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DOI10.1126/science.1061361
Mantle flow beneath a continental strike-slip fault: Postseismic deformation after the 1999 Hector Mine earthquake
Pollitz F.F.; Wicks C.; Thatcher W.
发表日期2001
ISSN0036-8075
起始页码1814
结束页码1818
卷号293期号:5536
英文摘要Two recent large earthquakes in the Mojave Desert, California - the magnitude 7.3 1992 Landers and magnitude 7.1 1999 Hector Mine earthquakes - have each been fog[owed by elevated crustal strain rates over periods of months and years. Geodetic data collected after the Hector Mine earthquake exhibit a temporaLLy decaying horizOntaL velocity field and a quadrant uplift pattern opposite to that expected for LocaLized shear beneath the earthquake rupture. We interpret the origin of this accelerated crustal deformation to be vigorous flow in the upper mantle in response to the stress changes generated by the earthquake. Our results suggest that transient flow in the upper mantle is a fundamental component of the earthquake cycle and that the Lower crust is a coherent stress guide coupling the upper crust with the upper mantle.
英文关键词Deformation; Earthquakes; Mines; Strain; Velocity; Mantle flow; Seismology; crustal deformation; earthquake; postseismic process; strike-slip fault; upper mantle; article; earthquake; geography; geology; priority journal; United States; velocity; United States
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/245106
作者单位U.S. Geological Survey, MS 977, 345 Middlefield Road, Menlo Park, CA 94025, United States
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Pollitz F.F.,Wicks C.,Thatcher W.. Mantle flow beneath a continental strike-slip fault: Postseismic deformation after the 1999 Hector Mine earthquake[J],2001,293(5536).
APA Pollitz F.F.,Wicks C.,&Thatcher W..(2001).Mantle flow beneath a continental strike-slip fault: Postseismic deformation after the 1999 Hector Mine earthquake.Science,293(5536).
MLA Pollitz F.F.,et al."Mantle flow beneath a continental strike-slip fault: Postseismic deformation after the 1999 Hector Mine earthquake".Science 293.5536(2001).
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