The preparation of earthquake catalogues for seismic hazard analysis requires the use of uniform parameters, in particular for magnitudes, although the original data include a variety of formats, such as macroseismic intensities and various instrumental mag- nitude scales. In regions of low seismicity, such as South Africa, data are generally sparse and not always suffi- cient to develop locally calibrated conversion relations. They can nevertheless be used to test the applicability of imported conversion relations, as well as their consis- tency. The Koffiefontein region of South Africa pro- vides a good test case in view of its somewhat higher level of seismicity, and central geographic location with- in the country. This paper reviews de...
Macroseismic data in the form of felt reports of earthquake shaking is vital to seismic hazard asses...
A uniform earthquake catalogue is an essential tool in any seismic hazard analysis. In this study a ...
This article evaluates the occurrence of 0 ≤ M ≤ 8 earthquake data sets for the period of 50 years (...
The preparation of earthquake catalogues for seismic hazard analysis requires the use of uniform par...
A database of intensity observations from instrumentally-recorded earthquakes in South Africa has be...
A database of intensity observations from instrumentally-recorded earthquakes in South Africa has be...
The seismicity of Grahamstown, in the Eastern Cape Province of South Africa, for the years between 1...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Study of Seismicity pattern in the Southern Africa from 1986 to 2009 was undertaken natural earthqua...
The seismicity of Grahamstown, in the Eastern Cape Province of South Africa, for the years between 1...
Parameters of seismic hazard are estimated by the application of the maximum likelihood method. The ...
Parameters of seismic hazard are estimated by the application of the maximum likelihood method. The ...
Macroseismic data in the form of felt reports of earthquake shaking is vital to seismic hazard asses...
A uniform earthquake catalogue is an essential tool in any seismic hazard analysis. In this study a ...
This article evaluates the occurrence of 0 ≤ M ≤ 8 earthquake data sets for the period of 50 years (...
The preparation of earthquake catalogues for seismic hazard analysis requires the use of uniform par...
A database of intensity observations from instrumentally-recorded earthquakes in South Africa has be...
A database of intensity observations from instrumentally-recorded earthquakes in South Africa has be...
The seismicity of Grahamstown, in the Eastern Cape Province of South Africa, for the years between 1...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Seismic hazard assessment for the Eastern and Southern Africa region was done using the probabilisti...
Study of Seismicity pattern in the Southern Africa from 1986 to 2009 was undertaken natural earthqua...
The seismicity of Grahamstown, in the Eastern Cape Province of South Africa, for the years between 1...
Parameters of seismic hazard are estimated by the application of the maximum likelihood method. The ...
Parameters of seismic hazard are estimated by the application of the maximum likelihood method. The ...
Macroseismic data in the form of felt reports of earthquake shaking is vital to seismic hazard asses...
A uniform earthquake catalogue is an essential tool in any seismic hazard analysis. In this study a ...
This article evaluates the occurrence of 0 ≤ M ≤ 8 earthquake data sets for the period of 50 years (...