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    Gravity anomaly grids for the New Zealand region

    Access Status
    Fulltext not available
    Authors
    McCubbine, Jack
    Stagpoole, V.
    Caratori Tontini, F.
    Amos, M.
    Smith, E.
    Winefield, R.
    Date
    2017
    Type
    Journal Article
    
    Metadata
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    Citation
    McCubbine, J. and Stagpoole, V. and Caratori Tontini, F. and Amos, M. and Smith, E. and Winefield, R. 2017. Gravity anomaly grids for the New Zealand region. New Zealand Journal of Geology and Geophysics. 60 (4): pp. 381-391.
    Source Title
    New Zealand Journal of Geology and Geophysics
    DOI
    10.1080/00288306.2017.1346692
    ISSN
    0028-8306
    School
    School of Earth and Planetary Sciences (EPS)
    URI
    http://hdl.handle.net/20.500.11937/73431
    Collection
    • Curtin Research Publications
    Abstract

    © 2017 The Royal Society of New Zealand. We present 1 arc-minute Bouguer, Faye, free air and topography corrected gravity anomaly grids for the New Zealand region, 25°S to 60°S and 160°E to 170°W. The grids were compiled from existing terrestrial, marine and satellite altimetry-derived gravity data enhanced with new airborne gravimetry data that were acquired for improvement of the New Zealand vertical datum. The airborne data seamlessly cover onshore and offshore areas over New Zealand’s North, South and Stewart islands with a uniform flight line spacing of 10 km. All data were corrected for the gravitational effect of the Geodetic Reference System 1980 (GRS80) reference ellipsoid and tied to the International Gravity Standardization Net 1971 (I.G.S.N.71) gravity datum. The gravity anomaly data from all sources were combined using the method of least squares collocation with a three dimensional logarithmic covariance function. Terrain corrections for gravity anomaly grids were calculated using an 8 m digital elevation model for topography above sea level and a 250 m seafloor topography model.

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