Field- to nano-scale evidence for weakening mechanisms along the fault of the 2016 Amatrice and Norcia earthquakes, Italy

Tectonophysics

Volumn 712-713, Issue , 2017, Pages 156-169

  Luca, Smeraglia ^a   Billi, Andrea ^b   Carminati, Eugenio ^a,b   Cavallo, Andrea ^c   Doglioni, Carlo ^a,d  

^a SAPIENZA UNIVERSITY OF ROME   (Italy)

^b IGAG ^*  (Italy)

^c Multidisciplinary technology laboratory   (Italy)

^d ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

Author keywords

Amatrice Norcia earthquakes; Clay bearing fault; Fault zone structure; Fluidized cataclasite; Seismic slip propagation; Weakening mechanisms

Indexed keywords

EARTHQUAKES; FAULTING; FLUIDIZATION; GEOPHYSICS; NANOTECHNOLOGY; SEISMOLOGY; SHEAR FLOW; SILICATES; YARN;

BEARING FAULT; CATACLASITE; CRYSTALLOGRAPHIC TEXTURES; FAULT ZONE STRUCTURES; HYDROTHERMAL TEMPERATURE; SEISMIC SLIPS; SEISMIC VELOCITIES; SEISMOGENIC FAULTS;

FAULT SLIPS;

CATACLASITE; COSEISMIC PROCESS; EARTHQUAKE MAGNITUDE; EARTHQUAKE MECHANISM; FAULT SLIP; FAULT ZONE; NORMAL FAULT; SEISMICITY; SLIP RATE; STRUCTURAL GEOLOGY; TECTONIC SETTING;

ITALY;

EID: 85019678509     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2017.05.014     Document Type: Article

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