Add to ORKGThe present paper is based upon the author's recent investigation of "The Partition of Energy among Seismic Waves Reflected and Refracted at the Earth's Core.'' Its purpose is the expression of the amplitudes of certain waves reflected and refracted at the earth's core in terms of the horizontal and vertical components of the displacement which they produce at the surface of the earth
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The attenuation of seismic waves is one manifestation of the earth's anelasticity and is not unrelat...
The present paper is based upon the author's recent investigation of "The Partition of Energy among...
The reflection and refraction of seismic waves has been studied extensively in the past by various ...
The reflection and refraction of seismic waves has been studied extensively in the past by various ...
The investigation of amplitudes of elastic waves passing through layers of the earth, either in eart...
The Zoeppritz equations are used to determine the energy partition in seismic waves reflected and r...
The Zoeppritz equations are used to determine the energy partition in seismic waves reflected and r...
Waves reflected from the outer boundary of the core of the earth often record trace amplitudes that ...
A method of calculating the amplitudes of bodily waves in earthquakes is applied to a study of the a...
A method of calculating the amplitudes of bodily waves in earthquakes is applied to a study of the a...
The subject of energy ratios of seismic waves reflected and refracted at a discontinuity has been s...
The subject of energy ratios of seismic waves reflected and refracted at a discontinuity has been s...
The investigation of amplitudes of elastic waves passing through layers of the earth, either in eart...
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The attenuation of seismic waves is one manifestation of the earth's anelasticity and is not unrelat...
The present paper is based upon the author's recent investigation of "The Partition of Energy among...
The reflection and refraction of seismic waves has been studied extensively in the past by various ...
The reflection and refraction of seismic waves has been studied extensively in the past by various ...
The investigation of amplitudes of elastic waves passing through layers of the earth, either in eart...
The Zoeppritz equations are used to determine the energy partition in seismic waves reflected and r...
The Zoeppritz equations are used to determine the energy partition in seismic waves reflected and r...
Waves reflected from the outer boundary of the core of the earth often record trace amplitudes that ...
A method of calculating the amplitudes of bodily waves in earthquakes is applied to a study of the a...
A method of calculating the amplitudes of bodily waves in earthquakes is applied to a study of the a...
The subject of energy ratios of seismic waves reflected and refracted at a discontinuity has been s...
The subject of energy ratios of seismic waves reflected and refracted at a discontinuity has been s...
The investigation of amplitudes of elastic waves passing through layers of the earth, either in eart...
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The energy observed in the seismic waves P and pP in a large number of earthquakes is compared, by m...
The attenuation of seismic waves is one manifestation of the earth's anelasticity and is not unrelat...