Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications

We have carried out zircon U-Pb SHRIMP dating and Hf isotope determinations as well as geochemical analyses on three plutonic units of Gondwanan magmatism that crop out in NW Argentina. Two episodes of different age and genesis have been identified. The older one includes gabbros and diorites (Río G...

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Autores principales: Poma, S., Zappettini, E.O., Quenardelle, S., Santos, J.O., Koukharsky, M., Belousova, E., McNaughton, N.
Formato: JOUR
Materias:
Geochemistry
Gondwanan magmatism
Lu-Hf isotope
NW Argentina
U-Pb SHRIMP dating
diorite
gabbro
geochemistry
geodynamics
Gondwana
granitoid
hafnium
isotopic analysis
lutetium
magmatism
mantle source
petrogenesis
SHRIMP dating
tectonic setting
uranium-lead dating
zircon
Andes
Argentina
Cordillera Frontal
Mendoza
San Rafael [Mendoza]
Anisia
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_07187092_v41_n2_p267_Poma
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
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spelling todo:paper_07187092_v41_n2_p267_Poma2023-10-03T15:36:43Z Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications Poma, S. Zappettini, E.O. Quenardelle, S. Santos, J.O. Koukharsky, M. Belousova, E. McNaughton, N. Geochemistry Gondwanan magmatism Lu-Hf isotope NW Argentina U-Pb SHRIMP dating diorite gabbro geochemistry geodynamics Gondwana granitoid hafnium isotopic analysis lutetium magmatism mantle source petrogenesis SHRIMP dating tectonic setting uranium-lead dating zircon Andes Argentina Cordillera Frontal Mendoza San Rafael [Mendoza] Anisia We have carried out zircon U-Pb SHRIMP dating and Hf isotope determinations as well as geochemical analyses on three plutonic units of Gondwanan magmatism that crop out in NW Argentina. Two episodes of different age and genesis have been identified. The older one includes gabbros and diorites (Río Grande Unit) of 267±3 Ma and granitoids (belonging to the Llullaillaco Unit) of 263±1 Ma (late Permian, Guadalupian); the parent magmas were generated in an intraplate environment and derived from an enriched mantle but were subsequently contaminated by crustal components. The younger rocks are granodiorites with arc signature (Chuculaqui Unit) and an age of 247±2 Ma (middle Triassic-Anisian). Hf isotope signature of the units indicates mantle sources as well as crustal components. Hf model ages obtained are consistent with the presence of crustal Mesoproterozoic (mainly Ectasian to Calymnian (TDM(c) =1.24 to 1.44 Ga-negative Hf(T)) and juvenile Cryogenian sources (TDM=0.65 to 0.79 Ga-positive εHf(T)), supporting the idea of a continuous, mostly Mesoproterozoic, basement under the Central Andes, as an extension of the Arequipa-Antofalla massif. The tectonic setting and age of the Gondwanan magmatism in NW Argentina allow to differentiate: a. Permian intra-plate magmatism developed under similar conditions to the upper section of the Choiyoi magmatism exposed in the Frontal Cordillera and San Rafael Block, Argentina; b. Triassic magmatism belonging to a poorly known subduction-related magmatic arc segment of mostly NS trend with evidence of porphyry type mineralization in Chile, allowing to extend this metallotect into Argentina. Fil:Poma, S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Zappettini, E.O. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Quenardelle, S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Koukharsky, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_07187092_v41_n2_p267_Poma
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Geochemistry
Gondwanan magmatism
Lu-Hf isotope
NW Argentina
U-Pb SHRIMP dating
diorite
gabbro
geochemistry
geodynamics
Gondwana
granitoid
hafnium
isotopic analysis
lutetium
magmatism
mantle source
petrogenesis
SHRIMP dating
tectonic setting
uranium-lead dating
zircon
Andes
Argentina
Cordillera Frontal
Mendoza
San Rafael [Mendoza]
Anisia
spellingShingle Geochemistry
Gondwanan magmatism
Lu-Hf isotope
NW Argentina
U-Pb SHRIMP dating
diorite
gabbro
geochemistry
geodynamics
Gondwana
granitoid
hafnium
isotopic analysis
lutetium
magmatism
mantle source
petrogenesis
SHRIMP dating
tectonic setting
uranium-lead dating
zircon
Andes
Argentina
Cordillera Frontal
Mendoza
San Rafael [Mendoza]
Anisia
Poma, S.
Zappettini, E.O.
Quenardelle, S.
Santos, J.O.
Koukharsky, M.
Belousova, E.
McNaughton, N.
Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
topic_facet Geochemistry
Gondwanan magmatism
Lu-Hf isotope
NW Argentina
U-Pb SHRIMP dating
diorite
gabbro
geochemistry
geodynamics
Gondwana
granitoid
hafnium
isotopic analysis
lutetium
magmatism
mantle source
petrogenesis
SHRIMP dating
tectonic setting
uranium-lead dating
zircon
Andes
Argentina
Cordillera Frontal
Mendoza
San Rafael [Mendoza]
Anisia
description We have carried out zircon U-Pb SHRIMP dating and Hf isotope determinations as well as geochemical analyses on three plutonic units of Gondwanan magmatism that crop out in NW Argentina. Two episodes of different age and genesis have been identified. The older one includes gabbros and diorites (Río Grande Unit) of 267±3 Ma and granitoids (belonging to the Llullaillaco Unit) of 263±1 Ma (late Permian, Guadalupian); the parent magmas were generated in an intraplate environment and derived from an enriched mantle but were subsequently contaminated by crustal components. The younger rocks are granodiorites with arc signature (Chuculaqui Unit) and an age of 247±2 Ma (middle Triassic-Anisian). Hf isotope signature of the units indicates mantle sources as well as crustal components. Hf model ages obtained are consistent with the presence of crustal Mesoproterozoic (mainly Ectasian to Calymnian (TDM(c) =1.24 to 1.44 Ga-negative Hf(T)) and juvenile Cryogenian sources (TDM=0.65 to 0.79 Ga-positive εHf(T)), supporting the idea of a continuous, mostly Mesoproterozoic, basement under the Central Andes, as an extension of the Arequipa-Antofalla massif. The tectonic setting and age of the Gondwanan magmatism in NW Argentina allow to differentiate: a. Permian intra-plate magmatism developed under similar conditions to the upper section of the Choiyoi magmatism exposed in the Frontal Cordillera and San Rafael Block, Argentina; b. Triassic magmatism belonging to a poorly known subduction-related magmatic arc segment of mostly NS trend with evidence of porphyry type mineralization in Chile, allowing to extend this metallotect into Argentina.
format JOUR
author Poma, S.
Zappettini, E.O.
Quenardelle, S.
Santos, J.O.
Koukharsky, M.
Belousova, E.
McNaughton, N.
author_facet Poma, S.
Zappettini, E.O.
Quenardelle, S.
Santos, J.O.
Koukharsky, M.
Belousova, E.
McNaughton, N.
author_sort Poma, S.
title Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
title_short Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
title_full Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
title_fullStr Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
title_full_unstemmed Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: Petrogenesis and geodynamic implications
title_sort geochemistry, u-pb shrimp zircon dating and hf isotopes of the gondwanan magmatism in nw argentina: petrogenesis and geodynamic implications
url http://hdl.handle.net/20.500.12110/paper_07187092_v41_n2_p267_Poma
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