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the elasticity formalism whirh cxtendR, (he vali(lit.y uf the Thomils-I<'eflili
Illodel to pressures of geoph:rsical illterest. The model is (')le('kcd with
sho('k Waves (lata, with the Bireh-~rurnaghan f'qllations und \\"ith the Earth's
('onl e(juation of sta(.e.
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