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As rock textures reflect the physical conditions and the mechanisms of formation of the rocks, new approaches are used for improving texture analyses, both qualitatively and quantitatively. Pioneer work has recently boosted interest in fractal analysis for quantifying and correlating patterns. Fractal-like patterns relate to a degree of multiscale...

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... spinel less than 1%. The compositional range of the studied peridotites is quite large (Table 1), ranging from opx-enriched rocks to opx-depleted, cpx-enriched rocks, so that some samples are lherzolites according to the IUGS classification (Le Maitre, 2002). ...
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... of the youngest igneous episodes (447-441 Myr) formed the Agardag alkaline lamprophyre dyke complex ( Izokh et al., 2001;Vladimirov et al., 2005;Gibsher et al., 2012). These lamprophyre dykes contain rare mantle xenoliths ( Egorova et al., 2006; Table 1. Mineral compositions (oxides in wt. ...
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... mineral compositions for the spinel-peridotites from Pico Santa Isabel (Table 1) are typical of Phanerozoic man- tle. Olivine has a very restricted compositional range with Mg# {=molar Mg/(Mg + Fe)} varying from 0.90 to 0.91, which is similar to xenoliths worldwide ( Frey and Prinz, 1978;Xu et al., 1996Xu et al., , 1999Ionov, 1998). ...
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... Fe-Mg distribution between olivine and orthopyroxene suggests complete chemical equilibrium. Clinopyroxene is a diopside with Mg# varying from 0.92 to 0.93 and CaO and Al 2 O 3 contents varying from 20.40 to 23.63 wt.% and from 2.73 to 4.71 wt.% respectively (Table 1). Spinel displays quite large variations in Cr# (0.31 to 0.46) from sample to sample but is composition- ally homogeneous at the thin-section scale. ...
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... equilibrium temperatures, for a fixed pressure of 1.5 GPa, obtained by using the mineral major element com- position and the Brey and Köhler thermometer are reported in Table 1 for Bioko mantle xenoliths. The temperature of equilibration for the xenoliths from Bioko Island ranges from 933 °C to 1163 °C (Fig. 3). ...

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... Nevertheless, establishing a relationship between fractal dimension (FD) (a ratio providing a statistical index of complexity) and various geological conditions that control textural pattern remains a challenge. Fractal studies have mostly been limited to silicate minerals [24][25][26][27][28][29] . Not much work has been done on the fractal nature of sulphides and specifically their textures [30][31][32] , in spite of the fact that they reveal a lot of information about the geological setting and conditions of formation of a mineral deposit. ...
... Recently we have noticed the renascence of application of the fractal dimension: in geology (Nkono et al., 2015), materials science (Lashgari et al., 2015), novel pharmaceutics Demetzos, 2014, 2015), medicine (Nakatsuka et al., 2015;Dedović et al., 2015;Lennon et al., 2015;Gokilavani and Vanitha, 2015;Smitha and Narayanan, 2015;Lawrence et al., 2015), etc. Examples of such recent applications are described in detail below. ...
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Article
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Article
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Article
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Chapter
This work investigates the use of Dirichlet series in the modeling of texture images, with application in image classification. The proposed model is based on a strategy that associates each pixel with its corresponding color (gray level in our case) to a vertex of a complex network and the gray level dissimilarity within neighbor pixels with edge weights. The degree distribution of such network is known to be very effective in providing image descriptors. Here, we propose an improvement over this technique, by working on this distribution as a Dirichlet (exponential) series and varying the exponential parameter. A family of statistical measures are extracted from the series and compose a feature vector employed here for texture image classification. In our tests, the achieved accuracy is promising when compared with other state-of-the-art approaches in different databases classically used for benchmark purposes.