...Karl Koch; Klaus Stammler Up to now the detection and elimination of such timing errors was considered an unsolvable problem. This would certainly be true if the GERESS array were a single- (or three-) component station. However, an array provides the chance to use waveform correlation...

...V. Schlindwein; K. Koch Abstract Site effects were studied for the individual sites of the 25 elements of the German Experimental Seismic System (GERESS) array based on the traditional spectral ratio (TSR) technique and horizontal-to-vertical ratios (HVRs) for earthquakes and microtremors, commonly...

...M. L. Jost; J. Schweitzer; H.-P. Harjes Abstract Since the installation of the 25-element GERman Experimental Seismic System ( GERESS ) array in southeastern Germany in 1990, 36 presumed nuclear tests were recorded by this system: 16 from Nevada, 12 from the Tuamotu Archipelago, 7 from Lop Nor...

...Götz H. R. Bokelmann Abstract For high signal-to-noise ratio events, body-wave travel times at GERESS stations are well fit by a plane-wave model corresponding to travel time uncertainties of about 1/100 sec. Slownesses obtained in this study are accurate to about 0.5 sec/deg, while azimuth...

... it has been operated continuously to process the data from four high-frequency arrays (adding FINESA in Finland and GERESS in Germany). For some periods data from as many as seven 3-component stations in Eurasia have also been included in the processing. The most important new element is ESAL (Expert...

...Götz H. R. Bokelmann; Stefan Baisch Abstract We study the nature of extremely narrow-band signals that appear in typical long-time spectra of seismic recordings. At the German Experimental Seismic System ( GERESS ) array, we observe several of these time-continuous spectral lines. The most...

... explosions, mining blasts, and earthquakes, recorded by the ARCESS and GERESS arrays in Norway and Germany, respectively, station WMQ in China, and stations KNB and MNV in the western United States, are presented and compared. The outlier-test procedure is applied in each region, using Pn/Lg , Pn/Sn , and Pg...

...Jan Wüster Abstract Both natural and artificial seismicity is observed in the Vogtland area at near regional distance (180 km) from the GERESS array. This setting offers the opportunity to test various discrimination criteria using a uniform data set of 39 earthquakes and 22 chemical explosions...

... for analysis jointly with existing arrays. The first additional data to become available will be from the GERESS array, which will be established in the Federal Republic of Germany in 1990. Future perspectives also include the use of expert system technology in the data analysis, and the IMS system already...

.... There is no clear evidence for a negative noise correlation distance at these frequencies. Signal coherence in the same frequency bands proved to be excellent (>0.9) for all regional phases over the 3 km aperture of the test array. The final configuration of the new regional array in the BF area—named GERESS—has...

... and at test sites of Novaya Zemlya and eastern Kazakh. Also, recordings at the Graefenburg array, near the new GERESS regional array, of Novaya Zemlya events and an eastern European platform (White Sea) event have been compared with the Norwegian array recordings of the same events. The White Sea explosion...

... GERESS array (Bokelmann, 1995), which are sensitive to anisotropy close to the receivers. In the following, we will discuss these arguments and subsequently show that the Hudson model may in fact give a good fit to the splitting delay data of Vav- 653 654 Comments and Replies pressure is somewhat...

...) for the Gr~ifenberg and GERESS (Harjes, 1990) arrays for explosions on Mururoa (top) and Fangataufa (bottom). The stations of the 13-element GRF array have been rotated into a common plane; only the theoretical seismogram for the center element GEC2 was calculated for the small-aperture GERESS array...

..., it is suggested to take into account the vertical slowness during the slowness estimation as Bokelmann (1995) did for the GERESS array or make static corrections before the slowness estimation as Lindquist et al. (2007) and Tibuleac and Stroujkova (2009) did. Thirdly, one may notice that there are some...