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    A regional scale gravity survey of the Southern Cross Greenstone Belt, Western Australia

    Access Status
    Fulltext not available
    Authors
    Rout, D.
    Dentith, M.
    Featherstone, Will
    Date
    1995
    Type
    Journal Article
    
    Metadata
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    Citation
    Rout, David and Dentith, Michael and Featherstone, Will. 1995. A regional scale gravity survey of the Southern Cross Greenstone Belt, Western Australia. Exploration Geophysics 26 (3): pp. 233-240.
    Source Title
    Exploration Geophysics
    DOI
    10.1071/EG995233
    ISSN
    08123985
    Faculty
    Department of Exploration Geophysics
    Faculty of Science and Engineering
    WA School of Mines
    School
    Department of Spatial Sciences
    URI
    http://hdl.handle.net/20.500.11937/14298
    Collection
    • Curtin Research Publications
    Abstract

    A case study is presented from the Southern Cross Greenstone Belt, Western Australia, where regional scale gravity data have been collected in order to study the belt and associated granitoid bodies. Differential Global Positioning System (GPS) satellite surveying techniques have been used to coordinate the gravity observations, and automated processing techniques, such as terrain corrections based on digital elevation models (DEMs), have been used as part of the study. These approaches greatly reduce the manual effort and time needed to collect and process the gravity data. While the use of GPS methods introduces further considerations in data reduction, such as the geoid-spheroid separation, it can provide up to a 250% increase in efficiency in the field while collecting survey data. The computer based terrain correction calculation using a DEM provides a considerable saving in the time expended on data reduction. With the introduction of such field practices and reduction methods, gravity as a semi-regional scale exploration tool is becoming more attractive. The present study has shown that station spacings of 1 km should be considered a maximum when working on the semi-regional scale (50?60 km square areas), with closer station spacings (500 m maximum) more appropriate close to expected geological contacts.

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