Global seismicity characteristics of subduction-to-strike-slip transitions
نویسندگان
چکیده
منابع مشابه
Application of real-time GPS to earthquake early warning in subduction and strike-slip environments
[1] We explore the application of GPS data to earthquake early warning and investigate whether the coseismic ground deformation can be used to provide fast and reliable magnitude estimations and ground shaking predictions. We use an algorithm to extract the permanent static offset fromGPS displacement time series and invert for the slip distribution on the fault plane, which is discretized into...
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fert, M.E. Cameron, B. R. Smith-Konter, R.T. Pappalardo, and G. C. Collins, University of Michigan, Atmospheric Oceanic and Space Sciences Department, [email protected], Jet Propulsion Laboratory California Institute of Technology, [email protected], University of Hawaii at Manoa, Department of Geology and Geophysics, [email protected], [email protected], 4 Wheaton College, Ph...
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Fault zones and fault-related fracture systems control the mechanical behaviors and fluid-flow properties of the Earth’s crust. Furthermore, nowadays, modeling is being increasingly used in order to understand the behavior of rock masses, and to determine their characteristics. In this work, fault zones and fracture patterns are reviewed, and also comprehensive studies are carried out on the fr...
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We evaluated the influence of the trench-parallel component of plate motion on the active fault system within the Nankai accretionary wedge from reflection seismic profiles, high-resolution seafloor bathymetry, and deep-towed sub-bottom profiles. Our study demonstrated that a large portion of the trench-parallel component of oblique plate subduction is released by strike-slip motion along a fau...
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Analytical methods presented to analyze the buried steel pipelines at strike-slip fault crossing use the Euler-Bernoulli beam theory. The cross-section of a buried pipe that is completely surrounded by soil cannot rotate freely and would not be remained perpendicular to the bending line after deformation. So it would be better to take into consideration a rotation between the cross-section and ...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research: Solid Earth
سال: 2001
ISSN: 0148-0227
DOI: 10.1029/2000jb900309