The present paper is supplementary to a previous publication under the same title, for which a list of errata is here given. The first paper has been translated into French by Professor E. Rothé, and is to be published by the Bureau Central Séismologique International. (The French publication will contain a travel-time chart for focal depth 600 km. in place of that for 400 km. given in the English paper.) At the request of Professor Rothé a more detailed account of the calculation of certain travel times was drawn up, which he has also translated, and which will appear as an additional note in the French publication. This additional note is given in English in the present paper. To this are added a new table (table 1, pp. 161-165 b...
In this paper the Author suggests to regard the lowerlimit of the category of the so-called shallow ...
Wave velocities in the interior of the earth are usually calculated by means of the Wiechert-Herglot...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
Travel times of normal earthquakes are made the basis for calculated travel times for shocks at dept...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
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 ...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1972.Inc...
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...
This paper is based on detailed catalogues giving epicenters, origin times, and hypocentral depth fo...
Two methods for determining the time of origin, depth of focus, and the average velocities from the ...
Travel times of waves generated by an earthquake at a depth of 600 km and reflected from the inside ...
Travel times of waves generated by an earthquake at a depth of 600 km and reflected from the inside ...
In this paper the Author suggests to regard the lowerlimit of the category of the so-called shallow ...
Wave velocities in the interior of the earth are usually calculated by means of the Wiechert-Herglot...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...
Travel times of normal earthquakes are made the basis for calculated travel times for shocks at dept...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
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 ...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1972.Inc...
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...
This paper is based on detailed catalogues giving epicenters, origin times, and hypocentral depth fo...
Two methods for determining the time of origin, depth of focus, and the average velocities from the ...
Travel times of waves generated by an earthquake at a depth of 600 km and reflected from the inside ...
Travel times of waves generated by an earthquake at a depth of 600 km and reflected from the inside ...
In this paper the Author suggests to regard the lowerlimit of the category of the so-called shallow ...
Wave velocities in the interior of the earth are usually calculated by means of the Wiechert-Herglot...
The magnitude of deep-focus earthquakes is so defined as to make the energy released in two shocks o...