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  • GFZ German Research Centre for Geos...

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    Authors: Antico, P.; Vera, J.; Pasquaré, A.; Galván, R.; +5 Authors

    Surface air temperature measurements obtained from different sensors are used to construct a unique time series with one minute time-interval. Apart from differences in design and environmental exposition, periods of missing data also exist in the data series of each sensor. A primary data set was selected in terms of quality and temporal extension. A combination of two different techniques is applied to complete this data set: one is based on the autocorrelation of the series and the other on measurements taken from other sensors. The resulting values constitute a complete series of surface air temperature at AGGO.

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    Authors: Marcelo Bianchi; Peter Evans; Andres Heinloo; J. Quinteros;
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    Authors: Boese, C.; Kwiatek, G.; Fischer, T.; Plenkers, K.; +1 Authors

    In 2020 and 2021 the STIMTEC-X hydraulic stimulation experiment was performed at ca.~130 m below surface at the Reiche Zeche underground research laboratory in Freiberg, Saxony/Germany. The project temporally followed the STIMTEC experiment at the same site and aimed at understanding the stress heterogeneity of the anisotropic and metamorphic gneiss rock mass. The STIMTEC-X experiment applied the hydraulic stimulation technique in several boreholes at the mine-scale. Complementary to the stimulations, there were active seismic ultrasonic transmission data acquired before the stimulations. We use a seismic monitoring network consisting of six single-component acoustic emission (AE) sensors (sensitivity 1-60 kHz), six hydrophone-like AE sensors (sensitivity 1-40 kHz) and four to twelve single-component Wilcoxon accelerometers (sensitivity 50 Hz-25 kHz). The AE sensors and remained stationary in sub-horizontal and upwards reaching boreholes, the accelerometers were mostly installed along the tunnel walls with one accelerometer in a shallow borehole in each tunnel, and the hydrophone-like AE sensors were installed in the down-going water filled boreholes, but repositioned for each measurement campaign (Figure 1). This data set of 120 active ultrasonic transmission (UT) measurements is supplementary to Boese et al. (2022, in review), which introduces some of the active measurement campaigns of the STIMTEC-X experiment in detail. The whole data set togetter with the “Ultrasonic transmission measurements from six boreholes from the STIMTEC experiment, Reiche Zeche Mine, Freiberg (Saxony, Germany)” [https://doi.org/10.5880/GFZ.4.2.2021.002] was used to evaluate performance measures such as sensitivity and frequency bandwith, coupling, placement and polarity of the hydrophone-like AE sensor compared to AE sensors. The active seismic data provided here are from seven boreholes (BH01, BH05, BH06, BH10, BH14, BH18, BH19) as shown in Figure 1. There are nine tables provided as metadata of which seven contain the STIMTEC-X sensor coordinates for each measurement campaign, the event information of all the 120 UT measurements and the UT picks. The UT measurements were recorded with a sampling rate of 1 MHz and results from an automatic stack of 1024 UT pulses generated by the ultrasonic transmitter and recorded by the STIMTEC-X sensors. The UT measurements are saved in binary file format (fsf file format). Fsf-files can be processed with FOCI software: https://www.induced.pl/software/foci. Each fsf file contains 32768 samples, which corresponds to 0.032768 seconds. All UT event files were manual inspected and phase arrivals identified. These are stored in the fsf-file header as well as in the table STIMTECX_UT_picks.csv.

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    Authors: Morales, J.; Martín, J.; Martín, R.; Mancilla Perez, F.; +2 Authors

    We carried out a passive experiment operated with 10 broadband and short period seismic stations which were installed between July 2013 and May 2015 by a joint effort between the Instituto Andaluz de Geofísica, Granada University and the German Research Centre for Geosciences GFZ. The goal of this project is to study the crustal and upper mantle structures under the Central Betic mountain ranges and the variations of these structures between the different geological domains as a prolongation towards the north of the HIRE profile (Heit, Yuan and Mancilla; 2010). Waveform data is available from the GEOFON data centre, under network code 3J.

