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    Open Apatite Sr Isotopic System in Low-Temperature Hydrous Regimes

    Access Status
    Open access via publisher
    Authors
    Cao, Mingjian
    Evans, Noreen
    Qin, K.
    Danišík, Martin
    Li, G.
    McInnes, Brent
    Date
    2019
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Cao, M. and Evans, N.J. and Qin, K. and Danišík, M. and Li, G. and McInnes, B.I.A. 2019. Open Apatite Sr Isotopic System in Low-Temperature Hydrous Regimes. Journal of Geophysical Research: Solid Earth. 124 (11): pp. 11192-11203.
    Source Title
    Journal of Geophysical Research: Solid Earth
    DOI
    10.1029/2019JB018085
    ISSN
    2169-9313
    Faculty
    Faculty of Science and Engineering
    School
    John de Laeter Centre (JdLC)
    School of Earth and Planetary Sciences (EPS)
    Funding and Sponsorship
    http://purl.org/au-research/grants/arc/DP160102427
    URI
    http://hdl.handle.net/20.500.11937/90784
    Collection
    • Curtin Research Publications
    Abstract

    Single crystal in situ Sr and Nd isotopic analysis of apatite permits more accurate interrogation of a variety of geoscience questions, including provenance, petrogenesis, and ore system evolution. However, the degree to which the apatite Sr and Nd isotopic systems remain closed under extended low-temperature hydrous conditions is not well constrained. Granitoids at the Baogutu deposit in NW China contain veins of low-temperature H2O-rich epistilbite and thus provide an excellent opportunity to evaluate isotopic system integrity under low-temperature hydrous conditions. Apatite from the Late Carboniferous diorite and granodiorite porphyry show variable (87Sr/86Sr)i ratios (0.7042 to 0.7062) but restricted εNd(t) values (+7.0±0.4 and +6.5±0.4, 1σ). The apatite Sr isotope signatures are transitional between whole rock (0.7035) and vein epistilbite (~0.7062), indicating apparent incorporation of radiogenic Sr from the epistilbite-related hydrothermal fluid into the igneous apatite, whereas εNd values closely match those of the whole rock (+6.9±0.2 and +6.5±0.2, 1σ) and epistilbite (+6.2±0.2, 1σ). Obvious metasomatic textures of apatite were revealed by cathodoluminescence images. The 260 to 300°C formation temperatures for earlier quartz-sulfide veins and chlorite alteration and homogenization temperature (~190°C) of fluid inclusions in epistilbite-calcite vein calcite constrain the temperature of the later epistilbite-related hydrothermal fluid to 190 to 260°C. These results indicate that Sr and likely Nd isotopes in apatite are mobile under low-temperature (<300°C) hydrous conditions and implies that Rb-Sr signatures in apatite from hydrothermally altered rocks reveal the presence and characteristics of modifying fluids.

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