1936
DOI: 10.1073/pnas.22.8.482
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The Elastic Properties of Rocks: A Correlation of Theory and Experiment

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Cited by 58 publications
(2 citation statements)
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“…The values of primary and secondary wave velocity and the density of the specimen are used to calculate these mechanical rock parameters. It is important to note that the dynamic moduli of the rock are different from the static moduli due to some assumptions before any calculation, such as homogeneous, isotropic and perfect elastic of the rock being studied, which is not always true in most cases [13]. The dynamic moduli of fine-grained and igneous rocks, as well as sedimentary rocks are higher than static moduli, including Young's modulus, shear modulus, and Poisson's ratio [14].…”
Section: Methodsmentioning
confidence: 99%
“…The values of primary and secondary wave velocity and the density of the specimen are used to calculate these mechanical rock parameters. It is important to note that the dynamic moduli of the rock are different from the static moduli due to some assumptions before any calculation, such as homogeneous, isotropic and perfect elastic of the rock being studied, which is not always true in most cases [13]. The dynamic moduli of fine-grained and igneous rocks, as well as sedimentary rocks are higher than static moduli, including Young's modulus, shear modulus, and Poisson's ratio [14].…”
Section: Methodsmentioning
confidence: 99%
“…K=Bulk modulus=16.7xlO n dynes/cm 2 (Zisman, 1933). G=Rigidity modulus=8.38xlO n dynes/cm2 (Ide, 1936). K=thermal diffusivity=0.181 cmVsec (Ingersoll and others, 1948).…”
Section: Behavior Of a Model Meteorite Body In A Desert Region Distribution Of Temperature And Thermal Stressmentioning
confidence: 99%