کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6444312 | 1640372 | 2014 | 32 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
3D modeling of earthquake cycles of the Xianshuihe fault, southwestern China
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
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چکیده انگلیسی
We perform 3D modeling of earthquake generation of the Xianshuihe fault, southwestern China, which is a highly active strike-slip fault with a length of about 350Â km, in order to understand earthquake cycles and segmentations for a long-term forecasting and earthquake nucleation process for a short-term forecasting. Historical earthquake data over the last 300Â years indicates repeated periods of seismic activity, and migration of large earthquake along the fault during active seismic periods. To develop the 3D model of earthquake cycles along the Xianshuihe fault, we use a rate- and state-dependent friction law. After analyzing the result, we find that the earthquakes occur in the reoccurrence intervals of 400-500Â years. Simulation result of slip velocity distribution along the fault at the depth of 10Â km during 2694Â years along the Xianshuihe fault indicates that since the third earthquake cycle, the fault has been divided into 3 parts. Some earthquake ruptures terminate at the bending part of the fault line, which may means the shape of the fault line controls how earthquake ruptures. The change of slip velocity and displacement at 10Â km depth is more tremendous than the change of the shallow and deep part of the fault and the largest slip velocity occurs at the depth of 10Â km which is the exact depth of the seismic zone where fast rupture occurs.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Asian Earth Sciences - Volume 96, 15 December 2014, Pages 205-212
Journal: Journal of Asian Earth Sciences - Volume 96, 15 December 2014, Pages 205-212
نویسندگان
Xiao-Fan Li, Bunichiro Shibazaki,