 |
| Titel |
Tectonic sources of caucasus strong earthquakes |
| VerfasserIn |
M. Kachakhidze, N. Kachakhidze, R. Kiladze, V. Kukhianidze, G. Ramishvili |
| Medientyp |
Artikel
|
| Sprache |
Englisch
|
| ISSN |
1561-8633
|
| Digitales Dokument |
URL |
| Erschienen |
In: Natural Hazards and Earth System Science ; 4, no. 1 ; Nr. 4, no. 1 (2004-03-01), S.53-58 |
| Datensatznummer |
250001465
|
| Publikation (Nr.) |
 copernicus.org/nhess-4-53-2004.pdf |
|
|
|
|
|
| Zusammenfassung |
| The method called "phase cone" is developed in order to define the
location, time of arising and velocity of the earthquakes initiating
the low-speed interference stress waves. From the data of the strong
earthquakes with M≥6.0 in Caucasus region during 1900-1992,
the immigrators or tectonic sources of low-speed waves were
revealed, interference nodes of which had initiated 19 earthquakes
out of total 33.
The time of arising of low-speed stress waves or periods of awaking
of tectonic sources is defined.
The velocities of constant initiative waves for all events were
calculated. Its average value is equal to 2.97km per year. |
| |
|
| Teil von |
|
|
|
|
|
|
|
|