Dept. of Geosciences Colloquium: The November 11 2019 Le Teil, France M5 earthquake: a shallow triggered event in nuclear country and an opportunity for hypocentral drilling

Jean Paul Ampuero, IRD & UCA, Nice

23 November 2020, 11:00 
Zoom: https://us02web.zoom.us/j/84082397568 
Dept. of Geosciences Colloquium

Zoom: https://us02web.zoom.us/j/84082397568

 

Recording: https://us02web.zoom.us/rec/share/hvcSNkkjMw28Y5mpUyNCGiRiBbgXeLoBustkvbS1xaQfVDSZwDPGkBA0FT8kpAEK.TcQymqU-1K3MFc1O?startTime=1606121254000

 

Abstract:

An earthquake of local magnitude 5 (Mw 4.9) occurred near the town of Le Teil, France on November 11 2019, causing damage locally and concern due to its proximity to nuclear facilities. Despite its moderate magnitude, this earthquake offers unique opportunities to advance research on earthquakes in general. We will present an overview of the source characteristics of this event and, based on analysis of InSAR data, seismological observations and optical images, we discuss its potential relation to human activity. We also discuss the emerging unique research opportunities.

 

The Le Teil earthquake occurred in a low seismicity region, a moderate hazard zone that has nevertheless experienced damaging earthquakes in the past. Its hypocentral depth is particularly shallow, less than 1.5 km. Radar images delineate the surface rupture and constrain well the coseismic slip distribution. The surface rupture corresponds to the previously mapped La Rouvière fault, an ancient normal fault reactivated as reverse-faulting by the Le Teil earthquake. Slip is predominantly confined to the top 1 km and extends along ~4.5 km along-strike with two main slip asperities and stress drop of a few MPa. 

 

A large cement quarry sits on top of the deep edge of the rupture area, ~1 km above the fault. Based on optical images we estimate the distribution of mass extracted from the nearby quarry since 1947. We then compute the induced Coulomb stresses on the fault: they are favorable for reverse faulting and reach about 150 kPa, within the range of stresses that have been previously reported to trigger earthquakes, but substantially smaller than the coseismic stress drop. Analysis of the mainshock and quarry blast signals on the nearest stations places the mainshock epicenter within the area of influence of the quarry-induced stresses. These analyses indicate that the Le Teil event is likely a triggered earthquake: its initiation was favored by the quarry-induced stresses, but the bulk of its rupture propagation was enabled by naturally pre-existing stresses.

 

The characteristics of the Le Teil earthquake bear on important questions: how can earthquakes nucleate at such shallow depth? what confines slip at such shallow depth? do structural features control the patchy distribution of slip? how do elongated ruptures stop? Owing to its very shallow rupture depth, it also offers a unique opportunity to study directly, by drilling at seismogenic depth, the three key spots of an earthquake: its hypocenter, its large slip area and its arrest area. Moreover, the high aspect ratio of the rupture, comparable to that of the largest earthquakes, opens a window into the physics of very large earthquakes. Continued research and observation structured around a drilling project at seismogenic depth would also address implications for seismic hazard in low seismicity areas, including the safety of nearby nuclear power plants, especially by evaluating and monitoring hazards on the unbroken sections of the fault system.

 

 

Event Organizers: Dr. Roy Barkan and Dr. Asaf Inbal

 

 

Tel Aviv University makes every effort to respect copyright. If you own copyright to the content contained here and / or the use of such content is in your opinion infringing, Contact us as soon as possible >>
Tel Aviv University, P.O. Box 39040, Tel Aviv 6997801, Israel
UI/UX Basch_Interactive