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GERES array

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Comparison of synthetic vertical P‐wave array beams (black lines) computed for different source depth and observations (gray lines) at (a) the GERES, Germany and (b) Alice Springs, Australia, seismic arrays. Waveforms are aligned so that time 0 corresponds to the first P onset.
Published: 11 January 2017
Figure 8. Comparison of synthetic vertical P ‐wave array beams (black lines) computed for different source depth and observations (gray lines) at (a) the GERES, Germany and (b) Alice Springs, Australia, seismic arrays. Waveforms are aligned so that time 0 corresponds to the first P onset.
Image
Comparison of observed (solid line) and synthetic vertical P‐wave displacement array beams at the GERES, Germany, and Alice Springs, Australia, seismic arrays for two competing source models: model 1 (dashed line) was computed for the best MT solution out of the amplitude spectra inversion, model 2 (dotted line) corresponds to a competing MT, dominated by a negative CLVD.
Published: 11 January 2017
Figure 7. Comparison of observed (solid line) and synthetic vertical P ‐wave displacement array beams at the GERES, Germany, and Alice Springs, Australia, seismic arrays for two competing source models: model 1 (dashed line) was computed for the best MT solution out of the amplitude spectra
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Mainshock location result obtained using (a) the stacking method (for the epicenter) and (b) the array beam method (for the depth). (a) Coherence matrix representation: yellow and dark blue colors indicate high and low coherence, respectively (see color scale). The X and Y axes (in kilometer) are along the east–west and north–south directions, respectively. The coordinate system origin (0, 0) corresponds to (43.65° N, 13.05° E). (b) Depth estimation of the mainshock from regional array beam modeling using the seismic array GERES in Germany (Fig. S1). The synthetic waveforms (gray) are the modeled waveforms, assuming the events occurred at various depths from 3 to 11 km, with an increment of 1 km. The observed waveform (blue) is the seismogram of the mainshock observed by the array. By visually comparing the observed waveform with the synthetic waveforms, the depth of the mainshock is constrained at 6.5 km. The color version of this figure is available only in the electronic edition.
Published: 29 April 2024
(in kilometer) are along the east–west and north–south directions, respectively. The coordinate system origin (0, 0) corresponds to (43.65° N, 13.05° E). (b) Depth estimation of the mainshock from regional array beam modeling using the seismic array GERES in Germany (Fig. S1). The synthetic waveforms (gray
Journal Article
Published: 01 August 2008
Bulletin of the Seismological Society of America (2008) 98 (4): 1876–1886.
... ) or the GERES ( Harjes, 1990 ) array. A simple recipe on how to conduct such a study can be found in Schweitzer et al. (2002) . However, the calculation of cross-correlation values between noise samples at single sensors without any time shifts leads to measures of noise coherence that correspond to only one...
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Journal Article
Published: 01 December 1997
Bulletin of the Seismological Society of America (1997) 87 (6): 1576–1597.
... European arrays NORES, detection and phase association based on work by Mykkelt- ARCES, FINES, and GERES. These and arrays with similar veit and Bungum (1984 which yielded azimuth and slow- configurations will be the most capable of the primary in- ness information (Kva~rnaand Doornbos, 1986). In addition...
Journal Article
Published: 11 January 2017
Seismological Research Letters (2017) 88 (2A): 300–310.
...Figure 8. Comparison of synthetic vertical P ‐wave array beams (black lines) computed for different source depth and observations (gray lines) at (a) the GERES, Germany and (b) Alice Springs, Australia, seismic arrays. Waveforms are aligned so that time 0 corresponds to the first P onset. ...
FIGURES | View All (9)
Journal Article
Published: 01 June 1994
Bulletin of the Seismological Society of America (1994) 84 (3): 806–816.
... on the Imperial and Superstition Hills faults trig- gered by the Westmodand, California, earthquake of 26 April Burford, R. O. and P. W. Harsh (1980). Slip on the San Andreas 1981, Bull. Seism. Soc. Am. 76, 949-965. fault in central California from alignment array surveys, Bull. Sharp, R. V., M. J. Rymer, and D...
Journal Article
Published: 23 March 2016
Seismological Research Letters (2016) 87 (3): 719–725.
... will consist of a set of vertices that defines the positions of the corners of the triangles. If a model is comprised of more than one multilevel tessellation, they will share common vertices, to the extent possible. Data arrays: Each data array is a 1D array of data values that may be of type double...
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Journal Article
Published: 01 November 2003
Seismological Research Letters (2003) 74 (6): 791–802.
