Direction of Faulting in the Deep-Focus Spanish Earthquake of March 29, 1954
Open Access
- 1 January 1956
- journal article
- Published by Stockholm University Press in Tellus A: Dynamic Meteorology and Oceanography
- Vol. 8 (3) , 321-328
- https://doi.org/10.3402/tellusa.v8i3.9020
Abstract
An earthquake of magnitude 7.1 occurred off the south coast of Spain on March 29, 1954. The earthquake was remarkable in that it had a focal depth of about 650 km; no earthquake with focal depth greater than normal is known to have occurred in this area previously. Using methods already established but here reviewed, the mechanism at the focus is investigated. The method defines two planes, without determining which is the fault. There are thus two possibilities. Under the first possibility the fault is approximately vertical and strikes north-south. The movement is vertical, such that the eastern side of the fault rises with respect to the western side. Under the second possibility the fault is approximately horizontal, and the movement is also horizontal, the material above the focus moving due east (that is, in the sense of the earth's rotation) with respect to the material below the focus.Keywords
This publication has 3 references indexed in Scilit:
- Phase change of PP and pP on reflection at a free surface*Bulletin of the Seismological Society of America, 1956
- Direction of faulting in some of the larger earthquakes of 1949*Bulletin of the Seismological Society of America, 1954
- Tables extending byerly's fault-plane techniques to earthquakes of any focal depth*Bulletin of the Seismological Society of America, 1953