High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry
This study explores the origin and geochemical evolution of apatite, monazite, and xenotime along two metamorphic traverses. The first, from the Kigluaik Mountains, Seward Peninsula, Alaska, consists of a localized (85 cm) orthopyroxene–clinopyroxene-bearing dehydration zone. The second consists of...
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2002
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fthighwire:oai:open-archive.highwire.org:petrology:43/5/801 2023-05-15T18:19:18+02:00 High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry HARLOV, DANIEL E. FÖRSTER, HANS-JÜRGEN 2002-05-01 00:00:00.0 text/html http://petrology.oxfordjournals.org/cgi/content/short/43/5/801 https://doi.org/10.1093/petrology/43.5.801 en eng Oxford University Press http://petrology.oxfordjournals.org/cgi/content/short/43/5/801 http://dx.doi.org/10.1093/petrology/43.5.801 Copyright (C) 2002, Oxford University Press ARTICLES TEXT 2002 fthighwire https://doi.org/10.1093/petrology/43.5.801 2013-05-27T15:51:18Z This study explores the origin and geochemical evolution of apatite, monazite, and xenotime along two metamorphic traverses. The first, from the Kigluaik Mountains, Seward Peninsula, Alaska, consists of a localized (85 cm) orthopyroxene–clinopyroxene-bearing dehydration zone. The second consists of orthopyroxene ± clinopyroxene-bearing granulite facies metabasite layers interlayered with metapelites over a 3–4 km traverse, along the Val Strona, Ivrea–Verbano Zone, Northern Italy (IVZ). In both dehydration zones small Th- and U-poor inclusions of monazite and/or xenotime occur in the apatite. These inclusions are metasomatically induced and nucleated within the apatite via the coupled substitutions Na + + (Y + REE) 3+ = 2 Ca 2+ and Si 4+ + (Y + REE) 3+ = P 5+ + Ca 2+ . These are not present in apatite from the original amphibolite facies gneiss. Apatite, in both dehydration zones, also shows a relative increase in both F and Cl compared with apatite from the amphibolite facies zone. Granulite facies metabasites in the IVZ also contain isolated monazite grains, which range from uniform to complexly zoned in Th the (13–30·1 mol % ThSiO 4 ). These are the product of breakdown and subsequent mobilization of the lanthanides and actinides from monazite-(Ce) in the metapelite layers into the metabasite layers at the start of granulite facies metamorphism. Text Seward Peninsula Alaska HighWire Press (Stanford University) Journal of Petrology 43 5 801 824 |
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ARTICLES HARLOV, DANIEL E. FÖRSTER, HANS-JÜRGEN High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
topic_facet |
ARTICLES |
description |
This study explores the origin and geochemical evolution of apatite, monazite, and xenotime along two metamorphic traverses. The first, from the Kigluaik Mountains, Seward Peninsula, Alaska, consists of a localized (85 cm) orthopyroxene–clinopyroxene-bearing dehydration zone. The second consists of orthopyroxene ± clinopyroxene-bearing granulite facies metabasite layers interlayered with metapelites over a 3–4 km traverse, along the Val Strona, Ivrea–Verbano Zone, Northern Italy (IVZ). In both dehydration zones small Th- and U-poor inclusions of monazite and/or xenotime occur in the apatite. These inclusions are metasomatically induced and nucleated within the apatite via the coupled substitutions Na + + (Y + REE) 3+ = 2 Ca 2+ and Si 4+ + (Y + REE) 3+ = P 5+ + Ca 2+ . These are not present in apatite from the original amphibolite facies gneiss. Apatite, in both dehydration zones, also shows a relative increase in both F and Cl compared with apatite from the amphibolite facies zone. Granulite facies metabasites in the IVZ also contain isolated monazite grains, which range from uniform to complexly zoned in Th the (13–30·1 mol % ThSiO 4 ). These are the product of breakdown and subsequent mobilization of the lanthanides and actinides from monazite-(Ce) in the metapelite layers into the metabasite layers at the start of granulite facies metamorphism. |
format |
Text |
author |
HARLOV, DANIEL E. FÖRSTER, HANS-JÜRGEN |
author_facet |
HARLOV, DANIEL E. FÖRSTER, HANS-JÜRGEN |
author_sort |
HARLOV, DANIEL E. |
title |
High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
title_short |
High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
title_full |
High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
title_fullStr |
High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
title_full_unstemmed |
High-Grade Fluid Metasomatism on both a Local and a Regional Scale: the Seward Peninsula, Alaska, and the Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate Mineral Chemistry |
title_sort |
high-grade fluid metasomatism on both a local and a regional scale: the seward peninsula, alaska, and the val strona di omegna, ivrea-verbano zone, northern italy. part ii: phosphate mineral chemistry |
publisher |
Oxford University Press |
publishDate |
2002 |
url |
http://petrology.oxfordjournals.org/cgi/content/short/43/5/801 https://doi.org/10.1093/petrology/43.5.801 |
genre |
Seward Peninsula Alaska |
genre_facet |
Seward Peninsula Alaska |
op_relation |
http://petrology.oxfordjournals.org/cgi/content/short/43/5/801 http://dx.doi.org/10.1093/petrology/43.5.801 |
op_rights |
Copyright (C) 2002, Oxford University Press |
op_doi |
https://doi.org/10.1093/petrology/43.5.801 |
container_title |
Journal of Petrology |
container_volume |
43 |
container_issue |
5 |
container_start_page |
801 |
op_container_end_page |
824 |
_version_ |
1766196379790606336 |