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    Authors: M. Ziegler;
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    Authors: Sippl, C.; Schurr, B.; Asch, G.; Kummerow, J.;

    The present dataset is a comprehensive earthquake catalogue for the Northern Chile subduction zone forearc, determined from IPOC seismic station data (GFZ and CNRS-INSU 2006; http://doi.org/10.14470/PK615318) plus some auxiliary stations (IPOC = Integrated Plate Boundary Observatory Chile; http://www.ipoc-network.org). The method of automatized earthquake catalogue retrieval, the different relocation steps as well as the different earthquake class labels and the structures outlined by the seismicity are described in detail in Sippl et al. (2018). Unlike the catalogue that is supplied as a supplementary file with said paper, this record here will grow over the years, i.e. data from additional years beyond 2014, processed in the same way, will be added. The columns of the data files are: year, month, day, hour, minute, second, latitude [dec. degrees], longitude [dec. degrees], depth [km], magnitude [ML], identifier The identifier term provides a first-order spatial classification of the seismicity, an explanation is given in Table 1 of Sippl et al. (2018).

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    Authors: Gottschalk, M.;

    This data publication reports results of Monte-Carlo simulations, configurations, pair-, and triplet-correlation functions for a Lennard-Jones fluid. The Lennard-Jones potential (Jones 1924) u^LJ is one of the prototypes of an intermolecular interaction. Gottschalk (2019) performed 32705 NVT Monte-Carlo simulations using 1372 LJ particles (N) for a large number of densities rho a and temperatures T. The simulations range from 0.002 ≤ rho* ≤ 1.41 and 0.45 ≤ T* ≤ 25 using a cut-off of 5.0 for rho* ≤ 1.37 and 4.5 for rho* > 1.37, respectively. At each state point, 1372 LJ particles (N = 1372) were equilibrated using 5 x 10^4 cycles and subsequently sampled for 0.75 x 10^6 cycles. One cycle did consist of 1372 trial moves, one for each particle. Every 1000 cycles the thermodynamic properties U* and p* are recorded as well as the current configuration of particles including the pair- and triplet-correlation functions. A total of 27615 of these simulations were in the stable and metastable single fluid phase field which is a necessary requirement. Field boundaries, U*, p* and further details of the Monte-Carlo simulations are given in Gottschalk (2019). Bin widths of 0.005 for pair- and 0.04 in all directions for triplet-correlation functions were used. Further details for the calculations of the pair- and triplet-correlation functions are presented in Gottschalk (2021). All configurations of particles, pair- and triplet-correlation functions of those 27615 simulations are reported here. However, the total amount of data for configurations, pair-, and triplet-configurations is 600, 0.3, and 1170 GB, respectively. The data are provided as zipped files and described in the data description and the associated Read-me.txt. All rho* and T* state points are listed in the file Conditions.txt in the top level of the files.

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    Authors: Mayer-Gürr, T.; Behzadpur, S.; Ellmer, M.; Kvas, A.; +3 Authors
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    Authors: S. Itzerott; Christian Hohmann; Vivien Stender; Holger Maass; +6 Authors
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    Authors: Becker, D.; Martinez Garzon, P.; Wollin, C.; Kılıç, T.; +1 Authors

    The dataset is an extended and updated version of the homogenized regional earthquake catalogue of the Marmara region, north-western Turkey, presented in Bohnhof et al. (2017) and Wollin et al. (2018). It is built on the regional Turkish seismicity catalogues provided by AFAD (Disaster and Emergency Management Presidency of Turkey) and KOERI (Kandilli Observatory and Earthquake Research Institute) and spans the time interval 2006-2020. All events available in these two catalogues in the wider Marmara region were combined and dublicate events removed. A total of 13812 events having at least 6 P- and/or S-picks were located using the NLLoc software (Lomax et al., 2000, 2009) in Octtree mode utilizing automatic picks (see Wollin et al., 2018 for details) for all available waveforms. The magnitude range is between M0.3 and M5.7 with time-variable magnitude of completeness and covers the area 39.70S-41.50S and 26.0E-30.65E. The full description of the data and methods is provided in the data description file.

