Development of viscous fingering between mafic and felsic magmas: evidence from the Terra Nova Intrusive Complex (Antarctica)

Details Development of viscous fingering between mafic and felsic magmas: evidence from the Terra Nova Intrusive Complex (Antarctica) Development of viscous fingering between mafic and felsic magmas: evidence from the Terra Nova Intrusive Complex (Antarctica)

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005minpe..83..151p&link_type=abstract

Mineralogy and Petrology, Volume 83, Issue 3-4, pp. 151-166

Computer Science

3

Scientific paper

A wide range of types of contact morphology among mafic and felsic magmas are observed in outcrops on Vegetation Island (Terra Nova Intrusive Complex, Antarctica). Image analysis and fractal geometry techniques were applied for in-depth study of the mafic/felsic interface, with the aim of studying the origin of the varied morphologies. In particular, the length (IPN) and fractal dimension (Dbox) of interfaces were measured. Results indicate that there is a close exponential dependence of IPN on Dbox.

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