Early in the history of seismology it was occasionally suggested that, in addition to earthquakes with foci comparatively near the surface of the earth, shocks might also originate at depths of the order of several hundred kilometers. However, down to a comparatively recent date, all such conclusions were either purely speculative or were based on inadequate or misinterpreted data
This paper is based on detailed catalogues giving epicenters, origin times, and hypocentral depth fo...
We describe a method for determining the depth of deep earthquakes utilizing the travel-time differe...
Analysing the areal distribution of earthquakes produced in the Carpathian Basin the conclusion can ...
Early in the history of seismology it was occasionally suggested that, in addition to earthquakes w...
Early in the history of seismology it was occasionally suggested that, in addition to earthquakes w...
This paper is a continuation of a previous publication (1938). The writers distinguish (1) shallow ...
This paper is a continuation of a previous publication (1938). The writers distinguish (1) shallow ...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
The great majority of earthquakes are caused by the movement of faults. Two terms are used to determ...
The great majority of earthquakes are caused by the movement of faults. Two terms are used to determ...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
This paper is based on detailed catalogues giving epicenters, origin times, and hypocentral depth fo...
We describe a method for determining the depth of deep earthquakes utilizing the travel-time differe...
Analysing the areal distribution of earthquakes produced in the Carpathian Basin the conclusion can ...
Early in the history of seismology it was occasionally suggested that, in addition to earthquakes w...
Early in the history of seismology it was occasionally suggested that, in addition to earthquakes w...
This paper is a continuation of a previous publication (1938). The writers distinguish (1) shallow ...
This paper is a continuation of a previous publication (1938). The writers distinguish (1) shallow ...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
The great majority of earthquakes are caused by the movement of faults. Two terms are used to determ...
The great majority of earthquakes are caused by the movement of faults. Two terms are used to determ...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
Previous results are revised and extended. Most of the former conclusions are notably strengthened. ...
This paper is based on detailed catalogues giving epicenters, origin times, and hypocentral depth fo...
We describe a method for determining the depth of deep earthquakes utilizing the travel-time differe...
Analysing the areal distribution of earthquakes produced in the Carpathian Basin the conclusion can ...