Age and magmatic evolution of the Famatinian granitic rocks of Sierra de Ancasti,

JUAN A. DAHLQUIST; CARLOS W. RAPELA; ROBERT J. PANKHURST; C. MARK FANNING; JEFFREY D. VERVOORT; GARRET HART; EDGARDO G. BALDO; JUAN A. MURRA; PABLO H. ALASINO; FERNANDO COLOMBO

JOURNAL OF SOUTH AMERICAN EARTH SCIENCES

PERGAMON-ELSEVIER SCIENCE LTD

Año: 2011

0895-9811

The granitic rocks of the Sierra de Ancasti represent one of the easternmost outcrops of the Famatinian arc of the Sierras Pampeanas.We report here newUePb SHRIMPand LA-ICP-MSOrdovician ages and a petrological and geochemical study of the Las Cañadas I-type granitic complex in the central sector of Sierra de Ancasti. Numerical modelling indicates that calc-alkaline and metaluminousmonzogranites (SiO2¼69.8e73.0 wt.%) were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 and geochemical study of the Las Cañadas I-type granitic complex in the central sector of Sierra de Ancasti. Numerical modelling indicates that calc-alkaline and metaluminousmonzogranites (SiO2¼69.8e73.0 wt.%) were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 and geochemical study of the Las Cañadas I-type granitic complex in the central sector of Sierra de Ancasti. Numerical modelling indicates that calc-alkaline and metaluminousmonzogranites (SiO2¼69.8e73.0 wt.%) were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 ePb SHRIMPand LA-ICP-MSOrdovician ages and a petrological and geochemical study of the Las Cañadas I-type granitic complex in the central sector of Sierra de Ancasti. Numerical modelling indicates that calc-alkaline and metaluminousmonzogranites (SiO2¼69.8e73.0 wt.%) were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9 2¼69.8e73.0 wt.%) were produced by fractional crystallization of plagioclase-rich tonalite (w60% plagioclase and SiO2 ¼ 60.9w60% plagioclase and SiO2 ¼ 60.9 e62.5 wt.%) from an inferred parental magma of granodioritic composition (SiO2 ¼ 67.4 wt.%). SmeNd isotopic data on the dated rocks indicate a dominant continental crustal input, as reported for other Ordovician granitic rocks (Famatinian magmatism) farther west in the Sierras Pampeanas. Combined ages and isotopic data are consistent with previous studies indicating that Famatinian magmatism was short-lived (w20 Ma) and lacked a significant asthenospheric contribution. The occurrence of inherited zircon and the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. isotopic data on the dated rocks indicate a dominant continental crustal input, as reported for other Ordovician granitic rocks (Famatinian magmatism) farther west in the Sierras Pampeanas. Combined ages and isotopic data are consistent with previous studies indicating that Famatinian magmatism was short-lived (w20 Ma) and lacked a significant asthenospheric contribution. The occurrence of inherited zircon and the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. isotopic data on the dated rocks indicate a dominant continental crustal input, as reported for other Ordovician granitic rocks (Famatinian magmatism) farther west in the Sierras Pampeanas. Combined ages and isotopic data are consistent with previous studies indicating that Famatinian magmatism was short-lived (w20 Ma) and lacked a significant asthenospheric contribution. The occurrence of inherited zircon and the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. 62.5 wt.%) from an inferred parental magma of granodioritic composition (SiO2 ¼ 67.4 wt.%). SmeNd isotopic data on the dated rocks indicate a dominant continental crustal input, as reported for other Ordovician granitic rocks (Famatinian magmatism) farther west in the Sierras Pampeanas. Combined ages and isotopic data are consistent with previous studies indicating that Famatinian magmatism was short-lived (w20 Ma) and lacked a significant asthenospheric contribution. The occurrence of inherited zircon and the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C. w20 Ma) and lacked a significant asthenospheric contribution. The occurrence of inherited zircon and the petrological and geochemical data fromthe Las Cañadas complex indicate that the parental magmawas derived from mixed igneous and sedimentary material in the source or by partial melting of igneous rocks of different ages. Systematic dating of inherited zircon cores is required to clarify this issue. Zircon saturation geothermometrycombined with geochemical data indicates that the onset of zircon crystallization, together with variable amounts of other minerals such as plagioclase, quartz, biotite, oxides and apatite, occurred when the parental magma reached 67 wt.% SiO2 withw440 ppm of Zr at w878 C.2 withw440 ppm of Zr at w878 C.