Title: Observatoires sousmarins et rle pour la dtection des glissements sousmarins et des tsunamis
1Observatoires sous-marins et rôle pour la
détection des glissements sous-marins et des
tsunamis
- Pierre Henry, CEREGE - Collège de France
- Roland Person, IFREMER, Brest
- Anne Deschamps, Nicole Bethoux, Geosciences Azur,
Villefranche-sur-Mer et Sophia-Antipolis
2Tsunami Sources
- Earthquakes
- Tsunami source model
- Static (before/after) topography change
- A priori knowledge of fault geometry is required
- Volcanoes
- Multiple source types
- Caldeira collapse (Santorin, Krakatau)
- Landslides
- Explosions
- Slope instabilites
- Tsunami source model
- Dynamic effects must be included
- Detection
- Remote vs. in situ sensors
3New sounds from the shallow and deep ends of
subduction
Very-low frequency earthquakes
Obara and Ito (2005) Davis et al. (2006)
Tremors
Obara (2002)
4Very low frequency earthquakes -Obara and Ito
(2005)
Regular
VLF
5Related Questions - What is the difference
between an accretionary wedge and a landslide ?
- Detection
- What is the importance of slow slip (rupture
propagation velocity ltlt Rayleigh wave velocity)
in tsunami generation during an earthquake ? - How do silent slip events make noise ?
- Prevision
- Is the catastrophic evolution of landslides
controlled by the properties of the sliding
surface ? - What controls the seismic-aseismic transition in
subduction zones ? - Mechanics
- How does fluid pressure vary in a decollement and
how does it relate with deformation ?
6Sismomètres fond de mer large bandes
Crawford et al., BSSA, accepté
7LIMO
- Installatin of (Cabled) Borehole Observatories on
the Ligurian Margin - Pierre Henry, Roland Person, Charles K. Paull,
Nicole Béthoux, Anne Deschamps, Achim Kopf,
Sébastien Migeon, Barbara Romanowicz, Etienne
Ruellan, Françoise Sage, Bruno Savoye, Ralph
Stephen, Nabil Sultan.
8Observatory context
- ESONET Network of Excellence
- Optical cable link to ANTARES Neutrino telescope
- IODP needs test site for borehole instrumentation
- Ifremer center in Toulon can provide logistic
support (ROV servicing)
9LIMO - Science focus
- Approach gravity driven processes at different
scales - Alpine collapse, margin failure and subduction
initiation - Failure of sedimented slope
- Coupling between stress, pore-pressure and strain
- external forcing (sea level, fluid migration,
sedimentation and compaction, airports) vs.
internal processes (dilatancy, compaction) - Influence of coastal aquifers on offshore slope
stability
10Seismometer borehole(s)
- Cased (ROV accessible) hole
- Broadband
- Test short period strings (SEIS-Cork)
- Location
- Ideally above seismicity cluster N of Var canyon
- Alternate on Var Levee
11Hydrogeology boreholes
- Address permeability-scale dependency in clay
rich hemipelagite/turbidite series. - Develop alternatives to packers and CORKs.
CORK (cased hole) accessible inner casing partial
retrievability
Wireline instrument passive monitoring non
retrievable
12Submarine slope monitoring
- Strain and pore pressure
- Observatory components
- repeat AUV surveys -gt evolution of morphology (E.
Ruellan) - seafloor
- OBS tiltmeter (P. Charvis, Y. Guglielmi)
- Fiber optic distributes strain and temperature
sensor network - below seafloor
- pore pressure, temperature (N. Sultan, J.F.
Rollin) - electrical conductivity (coastal sites - P.
Pezard) - strain (tiltmeters ?)
- Implementation
- Need for a seafloor drill -gt alternate platform
- MeBo ? (Bremen University, A. Kopf)
- Telemetry
limo-3B
13What will be the main benefit for society ?
- Awareness
- Would Damocles feel better with a strain meter ?