Activity of UR in phase Sample Clauses

Activity of UR in phase. 1 The research activity of the Perugia UR is subdivided into two main sub-projects, which were dedicated to: i) the subsurface geology (wp 1.4 resp. X. Xxxxxxxxx) and to the surface geology and geomorphology (wp 1.5 resp. X. Xxxxxx). The Perugia UR also contributes to other investigations such as the geodetic ones and those on the active state of deformation, which are addressed by the INGV UR (wp 1.3, resp. X. X'Xxxxxxxx) through a subcontract with the Civil and Environmental Engineering Department of the University of Perugia (resp. X. Xxxxxxxxx) for the maintenance of the permanent GNSS/GPS stations of the GPSUMBRIA and LABTOPO networks. WP 1.4, Upper crustal structure and tectonic evolution of ATF (Xxxxxxxxx Xxxxxxxxx) The activity of the wp 1.4 was focused on the geological reconstruction of the subsurface of the Altotiberina normal fault (ATF) and on the sequential balancing of geological sections across the ATF. The UniPg people involved in this part are X. Xxxxxxxxx, X. Xxxxxx and X. Xxxxxxxxxx who is working on his PhD within this project. We started collecting the available data, both surface geological data (maps 1:10.000, 1:25.000, 1:100.000), and subsurface data (boreholes and commercial seismic data). The main topics addressed by this wp concern the coherent re-interpretation of the seismic data, calibration with boreholes and surface geology, estimation of the velocity field through the xxxxx sonic logs for the depth conversion of the reflectors and the sequential restoration of the extensional structures. The data, after being gathered and projected/reprojected into the same geographical reference system with GIS tools, were loaded into the MoveTM package which allows the depth conversion and sequential balancing of the geological sections to be made. The sequential restoration and balancing was addressed along two sections (L1 and L2 in figure and in D6 deliverable) which cross the region between the Tiber Valley and the Gubbio anticline. The interpretation of these two sections is tied to the stratigraphy of three boreholes, X.Xxxxxx0, X.Xxxxxxxxx0 and Perugia2.
Sample 1
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Activity of UR in phase. 1 The first year activity of the UR-Xxxxxxx primarily consisted (a) in the preparation of the earthquake dataset relative to seismicity occurring during 1988-2007 in the Xxxxxxx Straits area and (b) the focal mechanism computations by application of different techniques. Up to date, the analyses have been performed using the information collected during the last twenty years by the local and national permanent seismic networks. In the third semester, we are going to use also the data coming from the current INGV experiment in the study area (Xxxxxxx 1908-2008). We extracted from the INGV seismic catalogue all the earthquakes occurring in the study area until October 2008 characterised by focal depth less than 25 km and magnitude Ml ranging between 3 and 4.1. The dataset was restricted to the earthquakes recorded at a minimum of 4 three-component seismic stations equipped with broad-band sensors such as Trillium 40s, STS-2-120s, and Xxxxxxxx-3D-20s, located within a radius of 300km from the epicenter. The final data set used in this study consisted of about 1000 waveforms from 23 earthquakes. We relocated these events using the BAYLOC non-linear probabilistic location method by Xxxxxx et al. (2004, 2008) and the 3-D seismic velocity model proposed for the study area by Xxxxxxx et al. (2004). The state of art of knowledge on the earthquake mechanisms is represented by few solutions from waveform inversion (CMT, RCMT, TDMT solutions relative to earthquakes of magnitude 4 and larger; Xxxxxxxxx et al. [2006], xxxx://xxxxxxxxxx.xx.xxxx.xx/tdmt.php), and by tens of solutions estimated with the traditional methods of P-onset polarity inversion (Xxxxxxx and Xxxxx, 2000; Xxxxxxxxx and Xxxxxxxx, 2004; Xxxx et al., 2004). Nearly all the fault plane solutions estimated by inversion of P-onset polarities are affected by uncertainties larger than 15-20° due to poor network geometry caused by offshore location of many events and the lack of OBSs in the study area. We computed the moment tensor solutions using the “cut and paste” method based on broadband waveform inversion (Xxx and Xxxxxxxxxx, 1996, and Xxx et al., 2006). These results bring new knowledge on the seismogenic mechanisms in the study area. The results are going to be interpreted also in cooperation with others UR of this Project. The obtained focal solutions have been integrated with the data available in the official databases and in the literature. The already existing information coming from application o...
Sample 1

Related to Activity of UR in phase

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