4.2 Article

Surface ruptures following the 30 October 2016 M-w 6.5 Norcia earthquake, central Italy

期刊

JOURNAL OF MAPS
卷 14, 期 2, 页码 151-160

出版社

TAYLOR & FRANCIS LTD
DOI: 10.1080/17445647.2018.1441756

关键词

Surface faulting; coseismic ruptures; normal faulting; geological prompt surveys; 2016-2017 seismic sequence; central Italy

资金

  1. Italian Civil Protection Department
  2. NERC Studentship [NE/L501700/1]
  3. NERC [NE/P018858/1, NE/P01660X/1, NE/I02318X/1]
  4. NERC [NE/J016497/1, NE/I026715/1, NE/I024127/1, NE/H003266/1] Funding Source: UKRI
  5. Natural Environment Research Council [1758141, 1779208, NE/P018858/1, NE/I02318X/1, NE/P01660X/1, NE/I026715/1, NE/H003266/1] Funding Source: researchfish

向作者/读者索取更多资源

We present a 1:25,000 scale map of the coseismic surface ruptures following the 30 October 2016 M-w 6.5 Norcia normal-faulting earthquake, central Italy. Detailed rupture mapping is based on almost 11,000 oblique photographs taken from helicopter flights, that has been verified and integrated with field data (>7000 measurements). Thanks to the common efforts of the Open EMERGEO Working Group (130 people, 25 research institutions and universities from Europe), we were able to document a complex surface faulting pattern with a dominant strike of N135 degrees-160 degrees (SW-dipping) and a subordinate strike of N320 degrees-345 degrees (NE-dipping) along about 28km of the active Mt. Vettore-Mt. Bove fault system. Geometric and kinematic characteristics of the rupture were observed and recorded along closely spaced, parallel or subparallel, overlapping or step-like synthetic and antithetic fault splays of the activated fault systems, comprising a total surface rupture length of approximately 46km when all ruptures were considered.

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