Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina)
Amphibole ± phlogopite ± apatite-bearing mantle xenoliths at Gobernador Gregores display modal, bulk-rock and phase geochemical characteristics held as indicators of carbonatitic metasomatism. However, part of these xenoliths has high TiO₂/Al₂O3 and those displaying the most pronounced carbonatitic...
Autores principales: | , , , , |
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Formato: | Articulo |
Lenguaje: | Inglés |
Publicado: |
2004
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Materias: | |
Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/134912 |
Aporte de: |
id |
I19-R120-10915-134912 |
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record_format |
dspace |
institution |
Universidad Nacional de La Plata |
institution_str |
I-19 |
repository_str |
R-120 |
collection |
SEDICI (UNLP) |
language |
Inglés |
topic |
Ciencias Naturales High Field Strength Element Geochemical Variation Light Rare Earth Element Metasomatic Agent Modal Trend |
spellingShingle |
Ciencias Naturales High Field Strength Element Geochemical Variation Light Rare Earth Element Metasomatic Agent Modal Trend Rivalenti, Giorgio Zanetti, Alberto Mazzucchelli, Maurizio Vannucci, Riccardo Cingolani, Carlos Alberto Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
topic_facet |
Ciencias Naturales High Field Strength Element Geochemical Variation Light Rare Earth Element Metasomatic Agent Modal Trend |
description |
Amphibole ± phlogopite ± apatite-bearing mantle xenoliths at Gobernador Gregores display modal, bulk-rock and phase geochemical characteristics held as indicators of carbonatitic metasomatism. However, part of these xenoliths has high TiO₂/Al₂O3 and those displaying the most pronounced carbonatitic geochemical markers modally trend towards harzburgite. Bulk-rock, clinopyroxene and amphibole show Zr, Hf and Ti negative anomalies, which increase at decreasing Na₂O and high field strength elements (HFSE) concentrations. Steady variation trends between xenoliths which have and do not have carbonatitic characteristics suggest a control by reactive porous flow of only one agent, inferred to be initially a ne-normative hydrous basalt (because of the presence of wehrlites) evolving towards silica saturation. Variation trends exhibit cusps when amphibole appears in the mode. Appearance of amphibole may explain the Ti anomaly variations, but not those of Zr and Hf. Numerical modelling [Plate Model (Vernieres et al. in J Geophys Res 102:24771–24784, 1997)] gives results consistent with the observed geochemical features by assuming the presence of loveringite. Modest HFSE anomalies in the infiltrating melt may be acquired during percolation in the garnet-facies. |
format |
Articulo Articulo |
author |
Rivalenti, Giorgio Zanetti, Alberto Mazzucchelli, Maurizio Vannucci, Riccardo Cingolani, Carlos Alberto |
author_facet |
Rivalenti, Giorgio Zanetti, Alberto Mazzucchelli, Maurizio Vannucci, Riccardo Cingolani, Carlos Alberto |
author_sort |
Rivalenti, Giorgio |
title |
Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
title_short |
Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
title_full |
Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
title_fullStr |
Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
title_full_unstemmed |
Equivocal carbonatite markers in the mantle xenoliths of the Patagonia backarc: the Gobernador Gregores case (Santa Cruz Province, Argentina) |
title_sort |
equivocal carbonatite markers in the mantle xenoliths of the patagonia backarc: the gobernador gregores case (santa cruz province, argentina) |
publishDate |
2004 |
url |
http://sedici.unlp.edu.ar/handle/10915/134912 |
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bdutipo_str |
Repositorios |
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