Browsing by Author "Jordan T.H."
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Browsing by Author "Jordan T.H."
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Boettcher M.S.; Jordan T.H. (2004)A mid-ocean ridge transform fault (RTF) of length L, slip rate V, and moment release rate M can be characterized by a seismic coupling coefficient χ = AE/AT, where AE ∼ M/V is an effective seismic area and AT ∝ L3/2V-1/2 ...
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Korenaga Ju.; Jordan T.H. (2001)The physics of thermomechanical coupling of the continental lithosphere and its surrounding mantle is studied using a simple hydrodynamic model in which a fluid is heated from below and is bounded by rigid side walls. ...
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Korenaga Ju.; Jordan T.H. (2002)An assumption of isothermal and static asthenosphere as the normal state of sublithospheric mantle, as commonly employed in studies of terrestrial magmatism, may be physically implausible for a system cooled from above. ...
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McGuire J.L.; Zhao L.; Jordan T.H. (2002)The manner in which an earthquake rupture propagates across a fault reflects both the initial properties of the fault and the dynamical stresses produced by the rupture. We quantify the propagation of an earthquake rupture ...
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Shapiro S.S.; Hager B.H.; Jordan T.H. (1999)Continental cratons overlie thick, high-viscosity, thermal and chemical boundary layers, where the chemical boundary layers are less dense than they would be due to thermal effects alone, perhaps because they are depleted ...
Now showing items 1-5 of 5