کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
809067 1468696 2015 8 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Effect of slip-weakening distance on selected seismic source parameters of mining-induced fault-slip
ترجمه فارسی عنوان
اثر فاصله تضعیف لغزش در پارامترهای منبع لرزه ای انتخاب شده از لغزش گسل ناشی از معادن
کلمات کلیدی
گسل لغزش، قانون لغزش ضعیف قانون فاصله ضعیف لغزش مشخص، پارامترهای منبع لرزه ای، میزان لغزش
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات مهندسی ژئوتکنیک و زمین شناسی مهندسی
چکیده انگلیسی


• Slip-weakening distance, d0, exerts a large influence on slip rates.
• Likewise, seismically radiated energy is significantly affected by d0.
• Seismic moment, M0, is susceptible to d0 for fault-slip occurring across a fault.
• M0 is not severely affected by d0 for fault-slip occurring within limited areas.

Fault-slip caused by mining activities in underground mines could cause severe damage to nearby mine openings due to seismic waves arising from the fault-slip. A better understanding of seismic source parameters, such as seismically radiated energy and the maximum slip rate, is of pivotal importance in estimating the damage induced by the fault-slip. It is widely recognized that dynamic behaviour of fault-slip is largely affected by slip-weakening behaviour. In the present study, the effect of the slip-weakening behaviour on selected seismic source parameters of fault-slip is investigated using a mine-wide numerical model encompassing a fault running parallel to an orebody. A linear slip-weakening law is employed in a parametrical study with respect to characteristic slip-weakening distance, d0, assuming two types of fault-slip: (a) zonal fault-slip taking place across the fault; (b) local fault-slip taking place within limited areas of the fault, i.e., it is assumed that fault-slip is arrested by surrounding rockmasses. Results obtained from the dynamic analysis indicate that seismically radiated energy and slip rates are significantly affected by d0 for both types of fault-slip. On the other hand, the seismic moment is susceptible to d0 only for zonal fault-slip, given that d0 is smaller than the maximum shear displacement increment during the fault-slip. These results imply that considering slip-weakening distance is critical in estimating seismically radiated energy and slip rates, whereas slip-weakening behaviour might not have a large influence on seismic moment of local fault-slip.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: International Journal of Rock Mechanics and Mining Sciences - Volume 73, January 2015, Pages 115–122
نویسندگان
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