منابع مشابه
Coulomb stress accumulation along the San Andreas Fault system
Stress accumulation rates along the primary segments of the San Andreas Fault system are computed using a three-dimensional (3-D) elastic half-space model with realistic fault geometry. The model is developed in the Fourier domain by solving for the response of an elastic halfspace due to a point vector body force and analytically integrating the force from a locking depth to infinite depth. Th...
متن کاملCrustal deformation along the Altyn Tagh fault system, western China, from GPS
Abstract. We collected GPS data from the southern Tarim basin, the Qaidam basin, and the western Kunlun Shan region between 1993 and 1998 to determine crustal deformation along the Altyn Tagh fault system at the northern margin of the Tibetan plateau. We conclude from these data that the Altyn Tagh is a left-lateral strike slip fault with a current slip rate of 9 mm/yr, in sharp contrast with g...
متن کاملLate Quaternary and present-day rates of slip along the Altyn Tagh Fault, northern margin of the Tibetan Plateau
[1] Both Global Positioning System (GPS) measurements and studies of Late Quaternary faulting are consistent with a slip rate of 10 mm/yr along the central segment of the Altyn Tagh Fault and a systematic decrease in that rate toward the eastern end of the fault. Dates of terraces above and below laterally offset terrace risers yield bounds on Quaternary slip rates that range from those that ag...
متن کاملSpatio-temporal evolution of aseismic slip along the Haiyuan fault, China: Implications for fault frictional properties
a Institut des Sciences de la Terre (ISTerre), Université Joseph Fourier – Grenoble 1, CNRS, UMR 5275, BP 53, 38041 Grenoble, France b Department of Earth and Space Science, University of California, Los Angeles, United States c Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, United States d Tectonic Observatory, California Institute of Technology, Pasadena, C...
متن کاملDetection of fault segments based on P–T dihedra analysis along the North Tabriz fault, NW Iran
Detection of fault segments is an essential step for tracking main transverse faults. General observations from field studies as well as attitude measurements can give an overall understanding of the lengths of the segments, but these are not always sufficient to accurately identify and characterize them. In this study, we analyze P–T dihedra variations based on their eigenvalues to detect faul...
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ژورنال
عنوان ژورنال: E3S Web of Conferences
سال: 2020
ISSN: 2267-1242
DOI: 10.1051/e3sconf/202016503013