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Post-VMS mineralization deformations (1880–1820 Ma) of the Skellefte district (Sweden): insights from the spatial pattern of VMS occurrences

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Abstract

In the last two to three decades or so, the spatial pattern of mineral occurrences of a deposit-type has been studied to derive insights to mineralization controls and assist mineral exploration. In the Skellefte district, Fry plots of volcanogenic massive sulfide (VMS) mines/prospects reveal patterns that are likely due to postmineralization deformation events. The fractal dimensions of the spatial patterns of the present-day VMS mines/prospects and that of the ‘original’ VMS deposits support the concept that spatial patterns of mineral deposits are spatially-invariant. Therefore, analysis of the spatial pattern of mineral deposits is useful not only in research about pre- and syn-mineralization geological settings but also post-mineralization geological settings.

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Authors and Affiliations

  1. School of Earth and Environmental Sciences, James Cook University, Townsville, Queensland, 4811, Australia

    Emmanuel John M. Carranza

  2. Geological Survey of Sweden, Villavägen 18, Uppsala, Sweden

    Martiya Sadeghi

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  1. Emmanuel John M. Carranza
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  2. Martiya Sadeghi
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Correspondence to Emmanuel John M. Carranza.

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Carranza, E.J.M., Sadeghi, M. Post-VMS mineralization deformations (1880–1820 Ma) of the Skellefte district (Sweden): insights from the spatial pattern of VMS occurrences. Front. Earth Sci. 8, 319–324 (2014). https://doi.org/10.1007/s11707-014-0466-3

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