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Fractal analysis of mingled/mixed magmas: an example from the Upper Pollara eruption (Salina Island, southern Tyrrhenian Sea, Italy) |
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| Authors: | Rosanna De Rosa Paola Donato Guido Ventura |
| Institution: | a Dipartimento Scienze della Terra, Universita' della Calabria, Ponte P. Bucci, 87036 Arcavacata di Rende (CS), Italy b Dipartimento Scienze della Terra e Geologico-ambientali, Universita' di Bologna, P.zza di Porta S. Donato 1, 40126, Bologna, Italy c Osservatorio Vesuviano, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via Diocleziano, 328, I-80124, Naples, Italy |
| Abstract: | Upper Pollara eruption products (13 ka, Salina Island, Italy) include both homogeneous and heterogeneous pumices resulting from mixing/mingling processes between an HK andesite and a high-SiO2 rhyolite. Representative samples of heterogeneous pumices are collected and analyzed in order to check the correspondence between glass composition and morphological features of the mingling/mixing structures. Image analysis techniques are applied and eight grey color ranges (classes) are extracted from high-resolution scans of pumice. Class 1 (lighter colors) and class 8 (darker colors) show end-member glass compositions, i.e. HK andesite and high-SiO2 rhyolite, respectively. These two classes show spot- to cluster-like morphological structures. Intermediate classes show an HK dacitic to rhyolitic composition and a banding- to fold-like morphology. Fractal analysis by box-counting of the boundary pattern of eight grey classified images is performed over a length scale of 0.028–1.8 cm. Fractal dimension D is between 1.01 and 1.84. Coupled fractal analysis and geochemical data reveal that D increases as the degree of magma interaction (homogenization) increases. This feature well fits the results from numerical models on the convective mixing of fluids driven by thermal convection. We conclude that the increase of D observed in the Upper Pollara samples reflects the transition from fractal mixing to homogenization. End-member magmas (HK andesite and high-SiO2 rhyolite) represent isolated mixing regions, while homogenized magmas represent active mixing regions. In the analyzed pumices, isolated and active mixing regions coexist at scales between 10?4 and 10?2 m. Morphological and compositional features of the Upper Pollara pumices result from turbulence. |
| Keywords: | Mixing Fractals Calcalkaline magmas Aeolian Islands |
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