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A fractal theory approach to the initial examination of normal faulting in Central Corinthian Gulf, Greece

机译:分形理论方法对希腊科林斯海湾中部正断层的初步检查

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An application of fractal theory in geological formations in the central Corinthian Gulf, Greece, is presented in an attempt to study the nature of presently active deformation. Fault patterns are approximated under the perspective of fractal theory concept, leading to the conclusion that fractal approach can be considered valid for the region of study. Nevertheless, homogeneity may be expected with the reservation that there are no considerable changes in the viscosities of the ductile layers in the region, so that the characteristic exponent b+1-a is less than zero.
机译:分形理论在希腊科林斯海湾中部地质构造中的应用,旨在研究当前活动变形的性质。分形理论概念下的断层模式是近似的,得出的结论是,分形方法可以被认为对研究区域是有效的。然而,在保留该区域的延展层的粘度没有显着变化的情况下,可以期望均匀性,使得特征指数b + 1-a小于零。

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