4.4 Article

European-Mediterranean regional centroid-moment tensors:: 1997-2000

Journal

PHYSICS OF THE EARTH AND PLANETARY INTERIORS
Volume 130, Issue 1-2, Pages 71-101

Publisher

ELSEVIER
DOI: 10.1016/S0031-9201(01)00312-0

Keywords

seismicity; moment tensors; Mediterranean region

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The Mediterranean region is seismically very active and undergoing rapid deformation. Earthquakes as strong as M greater than or equal to 6 are present, but relatively rare. On the other hand, moderate-magnitude seismicity (4.5 < M < 5.5) is widespread and, often, damaging. An improved knowedge of moderate-magnitude earthquakes can contribute significantly to a better understanding of active tectonics in the region. Harvard centroid-moment tensors (CMT) today represent the most widely used reference for reliable source mechanisms, but modelling seismic sources with the CMT technique for earthquakes with magnitude less than M approximate to 5-5.5 is quite difficult. Since 1997, we are using an extension of the standard CMT algorithm to compute regional centroid-moment tensors (RCMT) for moderate-magnitude earthquakes (M-W as low as 4.0), analyzing intermediate-period surface waves from regional and teleseismic seismograms. We routinely apply the algorithm to European-Mediterranean seismicity to produce a catalog of seismic moment tensors for events with magnitude between 4.5 and 5.5, which generally are not included in the Harvard CMT catalog. In this paper, we show the results for earthquakes that occurred between 1997 and 2000, consisting of 252 solutions, and we discuss the characteristics of the catalog and the areas where these new data are most relevant. (C) 2002 Elsevier Science B.V. All rights reserved.

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