Practal dimension of the 2001 El Salvador Earthquake time series

被引：0

作者：

Nurujjaman, Md. ^{[1
]}

Narayanan, R. ^{[1
]}

Iyengar, A. N. S. ^{[1
]}

机构：

[1] Saha Inst Nucl Phys, 1-AF,Bidhannagar, Kolkata 700064, W Bengal, India

来源：

MODELLING CRITICAL AND CATASTROPHIC PHENOMENA IN GEOSCIENCE: A STATISTICAL PHYSICS APPROACH | 2006年 / 705卷

关键词：

D O I：

10.1007/3-540-35375-5_19

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Earthquakes occur on the earth's surface as a result of rearrangement of terrestrial cortex or higher part of the mantle. The energy released in this process propagates over long distances in the form of elastic seismic waves [1]. In order to predict earthquakes many models have been proposed [2, 3]. Dynamics of an earthquake is so complicated that it is quite difficult to predict using available models. Seismicity is a classic example of a complex phenomenon that can be quantified using fractal concepts [4]. © 2006 Springer.

引用

页码：499 / +

页数：3

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