Dissimilar temperature profiles beneath oceans and continents give rise to thermoelastic stresses at and adjacent to the oceanic-continental margin. Computations of the magnitude and orientation of the maximum shear stress field reveal a zone of shear dipping beneath the continent from the margin.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/33354/1/0000752.pd
The principal objective of this paper is to present a simple and self-consistent review of the basic...
Super-continental insulation refers to an increase in mantle temperature below a supercontinent due ...
Continental breakup along transform margins produces a sequence of (1) continent-continent, (2) cont...
Temperature, velocity, and viscosity profiles for coupled thermal and mechanical models of the upper...
Geotherm families in which surface heat flow is the principal independent variable have been constru...
The mechanism of extension in the continental crust is apparently much more complex than that acting...
International audienceA scaling law for the heat flux out of a convective fluid covered totally or p...
Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sci...
Models for the thermal and mechanical evolution of the oceanic lithosphere predict he progressive de...
[1] Previous mantle convection studies with continents have revealed a first‐order influence of cont...
Super-continental insulation refers to an increase in mantle temperature below a supercontinent due ...
A coupled thermal and mechanical solid state model of the oceanic lithosphere and asthenosphere is p...
A map of the heat flux out of the earth's mantle has been prepared by subtracting the heat flow aris...
International audienceThe long geological history of passive margin evolution is complex yet typifie...
To evaluate the effects of variations in the thermal state of the overriding plate on the slab dip i...
The principal objective of this paper is to present a simple and self-consistent review of the basic...
Super-continental insulation refers to an increase in mantle temperature below a supercontinent due ...
Continental breakup along transform margins produces a sequence of (1) continent-continent, (2) cont...
Temperature, velocity, and viscosity profiles for coupled thermal and mechanical models of the upper...
Geotherm families in which surface heat flow is the principal independent variable have been constru...
The mechanism of extension in the continental crust is apparently much more complex than that acting...
International audienceA scaling law for the heat flux out of a convective fluid covered totally or p...
Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sci...
Models for the thermal and mechanical evolution of the oceanic lithosphere predict he progressive de...
[1] Previous mantle convection studies with continents have revealed a first‐order influence of cont...
Super-continental insulation refers to an increase in mantle temperature below a supercontinent due ...
A coupled thermal and mechanical solid state model of the oceanic lithosphere and asthenosphere is p...
A map of the heat flux out of the earth's mantle has been prepared by subtracting the heat flow aris...
International audienceThe long geological history of passive margin evolution is complex yet typifie...
To evaluate the effects of variations in the thermal state of the overriding plate on the slab dip i...
The principal objective of this paper is to present a simple and self-consistent review of the basic...
Super-continental insulation refers to an increase in mantle temperature below a supercontinent due ...
Continental breakup along transform margins produces a sequence of (1) continent-continent, (2) cont...
DOI
Add to ORKG