K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc
New U–Pb radiometric dates for K-bentonite horizons within the Lower Cambrian to Middle Ordovician platform carbonates from the Precordillera terrane of NW Argentina provide further constraints on models for the allochthonous or parautochthonous accretion of this terrane. Two K-bentonite layers from...
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Formato: | Articulo |
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2004
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Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/128923 |
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I19-R120-10915-128923 |
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institution |
Universidad Nacional de La Plata |
institution_str |
I-19 |
repository_str |
R-120 |
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SEDICI (UNLP) |
language |
Inglés |
topic |
Ciencias Naturales Geología U–Pb SHRIMP Ordovician Gondwana terranes |
spellingShingle |
Ciencias Naturales Geología U–Pb SHRIMP Ordovician Gondwana terranes Fanning, Christopher Pankhurst, Robert J. Rapela, Carlos Washington Baldo, Edgardo G. Casquet, César Galindo, Carmen K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
topic_facet |
Ciencias Naturales Geología U–Pb SHRIMP Ordovician Gondwana terranes |
description |
New U–Pb radiometric dates for K-bentonite horizons within the Lower Cambrian to Middle Ordovician platform carbonates from the Precordillera terrane of NW Argentina provide further constraints on models for the allochthonous or parautochthonous accretion of this terrane. Two K-bentonite layers from the Talacasto section yield indistinguishable sensitive high-resolution ion microprobe (SHRIMP) U–Pb zircon dates of 469.5 ± 3.2 Ma and 470.1 ± 3.3 Ma respectively. These are within uncertainty of the U–Pb SHRIMP zircon date of 468.3 ± 3.4 Ma for a porphyritic rhyolite from the Famatinian magmatic arc, Sierra de las Planchadas, near Rio Chaschuil. Geochemical and isotope data also demonstrate the similarity of the K-bentonite and Chaschuil rhyolite parent magmas. Thus, it is highly probable that the Famatinian arc volcanoes provided the ash for the K-bentonite horizons, suggesting proximity to the Precordillera terrane during the deposition of the Lower Cambrian to Middle Ordovician platform carbonates. This implication supports a mid-Ordovician collision model, but could also be compatible with a parautochthonous model for docking of the Precordillera terrane, by movement along the Pacific margin of Gondwana, rather than across the Iapetus Ocean. |
format |
Articulo Articulo |
author |
Fanning, Christopher Pankhurst, Robert J. Rapela, Carlos Washington Baldo, Edgardo G. Casquet, César Galindo, Carmen |
author_facet |
Fanning, Christopher Pankhurst, Robert J. Rapela, Carlos Washington Baldo, Edgardo G. Casquet, César Galindo, Carmen |
author_sort |
Fanning, Christopher |
title |
K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
title_short |
K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
title_full |
K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
title_fullStr |
K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
title_full_unstemmed |
K-bentonites in the Argentine Precordillera contemporaneous with rhyolite volcanism in the Famatinian Arc |
title_sort |
k-bentonites in the argentine precordillera contemporaneous with rhyolite volcanism in the famatinian arc |
publishDate |
2004 |
url |
http://sedici.unlp.edu.ar/handle/10915/128923 |
work_keys_str_mv |
AT fanningchristopher kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc AT pankhurstrobertj kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc AT rapelacarloswashington kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc AT baldoedgardog kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc AT casquetcesar kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc AT galindocarmen kbentonitesintheargentineprecordilleracontemporaneouswithrhyolitevolcanisminthefamatinianarc |
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Repositorios |
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1764820451685564418 |