FRACTAL TECHNIQUES AND THE SURFACE-ROUGHNESS OF TALUS SLOPES - REPLY

被引：2
|
作者：
ANDRLE, R
ABRAHAMS, AD
机构：
[1] Department of Geography, State University of New York at Buffalo, Buffalo, New York
来源：
EARTH SURFACE PROCESSES AND LANDFORMS | 1990年 / 15卷 / 03期
关键词：
Fractals; Talus slopes;
D O I：
10.1002/esp.3290150311
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
There is discussion of the role of the self similar fractal model (SSFM) as a dominant paradigm in geomorphology; and how it may be applied appropriately. There is also a difference in the interpretation of curvature in logarithmic plots of step length vs total number of steps. Thirdly there is disagreement about interpreting application of the model to the talus clast transects; and finally on the significance of the dimensions obtained (D < 1·27) along the transects. Copyright © 1990 John Wiley & Sons, Ltd
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页码：287 / 290
页数：4
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