... organization, known as the prototype IDC or pIDC. Waveform data are collected by the IMS seismic network, which contains a combination of three-component seismic stations and multi-instrument seismic arrays ( Figure 1 ). For the latter, signal-to-noise ratios are enhanced through beam forming. A subset...
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Journal Article
Published: 01 August 2010
Bulletin of the Seismological Society of America (2010) 100 (4): 1779–1784.
...Neil D. Selby Abstract Waveform data recorded at seven of the International Monitoring System ( IMS ) seismometer arrays are used to measure the relative times of teleseismic P signals with three methods: analyst picks, and two methods that make full use of the capabilities of seismometer arrays...
FIGURES
Journal Article
Published: 13 October 2021
Seismological Research Letters (2022) 93 (1): 33–44.
... in the area and distant ones like the GERES array, about 22° away. Figure 2. An aerial image showing the devastation of Beirut port facilities following the 4 August 2020 chemical explosion (3, Data and Resources ). Beirut is located at the eastern shore of the Mediterranean Sea. Figure  3...
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Journal Article
Published: 15 March 2016
Bulletin of the Seismological Society of America (2016) 106 (2): 435–452.
... performance on a network of arrays in terms of efficiency. We performed a large‐scale test of dynamic correlation processors on an 11 TB global dataset using 25 arrays in the 1–3 Hz frequency band. The system found over 3.2 million unique signals and produced 459,747 screened detections. A very satisfying...
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Journal Article
Journal: Paleobiology
Published: 01 January 2007
Paleobiology (2007) 33 (1): 116–124.
... of quantifying diversity that offers much potential to the study of the fossil record, and has been used to examine diversity patterns in a number of modern ecological studies (e.g., Wagner et al. 2000 ; Gering and Crist 2002 ; Crist et al. 2003 ; Okuda et al. 2004 ). Although the concept of additive...
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Journal Article
Published: 01 April 2012
Bulletin of the Seismological Society of America (2012) 102 (2): 867–872.
... ) in Alice Springs, Australia ( ASAR ), Haidmühle, Germany ( GERES ), and Mina, United States ( NVAR ), which are part of the International Monitoring System, are processed following Selby (2010) , where the array beam b at data point i is given by (1) where K is the number of channels...
FIGURES
Journal Article
Published: 01 August 2011
Bulletin of the Seismological Society of America (2011) 101 (4): 1563–1575.
... of the 10-min segments; unlike at the IDC , there is no finer-grained assessment of data quality. Table 1 Apertures and Number of Elements of the Arrays Used in This Study Station Aperture (km) Elements ARCES 3.12 25 BRTR 3.69 6 FINES 2.02 16 GERES 3.92 24 MKAR...
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Journal Article
Published: 29 April 2024
Seismological Research Letters (2024) 95 (5): 2779–2790.
... (in kilometer) are along the east–west and north–south directions, respectively. The coordinate system origin (0, 0) corresponds to (43.65° N, 13.05° E). (b) Depth estimation of the mainshock from regional array beam modeling using the seismic array GERES in Germany (Fig. S1). The synthetic waveforms (gray...
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Journal Article
Published: 01 February 1995
Bulletin of the Seismological Society of America (1995) 85 (1): 93–99.
... because of the lack of direct measurement of landslide behavior during seismic shaking. Two permanent instrument arrays have been installed on seismically active landslides to simultaneously record acceleration, pore pressure, and permanent landslide displacement, which will permit more accurate modeling...
Journal Article
Published: 01 June 1994
Bulletin of the Seismological Society of America (1994) 84 (3): 863–891.
... the largest events that were trig- shear and/or dilatational strains (and stresses) radiated gered by the Landers earthquake. Magnitude estimates from the Landers earthquake. We estimate the ampli- are also sensitive to network coverage (e.g., Haber- tudes of the dynamic strains from Landers and other re...
Journal Article
Published: 01 June 1994
Bulletin of the Seismological Society of America (1994) 84 (3): 835–843.
... J. B. Baker L. (1994) . Transient stresses at Parkfield, California, produced by the M 7.4 Landers earthquake of June 28, 1992: observations from the Upsar dense seismograph array , J. Geophys. Res. (submitted...
Journal Article
Journal: Paleobiology
Published: 01 May 2007
Paleobiology (2007) 33 (2): 295–309.
... a taxonomically and ecologically diverse array of marine invertebrates, including corals, bryozoans, brachiopods, mollusks, arthropods, and echinoderms ( Holland 1997 ). The invasion spans at least two depositional sequences and may have lasted 1–2 Myr, suggesting that the climatic shifts responsible...
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