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DOI10.1126/science.286.5438.272
Evidence of nonlinear elasticity of the crust from the Mw7.6 Manyi (Tibet) earthquake
Peltzer G.; Crampé F.; King G.
发表日期1999
ISSN0036-8075
起始页码272
结束页码276
卷号286期号:5438
英文摘要Satellite synthetic aperture radar (SAR) interferometry shows that the magnitude 7.6 Manyi earthquake of 8 November 1997 produced a 170-kilometer- long surface break with up to 7 meters of left-lateral slip, reactivating a N76 °E quaternary fault in western Tibet. The radar interferometric map reveals asymmetric, along-strike displacement profiles between the two sides of the surface rupture, a pattern that cannot be explained with linear elastic theory. This observation suggests that the elastic moduli of the crust in tension and in compression are different because of the presence of cracks in the crust at shallow depth. A model indicates that a ratio of 2 between compressive and tensile elastic moduli can account for the observed asymmetry, a ratio that is consistent with laboratory and borehole measurements.
英文关键词crustal structure; earthquake; elasticity; fault; rupture; synthetic aperture radar; article; earthquake; elasticity; geology; interferometer; Nepal; priority journal; rock; telecommunication; young modulus; China
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245031
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Peltzer G.,Crampé F.,King G.. Evidence of nonlinear elasticity of the crust from the Mw7.6 Manyi (Tibet) earthquake[J],1999,286(5438).
APA Peltzer G.,Crampé F.,&King G..(1999).Evidence of nonlinear elasticity of the crust from the Mw7.6 Manyi (Tibet) earthquake.Science,286(5438).
MLA Peltzer G.,et al."Evidence of nonlinear elasticity of the crust from the Mw7.6 Manyi (Tibet) earthquake".Science 286.5438(1999).
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