Add to ORKGWhen an earthquake occurs, two different kinds of waves are generated: waves which travel through the interior of the earth (space waves), and waves whose energy is propagated chiefly along surfaces (surface waves). The records of both kinds of waves can be used to study certain physical properties of the several layers of the earth, especially of the earth's crust
Seismology can be defined as the mathematical and physical study of earthquakes. It is also the stu...
The results of studies concerning the characteristics of the surface waves of earthquakes, carried ...
There are indications of two low-velocity layers in the earth's crust and mantle, one, in the contin...
When an earthquake occurs, two different kinds of waves are generated: waves which travel through th...
It has been assumed heretofore that the relatively large phase called [P bar] in records of near-by ...
Rayleigh waves from the Solomon Islands earthquake of July 29, 1950, recorded at Honolulu, Berkeley...
It has been assumed heretofore that the relatively large phase called [P bar] in records of near-by ...
Rayleigh waves from the Solomon Islands earthquake of July 29, 1950, recorded at Honolulu, Berkeley...
It has come to be realized in the present century that the science of Seismology, in addition to pro...
It has come to be realized in the present century that the science of Seismology, in addition to pro...
Properties of the suboceanic crust are deduced from dispersion of earthquake surface waves. Love wav...
The observed dispersion of Rayleigh waves across the Atlantic and Pacific oceans can be accounted f...
The observed dispersion of Rayleigh waves across the Atlantic and Pacific oceans can be accounted f...
We may now complete this paper with a brief summary. 1. The viscosity of water gives no influence up...
In 1910 A. Mohorovičić published the first paper in which arrival times of elastic waves from a nea...
Seismology can be defined as the mathematical and physical study of earthquakes. It is also the stu...
The results of studies concerning the characteristics of the surface waves of earthquakes, carried ...
There are indications of two low-velocity layers in the earth's crust and mantle, one, in the contin...
When an earthquake occurs, two different kinds of waves are generated: waves which travel through th...
It has been assumed heretofore that the relatively large phase called [P bar] in records of near-by ...
Rayleigh waves from the Solomon Islands earthquake of July 29, 1950, recorded at Honolulu, Berkeley...
It has been assumed heretofore that the relatively large phase called [P bar] in records of near-by ...
Rayleigh waves from the Solomon Islands earthquake of July 29, 1950, recorded at Honolulu, Berkeley...
It has come to be realized in the present century that the science of Seismology, in addition to pro...
It has come to be realized in the present century that the science of Seismology, in addition to pro...
Properties of the suboceanic crust are deduced from dispersion of earthquake surface waves. Love wav...
The observed dispersion of Rayleigh waves across the Atlantic and Pacific oceans can be accounted f...
The observed dispersion of Rayleigh waves across the Atlantic and Pacific oceans can be accounted f...
We may now complete this paper with a brief summary. 1. The viscosity of water gives no influence up...
In 1910 A. Mohorovičić published the first paper in which arrival times of elastic waves from a nea...
Seismology can be defined as the mathematical and physical study of earthquakes. It is also the stu...
The results of studies concerning the characteristics of the surface waves of earthquakes, carried ...
There are indications of two low-velocity layers in the earth's crust and mantle, one, in the contin...