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Eos, Transactions American Geophysical Union, 1921
I assume that I am expected to bring forward whatever ideas will, in my opinion, help most at the present time in the development of a study of isostasy by stimulating further thinking along that line. From among the many topics which might be treated, I am selecting three:(1) I shall make some remarks on the recent paper entitled “The Chemistry of the
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I assume that I am expected to bring forward whatever ideas will, in my opinion, help most at the present time in the development of a study of isostasy by stimulating further thinking along that line. From among the many topics which might be treated, I am selecting three:(1) I shall make some remarks on the recent paper entitled “The Chemistry of the
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2011
Thermal isostasy, that part of isostasy traceable to density differences being caused by temperature differences and thermal expansion of rock, is an important but underap-preciated condition in crustal geophysics. The condition/ process of thermal isostasy received much attention in oceanic regions with the discovery of plate tectonics and seafloor ...
Hasterok, D., Chapman, D.S.
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Thermal isostasy, that part of isostasy traceable to density differences being caused by temperature differences and thermal expansion of rock, is an important but underap-preciated condition in crustal geophysics. The condition/ process of thermal isostasy received much attention in oceanic regions with the discovery of plate tectonics and seafloor ...
Hasterok, D., Chapman, D.S.
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Physics of the Earth and Planetary Interiors, 1972
Abstract Both a theoretical treatment and observed data show that the isostatic gravity field and the seismicity are closely related. The equation for harmonic loading shows that large deviations from isostatic equilibrium lead to large shear stresses in the crust.
M.E. Artemjev +3 more
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Abstract Both a theoretical treatment and observed data show that the isostatic gravity field and the seismicity are closely related. The equation for harmonic loading shows that large deviations from isostatic equilibrium lead to large shear stresses in the crust.
M.E. Artemjev +3 more
openaire +1 more source