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    Authors: Antico, P.; Vera, J.; Pasquaré, A.; Galván, R.; +5 Authors

    Surface air temperature measurements obtained from different sensors are used to construct a unique time series with one minute time-interval. Apart from differences in design and environmental exposition, periods of missing data also exist in the data series of each sensor. A primary data set was selected in terms of quality and temporal extension. A combination of two different techniques is applied to complete this data set: one is based on the autocorrelation of the series and the other on measurements taken from other sensors. The resulting values constitute a complete series of surface air temperature at AGGO.

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    Authors: Marcelo Bianchi; Peter Evans; Andres Heinloo; J. Quinteros;
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    Authors: Boese, C.; Kwiatek, G.; Fischer, T.; Plenkers, K.; +1 Authors

    In 2020 and 2021 the STIMTEC-X hydraulic stimulation experiment was performed at ca.~130 m below surface at the Reiche Zeche underground research laboratory in Freiberg, Saxony/Germany. The project temporally followed the STIMTEC experiment at the same site and aimed at understanding the stress heterogeneity of the anisotropic and metamorphic gneiss rock mass. The STIMTEC-X experiment applied the hydraulic stimulation technique in several boreholes at the mine-scale. Complementary to the stimulations, there were active seismic ultrasonic transmission data acquired before the stimulations. We use a seismic monitoring network consisting of six single-component acoustic emission (AE) sensors (sensitivity 1-60 kHz), six hydrophone-like AE sensors (sensitivity 1-40 kHz) and four to twelve single-component Wilcoxon accelerometers (sensitivity 50 Hz-25 kHz). The AE sensors and remained stationary in sub-horizontal and upwards reaching boreholes, the accelerometers were mostly installed along the tunnel walls with one accelerometer in a shallow borehole in each tunnel, and the hydrophone-like AE sensors were installed in the down-going water filled boreholes, but repositioned for each measurement campaign (Figure 1). This data set of 120 active ultrasonic transmission (UT) measurements is supplementary to Boese et al. (2022, in review), which introduces some of the active measurement campaigns of the STIMTEC-X experiment in detail. The whole data set togetter with the “Ultrasonic transmission measurements from six boreholes from the STIMTEC experiment, Reiche Zeche Mine, Freiberg (Saxony, Germany)” [https://doi.org/10.5880/GFZ.4.2.2021.002] was used to evaluate performance measures such as sensitivity and frequency bandwith, coupling, placement and polarity of the hydrophone-like AE sensor compared to AE sensors. The active seismic data provided here are from seven boreholes (BH01, BH05, BH06, BH10, BH14, BH18, BH19) as shown in Figure 1. There are nine tables provided as metadata of which seven contain the STIMTEC-X sensor coordinates for each measurement campaign, the event information of all the 120 UT measurements and the UT picks. The UT measurements were recorded with a sampling rate of 1 MHz and results from an automatic stack of 1024 UT pulses generated by the ultrasonic transmitter and recorded by the STIMTEC-X sensors. The UT measurements are saved in binary file format (fsf file format). Fsf-files can be processed with FOCI software: https://www.induced.pl/software/foci. Each fsf file contains 32768 samples, which corresponds to 0.032768 seconds. All UT event files were manual inspected and phase arrivals identified. These are stored in the fsf-file header as well as in the table STIMTECX_UT_picks.csv.

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    Authors: Morales, J.; Martín, J.; Martín, R.; Mancilla Perez, F.; +2 Authors

    We carried out a passive experiment operated with 10 broadband and short period seismic stations which were installed between July 2013 and May 2015 by a joint effort between the Instituto Andaluz de Geofísica, Granada University and the German Research Centre for Geosciences GFZ. The goal of this project is to study the crustal and upper mantle structures under the Central Betic mountain ranges and the variations of these structures between the different geological domains as a prolongation towards the north of the HIRE profile (Heit, Yuan and Mancilla; 2010). Waveform data is available from the GEOFON data centre, under network code 3J.

