FRICTIONAL ATTENUATION - INHERENT AMPLITUDE DEPENDENCE

被引:93
作者
MAVKO, GM [1 ]
机构
[1] STANFORD UNIV, DEPT GEOPHYS, STANFORD, CA 94305 USA
来源
JOURNAL OF GEOPHYSICAL RESEARCH | 1979年 / 84卷 / NB9期
关键词
D O I
10.1029/JB084iB09p04769
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
Frictional sliding on crack surfaces and grain boundaries is examined as a mechanism of wave attenuation. In constrast to previous work based on idealized elloptic crack models a general description of internal surfaces is considered which allows for irregularities and partially closed cracks. This leads to Q- 1 that increases with strain amplitude. Such an amplitude dependence is often observed in large-strain laboratory measurements. This suggests that under in situ (small strain) conditions, frictional attenuation becomes secondary to linear loss mechanisms, either disappearing or becoming masked. -Author English
引用
收藏
页码:4769 / 4775
页数:7
相关论文
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