Mesozoic-Cenozoic evolution of the North Patagonian Batholith in Aysen, southern Chile

R. J. Pankhurst, S. D. Weaver, F. Hervé, P. Larrondo

Resultado de la investigación: Article

155 Citas (Scopus)

Resumen

A detailed Rb-Sr geochronological and geochemical study has been carried out on granitoids of the North Patagonian batholith in Aysen. The results for 25 plutonic bodies reveal a complex age pattern. The principal zones defined are, from west to east: Late Cretaceous (a single 76 Ma pluton), Early Cretaceous (c. 135 Ma), Eocene (c. 45 Ma), and Early Miocene (25-15 Ma), reverting to mid-Cretaceous (120-90 Ma) in the Main Cordillera. The igneous suite is typically metaluminous and calc-alkaline, with hornblende-biotite granodiorite and tonalite dominant, although small bodies of Late Miocene/Pliocene (c. 10-5 Ma) peraluminous leucogranite occur sporadically. Tertiary plutonism extends to gabbroic compositions and is concentrated in the vicinity of the dextral strike-slip Liquine-Ofqui fault zone. The highest initial 87Sr/86Sr ratios (c. 0.7050) occur in the Early Cretaceous group, with a sharp decrease to 0.7034-0.7045 that persists until a Late Miocene reversal to higher values (0.7040-0.7048). These variations are reflected by Nd isotopes, but trends in the εSr(t) v. εNd(t) diagram show that this is not due to contamination from the accretionary complex into which the batholith was emplaced. An origin by melting of mafic crustal underplate and lower crust is suggested for the main magma suite. The discrete episodes of magmatism correlate with significant changes in subduction kinematics.

Idioma originalEnglish
Páginas (desde-hasta)673-694
Número de páginas22
PublicaciónJournal of the Geological Society
Volumen156
N.º4
DOI
EstadoPublished - jul 1999

Huella dactilar

batholith
Cretaceous
Miocene
leucogranite
plutonism
tonalite
granodiorite
cordillera
hornblende
lower crust
pluton
fault zone
magmatism
biotite
Pliocene
Eocene
subduction
melting
kinematics
diagram

ASJC Scopus subject areas

  • Geology

Citar esto

Pankhurst, R. J. ; Weaver, S. D. ; Hervé, F. ; Larrondo, P. / Mesozoic-Cenozoic evolution of the North Patagonian Batholith in Aysen, southern Chile. En: Journal of the Geological Society. 1999 ; Vol. 156, N.º 4. pp. 673-694.
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abstract = "A detailed Rb-Sr geochronological and geochemical study has been carried out on granitoids of the North Patagonian batholith in Aysen. The results for 25 plutonic bodies reveal a complex age pattern. The principal zones defined are, from west to east: Late Cretaceous (a single 76 Ma pluton), Early Cretaceous (c. 135 Ma), Eocene (c. 45 Ma), and Early Miocene (25-15 Ma), reverting to mid-Cretaceous (120-90 Ma) in the Main Cordillera. The igneous suite is typically metaluminous and calc-alkaline, with hornblende-biotite granodiorite and tonalite dominant, although small bodies of Late Miocene/Pliocene (c. 10-5 Ma) peraluminous leucogranite occur sporadically. Tertiary plutonism extends to gabbroic compositions and is concentrated in the vicinity of the dextral strike-slip Liquine-Ofqui fault zone. The highest initial 87Sr/86Sr ratios (c. 0.7050) occur in the Early Cretaceous group, with a sharp decrease to 0.7034-0.7045 that persists until a Late Miocene reversal to higher values (0.7040-0.7048). These variations are reflected by Nd isotopes, but trends in the εSr(t) v. εNd(t) diagram show that this is not due to contamination from the accretionary complex into which the batholith was emplaced. An origin by melting of mafic crustal underplate and lower crust is suggested for the main magma suite. The discrete episodes of magmatism correlate with significant changes in subduction kinematics.",
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Mesozoic-Cenozoic evolution of the North Patagonian Batholith in Aysen, southern Chile. / Pankhurst, R. J.; Weaver, S. D.; Hervé, F.; Larrondo, P.

En: Journal of the Geological Society, Vol. 156, N.º 4, 07.1999, p. 673-694.

Resultado de la investigación: Article

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AU - Weaver, S. D.

AU - Hervé, F.

AU - Larrondo, P.

PY - 1999/7

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N2 - A detailed Rb-Sr geochronological and geochemical study has been carried out on granitoids of the North Patagonian batholith in Aysen. The results for 25 plutonic bodies reveal a complex age pattern. The principal zones defined are, from west to east: Late Cretaceous (a single 76 Ma pluton), Early Cretaceous (c. 135 Ma), Eocene (c. 45 Ma), and Early Miocene (25-15 Ma), reverting to mid-Cretaceous (120-90 Ma) in the Main Cordillera. The igneous suite is typically metaluminous and calc-alkaline, with hornblende-biotite granodiorite and tonalite dominant, although small bodies of Late Miocene/Pliocene (c. 10-5 Ma) peraluminous leucogranite occur sporadically. Tertiary plutonism extends to gabbroic compositions and is concentrated in the vicinity of the dextral strike-slip Liquine-Ofqui fault zone. The highest initial 87Sr/86Sr ratios (c. 0.7050) occur in the Early Cretaceous group, with a sharp decrease to 0.7034-0.7045 that persists until a Late Miocene reversal to higher values (0.7040-0.7048). These variations are reflected by Nd isotopes, but trends in the εSr(t) v. εNd(t) diagram show that this is not due to contamination from the accretionary complex into which the batholith was emplaced. An origin by melting of mafic crustal underplate and lower crust is suggested for the main magma suite. The discrete episodes of magmatism correlate with significant changes in subduction kinematics.

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