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Post-VMS mineralization deformations (1880-1820 Ma) of the Skellefte district (Sweden): insights from the spatial pattern of VMS occurrences 被引量:1

Post-VMS mineralization deformations (1880-1820 Ma) of the Skellefte district (Sweden): insights from the spatial pattern of VMS occurrences
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摘要 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 post- mineralization 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. 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 post- mineralization 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.
出处 《Frontiers of Earth Science》 SCIE CAS CSCD 2014年第3期319-324,共6页 地球科学前沿(英文版)
关键词 FRACTAL Fry analysis mineral deposits structural history orogenic belts fractal, Fry analysis, mineral deposits, structural history, orogenic belts
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