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      New high-precision 40Ar/39Ar ages for the Serra do Mar alkaline magmatism in the São Sebastião Island, SE Brazil, and implications

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          Abstract

          Abstract We present new high-resolution 40Ar/39Ar ages for alkaline layered gabbros and cross-cutting mafic-ultramafic and felsic dykes from the São Sebastião Island, in the northern sector of the Serra do Mar Alkaline Province, São Paulo, Brazil. Duplicate analysis of single kaersutite crystals yielded plateau ages of 88 ± 1 and 87.9 ± 0.8 Ma for a gabbro and 87 ± 1 and 86.0 ± 0.8 Ma for a picrite dyke. Two biotite aliquots from a trachyte yielded ages of 86.0 ± 0.5 and 86.2 ± 0.5 Ma, while an alkali feldspar concentrate yielded ages of 86.0 ± 0.5 Ma. The similar ages obtained for minerals with contrasting closure temperatures suggest that the results are crystallization ages and that the rocks were emplaced at shallow crustal levels. Our results, along with available high-resolution data, point to a relatively narrow time span (ca. 88-85 ± 0.6 Ma) for the entire alkaline magmatism on the island. Other alkaline occurrences both nearby and in the continent’s interior reveal similar ages, reinforcing the hypothesis that mantle decompression and upwelling of heterogeneous mantle sources led to crustal extension and fast ascension of a variety of alkaline magma types in this segment of South America.

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          Most cited references74

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          Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology

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            Magmatism at rift zones: The generation of volcanic continental margins and flood basalts

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              Synchronizing rock clocks of Earth history.

              Calibration of the geological time scale is achieved by independent radioisotopic and astronomical dating, but these techniques yield discrepancies of approximately 1.0% or more, limiting our ability to reconstruct Earth history. To overcome this fundamental setback, we compared astronomical and 40Ar/39Ar ages of tephras in marine deposits in Morocco to calibrate the age of Fish Canyon sanidine, the most widely used standard in 40Ar/39Ar geochronology. This calibration results in a more precise older age of 28.201 +/- 0.046 million years ago (Ma) and reduces the 40Ar/39Ar method's absolute uncertainty from approximately 2.5 to 0.25%. In addition, this calibration provides tight constraints for the astronomical tuning of pre-Neogene successions, resulting in a mutually consistent age of approximately 65.95 Ma for the Cretaceous/Tertiary boundary.
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                Author and article information

                Journal
                bjgeo
                Brazilian Journal of Geology
                Braz. J. Geol.
                Sociedade Brasileira de Geologia (São Paulo, SP, Brazil )
                2317-4889
                2317-4692
                2021
                : 51
                : 4
                : e20210046
                Affiliations
                [1] São Paulo São Paulo orgnameUniversidade de São Paulo orgdiv1Institute of Geosciences Brazil mariageologa@ 123456gmail.com
                [2] Brisbane Queensland orgnameUniversity of Queensland orgdiv1School of Earth and Environmental Sciences Australia p.vasconcelos@ 123456uq.edu.au
                Article
                S2317-48892021000400304 S2317-4889(21)05100400304
                10.1590/2317-4889202120210046
                4b3ce000-a5a3-4df6-bb8a-5acd3a4fa091

                This work is licensed under a Creative Commons Attribution 4.0 International License.

                History
                : 19 June 2021
                : 10 August 2021
                Page count
                Figures: 0, Tables: 0, Equations: 0, References: 81, Pages: 0
                Product

                SciELO Brazil

                Categories
                Article

                40Ar/39Ar geochronology,mafic-ultramafic and felsic alkaline rocks,São Sebastião Island,Serra do Mar Province,SE Brazil

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