11 journal:EUROPEAN JOURNAL OF MINERALOGY http://hdl.handle.net/11365/41585 doi:10.1127/ejm/4/3/0453 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0026452878 |
op_doi |
https://doi.org/10.1127/ejm/4/3/0453 |
container_title |
European Journal of Mineralogy |
container_volume |
4 |
container_issue |
3 |
container_start_page |
453 |
op_container_end_page |
464 |
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