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    3D reflection seismic investigation for mine planning and exploration in the Kevitsa Ni-Cu-PGE deposit, Northern Finland

    173613_41364_3D reflection seismic investigation for mine planning and exploration in the Kevitsa Ni-Cu-PGE.pdf (5.189Mb)
    Access Status
    Open access
    Authors
    Malehmir, A.
    Juhlin, C.
    Wijns, C.
    Urosevic, Milovan
    Valasti, P.
    Koivisto, E.
    Kukkonen, I.
    Heikkinen, P.
    Paananen, M.
    Date
    2011
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Malehmir, Alireza and Juhlin, Christopher and Wijns, Chris and Urosevic, Milovan and Valasti, Petri and Koivisto, Emilia and Kukkonen, Ilmo and Heikkinen, Pekka and Paananen, Markku. 2011. 3D reflection seismic investigation for mine planning and exploration in the Kevitsa Ni-Cu-PGE deposit, Northern Finland, in Society of Exploration Geophysics (ed), SEG/San Antonio 2011, Sep 18 2011, pp. 1237-1241. San Antonio, Texas: SEG
    Source Title
    SEG Technical Program Expanded Abstracts
    Source Conference
    SEG/San Antonio 2011
    DOI
    10.1190/1.3627427
    ISSN
    1949-4645
    School
    Department of Exploration Geophysics
    Remarks

    A link to the Society's web site is available from the Related Links field.

    Published by the Society of Exploration Geophysicists. © 2011 Society of Exploration Geophysicists.

    URI
    http://hdl.handle.net/20.500.11937/22185
    Collection
    • Curtin Research Publications
    Abstract

    A 3D reflection seismic survey was conducted over an area of about 9 km2 at the Kevitsa Ni-Cu-PGE (platinum group elements) deposit, Northern Finland. The principal objective of the survey was to image major fault and fracture zones at depth. Understanding the geometry of these zones is important for designing a steep open-pit for mining. Initial processing results suggest that the 3D seismic survey has been successful in imaging both gently dipping and steeply dipping reflections as shallow as 50 ms (or about 150 m), many of which correlate with fault systems and lithological contacts observed at the surface. Several new target areas can be identified in the seismic data that require further investigations for their mineralization potential.

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