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    Authors: M. Ziegler;
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    Authors: Sippl, C.; Schurr, B.; Asch, G.; Kummerow, J.;

    The present dataset is a comprehensive earthquake catalogue for the Northern Chile subduction zone forearc, determined from IPOC seismic station data (GFZ and CNRS-INSU 2006; http://doi.org/10.14470/PK615318) plus some auxiliary stations (IPOC = Integrated Plate Boundary Observatory Chile; http://www.ipoc-network.org). The method of automatized earthquake catalogue retrieval, the different relocation steps as well as the different earthquake class labels and the structures outlined by the seismicity are described in detail in Sippl et al. (2018). Unlike the catalogue that is supplied as a supplementary file with said paper, this record here will grow over the years, i.e. data from additional years beyond 2014, processed in the same way, will be added. The columns of the data files are: year, month, day, hour, minute, second, latitude [dec. degrees], longitude [dec. degrees], depth [km], magnitude [ML], identifier The identifier term provides a first-order spatial classification of the seismicity, an explanation is given in Table 1 of Sippl et al. (2018).

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    Authors: Gottschalk, M.;

    This data publication reports results of Monte-Carlo simulations, configurations, pair-, and triplet-correlation functions for a Lennard-Jones fluid. The Lennard-Jones potential (Jones 1924) u^LJ is one of the prototypes of an intermolecular interaction. Gottschalk (2019) performed 32705 NVT Monte-Carlo simulations using 1372 LJ particles (N) for a large number of densities rho a and temperatures T. The simulations range from 0.002 ≤ rho* ≤ 1.41 and 0.45 ≤ T* ≤ 25 using a cut-off of 5.0 for rho* ≤ 1.37 and 4.5 for rho* > 1.37, respectively. At each state point, 1372 LJ particles (N = 1372) were equilibrated using 5 x 10^4 cycles and subsequently sampled for 0.75 x 10^6 cycles. One cycle did consist of 1372 trial moves, one for each particle. Every 1000 cycles the thermodynamic properties U* and p* are recorded as well as the current configuration of particles including the pair- and triplet-correlation functions. A total of 27615 of these simulations were in the stable and metastable single fluid phase field which is a necessary requirement. Field boundaries, U*, p* and further details of the Monte-Carlo simulations are given in Gottschalk (2019). Bin widths of 0.005 for pair- and 0.04 in all directions for triplet-correlation functions were used. Further details for the calculations of the pair- and triplet-correlation functions are presented in Gottschalk (2021). All configurations of particles, pair- and triplet-correlation functions of those 27615 simulations are reported here. However, the total amount of data for configurations, pair-, and triplet-configurations is 600, 0.3, and 1170 GB, respectively. The data are provided as zipped files and described in the data description and the associated Read-me.txt. All rho* and T* state points are listed in the file Conditions.txt in the top level of the files.

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    Authors: Mayer-Gürr, T.; Behzadpur, S.; Ellmer, M.; Kvas, A.; +3 Authors
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    Authors: S. Itzerott; Christian Hohmann; Vivien Stender; Holger Maass; +6 Authors
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    Authors: Becker, D.; Martinez Garzon, P.; Wollin, C.; Kılıç, T.; +1 Authors

    The dataset is an extended and updated version of the homogenized regional earthquake catalogue of the Marmara region, north-western Turkey, presented in Bohnhof et al. (2017) and Wollin et al. (2018). It is built on the regional Turkish seismicity catalogues provided by AFAD (Disaster and Emergency Management Presidency of Turkey) and KOERI (Kandilli Observatory and Earthquake Research Institute) and spans the time interval 2006-2020. All events available in these two catalogues in the wider Marmara region were combined and dublicate events removed. A total of 13812 events having at least 6 P- and/or S-picks were located using the NLLoc software (Lomax et al., 2000, 2009) in Octtree mode utilizing automatic picks (see Wollin et al., 2018 for details) for all available waveforms. The magnitude range is between M0.3 and M5.7 with time-variable magnitude of completeness and covers the area 39.70S-41.50S and 26.0E-30.65E. The full description of the data and methods is provided in the data description file.

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