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Lithospheric flexure at the Hawaiian Islands and its implications for mantle rheology
Perspective view (to the NW) of the satellite-derived free-air gravity anomaly field along the Hawaiian Islands
S. J. Zhong (University of Colorado, Boulder, USA)A. B. Watts (University of Oxford, UK)
Kauai
Hawaii
MolokaiOahu
Depth converted seismic reflection profile data and flexure along the Kauai/Molokai transects
Watts & ten Brink (1989)
The elastic plate (flexure) model
Te = 28 km
Corrections applied to reflectors:
•Seafloor age•Swell height
•FZ crustal structure
Linear elasticityInviscid substrate
ρload = 2800 kg m-3
ρinfill = 2600 kg m-3 ρmantle = 3330 kg m-3
E = 1012 Paν = 0 .25
Hunter et al. (2014)
The behavior of oceanic lithosphere on seismic to geologic time-scales
There is a competition between thermal cooling which strengthens the lithosphere and a stress-induced relaxation which weakens the lithosphere
Te ~1/3 Tse
OahuLoad age = 3-4 Ma
Seafloor age = 80 Ma
Deep-sea trench – Outer Rise (Corrected for yielding)
Seamounts and OceanicIslands
Viscoelastic plate models and the time scales of isostatic adjustment
n = 1 (i.e. diffusion creep)
ε.
=τ s
μ
⎛⎝⎜
⎞⎠⎟
n
Aexp −Qp / RT( )
Karato & Wu (2003)
Fast isostasy
Slow isostasy
Watts & Zhong (2001)
Rheology of oceanic lithosphere: A laboratory perspective
•Frictional sliding (shallow depths) or Byerlee’s law:
•Semi-brittle (transitional regime, poorly understood)
•Plastic flow: a) Low-temperature plasticity (<~800 oC):
b) High-temperature creep (>~800 oC):
τ yield = c0 + μρgh
ε.
= Aσ n exp −Ep
RT1−
σ
σ p
⎛
⎝⎜
⎞
⎠⎟
p⎛
⎝⎜⎜
⎞
⎠⎟⎟
q⎧
⎨⎪
⎩⎪
⎫
⎬⎪
⎭⎪
ε.
= Aσ n exp −Ec
RT⎧⎨⎩
⎫⎬⎭
Zhong & Watts (2013)
Viscoelastic plate flexure and laboratory-based mantle rheology
Case R1Seafloor age = 80 MaMultilayered viscosity
Loading history
Byerlee friction lawμ = 0.7
Low temperature (<800 oC)plasticity (Mei et al 2010)
n=3.5, Ep=320 KJ/mol
High temperature (>800 oC)creep (Hirth & Kohlstedt
1996). Ec=360 KJ/mol
Case R14Seafloor age = 80 MaMultilayered viscosity
Loading history
Byerlee friction lawμ = 0.7
Low temperature (<800 oC)plasticity (Mei et al 2010)
n=3.5, Ep=320 KJ/mol
High temperature (>800 oC)creep (Hirth & Kohlstedt
1996). Ec=360 KJ/mol
+108 weakening
Conclusions
• Seismic and earthquake data at the Hawaiian Islands have been used, together with viscoelastic plate modelling, to constrain laboratory-based rheological laws.
• Flow laws such as Mei et al. that combine low and high temperature creep, fit the seismic data, but require significant weakening.
• A weakened Mei et al. predicts a ~30 km thick double seismic zone and a maximum bending stress of ~100-200 MPa.
• Earthquake data are most sensitive to frictional laws (e.g. Byerlee) and suggest coefficients in the range of 0.25-0.70.
• Models that incorporate the best fit rheological laws suggest the subsidence induced by volcano loads is more than ~30% achieved ~350 ka after loading and is essentially complete by ~750 ka.