کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4721050 1639360 2013 15 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Source parameters of small and moderate earthquakes in the area of the 2009 L’Aquila earthquake sequence (central Italy)
ترجمه فارسی عنوان
پارامترهای منبع زمین لرزه های کوچک و متوسط ​​در ناحیه لرزه اکتویل 2009 (مرکزی ایتالیا)
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات ژئوشیمی و پترولوژی
چکیده انگلیسی


• A database of 312 moment tensor solutions for the 2009 L’Aquila seismic sequence (central Italy) is presented.
• Stress tensors for the study region and selected sub-volumes are computed.
• A relation between Mw and Ml properly calibrated for the study area is furnished.

The main goal of this study is to provide moment tensor solutions for small and moderate earthquakes of the 2009 L’Aquila seismic sequence (central Italy). The analysis was performed by using data coming from the permanent Italian seismic network run by the Istituto Nazionale di Geofisica e Vulcanologia (INGV) and the “Cut And Paste” (CAP) method based on broadband waveform inversion. Focal mechanisms, source depths and moment magnitudes are determined through a grid search technique. By allowing time shifts between synthetics and observed data the CAP method reduces dependence of the solution on the assumed velocity model and on earthquake location. We computed seismic moment tensors for 312 earthquakes having local magnitude in the range between 2.7 and 5.9. The CAP method has made possible to considerably expand the database of focal mechanisms from waveform analysis in the lowest magnitude range (i.e. in the neighborhood of magnitude 3) without overlooking the reliability of results. The obtained focal mechanisms generally show NW–SE striking focal planes in agreement with mapped faults in the region. Comparisons with the already published solutions and with seismological and geological information available allowed us to proper interpret the moment tensor solutions in the frame of the seismic sequence evolution and also to furnish additional information about less energetic seismic phases. Focal data were inverted to obtain the seismogenic stress in the study area. Results are compatible with the major tectonic domain. We also obtained a relation between moment and local magnitude suitable for the area and for the available magnitude range.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Physics and Chemistry of the Earth, Parts A/B/C - Volume 63, 2013, Pages 77–91
نویسندگان
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