U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile

The Coastal Batholith of south-central Chile between latitudes 33° and 40°S is composed of calc-alkaline granitoids emplaced in a relatively restricted time period. New SHRIMP U-Pb zircon ages on eight quartzdioritic to granitic rocks collected over a distance of 800 km yielded ages between 300 and...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Deckart,Katja, Hervé,Francisco, Fanning,C. Mark, Ramírez,Valeria, Calderón,Mauricio, Godoy,Estanislao
Lenguaje:English
Publicado: Servicio Nacional de Geología y Minería (SERNAGEOMIN) 2014
Materias:
Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062014000100003
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:scielo:S0718-71062014000100003
record_format dspace
spelling oai:scielo:S0718-710620140001000032014-03-24U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central ChileDeckart,KatjaHervé,FranciscoFanning,C. MarkRamírez,ValeriaCalderón,MauricioGodoy,Estanislao Coastal Batholith Pennsylvanian zircons U-Pb Lu-Hf and O isotope geochemistry The Coastal Batholith of south-central Chile between latitudes 33° and 40°S is composed of calc-alkaline granitoids emplaced in a relatively restricted time period. New SHRIMP U-Pb zircon ages on eight quartzdioritic to granitic rocks collected over a distance of 800 km yielded ages between 300 and 320 Ma, Pennsylvanian (late Carboniferous). Lu-Hf isotopic analyses on the same zircon grains have initial εHf(i) values from +1.67 to -5.64. The δ18O ratios for that grains range from 6.4 to 8.6%o. These new isotopic data point to a relative homogeneous source with prominent components of the continental crust. The calculated Mesoproterozoic Depleted Mantel model ages, in addition to the short span of intrusive ages give insights to the position of the proto-Gondwana margin and the changing subduction mechanism at the end of late Paleozoic time.info:eu-repo/semantics/openAccessServicio Nacional de Geología y Minería (SERNAGEOMIN)Andean geology v.41 n.1 20142014-01-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062014000100003en10.5027/andgeoV41n1-a03
institution Scielo Chile
collection Scielo Chile
language English
topic Coastal Batholith
Pennsylvanian
zircons
U-Pb
Lu-Hf and O isotope geochemistry
spellingShingle Coastal Batholith
Pennsylvanian
zircons
U-Pb
Lu-Hf and O isotope geochemistry
Deckart,Katja
Hervé,Francisco
Fanning,C. Mark
Ramírez,Valeria
Calderón,Mauricio
Godoy,Estanislao
U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
description The Coastal Batholith of south-central Chile between latitudes 33° and 40°S is composed of calc-alkaline granitoids emplaced in a relatively restricted time period. New SHRIMP U-Pb zircon ages on eight quartzdioritic to granitic rocks collected over a distance of 800 km yielded ages between 300 and 320 Ma, Pennsylvanian (late Carboniferous). Lu-Hf isotopic analyses on the same zircon grains have initial εHf(i) values from +1.67 to -5.64. The δ18O ratios for that grains range from 6.4 to 8.6%o. These new isotopic data point to a relative homogeneous source with prominent components of the continental crust. The calculated Mesoproterozoic Depleted Mantel model ages, in addition to the short span of intrusive ages give insights to the position of the proto-Gondwana margin and the changing subduction mechanism at the end of late Paleozoic time.
author Deckart,Katja
Hervé,Francisco
Fanning,C. Mark
Ramírez,Valeria
Calderón,Mauricio
Godoy,Estanislao
author_facet Deckart,Katja
Hervé,Francisco
Fanning,C. Mark
Ramírez,Valeria
Calderón,Mauricio
Godoy,Estanislao
author_sort Deckart,Katja
title U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
title_short U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
title_full U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
title_fullStr U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
title_full_unstemmed U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
title_sort u-pb geochronology and hf-o isotopes of zircons from the pennsylvanian coastal batholith, south-central chile
publisher Servicio Nacional de Geología y Minería (SERNAGEOMIN)
publishDate 2014
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062014000100003
work_keys_str_mv AT deckartkatja upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
AT hervefrancisco upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
AT fanningcmark upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
AT ramirezvaleria upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
AT calderonmauricio upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
AT godoyestanislao upbgeochronologyandhfoisotopesofzirconsfromthepennsylvaniancoastalbatholithsouthcentralchile
_version_ 1714205843357958144