Titlebook: Relativistic Gravity Research; With Emphasis on Exp J. Ehlers,G. Schäfer Conference proceedings 1992 Springer-Verlag Berlin Heidelberg 1992

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K. Dorenwendttial equations containing some material-dependent parameters. The relatively general validity of the formalism makes the study of fracture in this intermediate (or mesoscopic) range of length scales particularly attractive to statistical physicists. If the reader wants to know more about recent deve

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Gerhard Schäfer fractal structures that can be produced in the laboratory under controlled circumstances and try to give answers to questions like: How do you make a fractal? How do you determine its structure, in particular the fractal dimension, ... What are the mechanical, electrical, and magnetic properties? I

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K. Danzmann,J. Chen,P. G. Nelson,T. M. Niebauer,A. Rüdiger,R. Schilling,L. Schnupp,K. A. Strain,H. Wsity determined on sedimentary rocks. This fractal model yields tortuosity and effective pore radius as functions of porosity as well as a general permeability-porosity relationship, the coefficients of which are characteristic for different rock types. It can be applied to interpret the diagenetic

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W. Winkler,colleagues of GEOension of fracture—size distribution and the Euclidean space dimension of specimen volume. This relation indicates a constraint of fractal geometry for fragmentation and is expected to be a powerful tool for the fractography analysis in the fields of tectonics and seismicity.

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Norbert Straumann lower fractal dimension than the tensional. (d) It is also found that the tectonic topography, which is related to neotectonic and earthquake activity, also has fractal structures, such as the channels, ridges, and so on. (e) Fractal research into earthquakes has led to the development of a new dis

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