کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
9528373 | 1636671 | 2018 | 34 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Holocene paleoseismology of the Norcia fault system (Central Italy)
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
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چکیده انگلیسی
We investigated the Late Quaternary activity of the Norcia fault system, one of the most hazardous seismogenic structures of Italy, responsible over the centuries for nucleating several Mw 6 earthquakes, possibly up to Mw 6.9 as on 14th January 1703. This fault is located only 10â¯km away from the Mount Vettore fault system, which was responsible for the deadly Mw 6.6 central Italy earthquake in 2016. Using evidence gathered from ten paleoseismological trenches, we reconstructed the history of the strongest earthquakes sourced by the Norcia faults during the past 4â¯ky, and in previous time-windows back to 20â¯ka. In particular, we found indications of the historical 1703 and 99â¯BCE events, as well as a previously unknown one in the Bronze Age. We also obtained a robust estimate of the slip-rate for the post Last Glacial Maximum period (1â¯Â±â¯0.2â¯mm/yr), and a rough 1.8â¯ky recurrence time for ~Mw 6.9 events during the late Holocene.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 745, 16 October 2018, Pages 154-169
Journal: Tectonophysics - Volume 745, 16 October 2018, Pages 154-169
نویسندگان
P. Galli, A. Galderisi, I. Ilardo, S. Piscitelli, V. Scionti, J. Bellanova, F. Calzoni,