Summary of key
observational / experimental constraints on models of subduction zones
Result of breakout
discussion group moderated by Tim Grove
Key observations to Match
- Heat
flow
- Gravity
and Geoid
- Topography
- Slab
dip (geometry)
Key observations to match/assess
- Distribution
of volcanoes above slab in 2D and along-strike in 3D
- Pressure
and temperature conditions at the top of the mantle wedge
- Low
seismic velocities at the top of the slab
- Thickness
variations observed in the upper plate
- General
seismic attenuation and velocity structure of the wedge
- Presence/absence
& time duration of back arc basins + Asymmetry of Pacific subduction
zones
- Limits
of shallow seismogenic zone
- Seismic
anisotropy of the wedge
- Major
element compositions of primitive lavas
Observations not to be used as constraints
- Temperature
at the slab/wedge interface. What is the conceivable range?
- Time
scale inferred for melt transport.
Issues to explore
- Influence
of 2 phase flow
- Does
the incorporation of water in the slab have important consequences?