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Rock Anisotropy and the Theory of Stress Measurements
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Rock Anisotropy and the Theory of Stress Measurements

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Any undisturbed rock mass is subject to natural stresses inclu­ ding gravitational stresses due to the mass of the overburden and possibly tectonic stresses due to the straining of the earth's crust and remanent stresses due to past tectonism.
Författare
Bernard Amadei
Upplaga
Softcover reprint of the original 1st ed. 1983
ISBN
9783540123880
Språk
Engelska
Vikt
310 gram
Utgivningsdatum
1983-05-01
Sidor
482