2 resultados para simulacrum of spontaneity
em University of Queensland eSpace - Australia
Resumo:
Starting from a comparison between the process of writing by hand and writing to screen, this paper contends that there is a continuity between the former, apparently archaic form of writing, and the latter, supposedly more modern form of writing. It will be suggested that, rather than being truly archaic, writing by hand perhaps constitutes a nostalgic act which attempts to bypass the perceived virtuality of the postmodern condition. As such, it will be claimed, via Baudrillard, that nostalgia of this kind is a type of hyper-simulacrum that relies on a misinterpretation of the noise created by the very act of expression. It will be claimed, however, that if interpreted without the sort of wilful misinterpretation to which noise often falls prey, many kinds of noise grafted onto contemporary cultural objects bear testimony to a certain continuity across historical eras as well as to the fact that we are ultimately incapable of recognising many cultural products' noise (and thus the products themselves in their entirety) in their own era. This paper therefore calls for a noisy theory which, analysing the world from an immanent position, would acknowledge the impossibility of full knowledge of the sign
Resumo:
Based on the three-dimensional elastic inclusion model proposed by Dobrovolskii, we developed a rheological inclusion model to study earthquake preparation processes. By using the Corresponding Principle in the theory of rheologic mechanics, we derived the analytic expressions of viscoelastic displacement U(r, t) , V(r, t) and W(r, t), normal strains epsilon(xx) (r, t), epsilon(yy) (r, t) and epsilon(zz) (r, t) and the bulk strain theta (r, t) at an arbitrary point (x, y, z) in three directions of X axis, Y axis and Z axis produced by a three-dimensional inclusion in the semi-infinite rheologic medium defined by the standard linear rheologic model. Subsequent to the spatial-temporal variation of bulk strain being computed on the ground produced by such a spherical rheologic inclusion, interesting results are obtained, suggesting that the bulk strain produced by a hard inclusion change with time according to three stages (alpha, beta, gamma) with different characteristics, similar to that of geodetic deformation observations, but different with the results of a soft inclusion. These theoretical results can be used to explain the characteristics of spatial-temporal evolution, patterns, quadrant-distribution of earthquake precursors, the changeability, spontaneity and complexity of short-term and imminent-term precursors. It offers a theoretical base to build physical models for earthquake precursors and to predict the earthquakes.