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Author Carranza, Emmanuel John M. ♦ Sadeghi, Martiya
Source SpringerLink
Content type Text
Publisher Higher Education Press
File Format PDF
Copyright Year ©2014
Language English
Subject Domain (in DDC) Natural sciences & mathematics ♦ Earth sciences
Subject Keyword fractal ♦ Fry analysis ♦ mineral deposits ♦ structural history ♦ orogenic belts ♦ Earth Sciences
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.
ISSN 20950195
Age Range 18 to 22 years ♦ above 22 year
Educational Use Research
Education Level UG and PG
Learning Resource Type Article
Publisher Date 2014-05-12
Publisher Institution Chinese Universities
Publisher Place Heidelberg
e-ISSN 20950209
Journal Frontiers of Earth Science in China
Volume Number 8
Issue Number 3
Page Count 6
Starting Page 319
Ending Page 324

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Source: SpringerLink