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Data processing. (a) Microphotograph of a peridotite thin section. (b) 2D distribution (in black) of orthopyroxene drawn from this thin section. (c) Fractal Dimension (FD) computed at fixed observation window, by varying the resolution (apparent pixel size) ε, and counting the number N(ε) of ε-pixels occupied by the orthopyroxene structure limited by the observation window. The red line represents the theoretical line; the blue line corresponds to the sample analysis. This figure is available in colour online at wileyonlinelibrary.com/journal/gj

Data processing. (a) Microphotograph of a peridotite thin section. (b) 2D distribution (in black) of orthopyroxene drawn from this thin section. (c) Fractal Dimension (FD) computed at fixed observation window, by varying the resolution (apparent pixel size) ε, and counting the number N(ε) of ε-pixels occupied by the orthopyroxene structure limited by the observation window. The red line represents the theoretical line; the blue line corresponds to the sample analysis. This figure is available in colour online at wileyonlinelibrary.com/journal/gj

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Article
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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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Context 1
... of natural and cross-polarized light digital microphotographs. Images of the thin sections were acquired with a digital camera coupled with an optical polarizing microscope to get com- posite photographs of each section through an image editing software. The crystal boundaries have been extracted and/or redrawn through photo-processing softwares (Fig. 2a); the spatial regions occupied by orthopyroxene in a thin section have been delineated (Fig. 2b). The obtained digital images were used for fractal analysis of each sample. ...
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... acquired with a digital camera coupled with an optical polarizing microscope to get com- posite photographs of each section through an image editing software. The crystal boundaries have been extracted and/or redrawn through photo-processing softwares (Fig. 2a); the spatial regions occupied by orthopyroxene in a thin section have been delineated (Fig. 2b). The obtained digital images were used for fractal analysis of each sample. ...
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... is the relationship N(r) ~ r D , where r is a variable radius, N(r) is the number of particles or the mass contained in a ball of radius r, and D is the fractal di- mension (FD). In our case, the texture of a given sample will be characterized by the fractal dimension of the distribution of orthopyroxene grains in the thin section of this sample (Fig. 2b). The FD (Fig. 2c) has been determined using the Fractalyse 2.4.1 software developed within the team 'City, mobility, territory' of ThéMA (Théoriser et Modéliser pour Aménager) of University of Franche-Comté in Bourgogne, France (Frankhauser et al., 2007(Frankhauser et al., , 2008Tarnier et al., 2008aTarnier et al., , 2008b). This ...
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... N(r) ~ r D , where r is a variable radius, N(r) is the number of particles or the mass contained in a ball of radius r, and D is the fractal di- mension (FD). In our case, the texture of a given sample will be characterized by the fractal dimension of the distribution of orthopyroxene grains in the thin section of this sample (Fig. 2b). The FD (Fig. 2c) has been determined using the Fractalyse 2.4.1 software developed within the team 'City, mobility, territory' of ThéMA (Théoriser et Modéliser pour Aménager) of University of Franche-Comté in Bourgogne, France (Frankhauser et al., 2007(Frankhauser et al., , 2008Tarnier et al., 2008aTarnier et al., , 2008b). This software, originally ...
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... structure (box counting method); the log-log plot of N(ε) vs ε would then display a straight line of opposite slope ÀD. The difference between the FD values obtained by the two methods (1) and (2) lies between 0.01 and 0.05, which is very small, so in this paper we con- sider only the values derived by applying the second calcu- lation option (Fig. 2c). Because a rock texture (or the photomicrograph of a thin section) is not a pure fractal (it is not a continuous structure but a discrete one spanning a finite range of scales), it is only possible to get an approximate fractal law, that is, the log- log plot of N(ε) vs ε displays only a roughly straight region, moreover in a finite ...
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... one spanning a finite range of scales), it is only possible to get an approximate fractal law, that is, the log- log plot of N(ε) vs ε displays only a roughly straight region, moreover in a finite range of scales. The slope value D is ob- tained from the best fit, its quality is appreciated by the cor- relation coefficient R (here R 2 = 0.90, Fig. 2c). For more information on the mathematical basis of the method, see the original papers of the ThéMA laboratory (Frankhauser et al., 2007(Frankhauser et al., , 2008Tarnier et al., 2008aTarnier et al., , ...

Citations

... 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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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.