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  • EARTH SCIENCE 〉 SOLID EARTH  (16)
  • General Chemistry
  • Seismology
  • GFZ Data Services  (17)
  • Lawrence Livermore National Laboratory  (5)
  • 2020-2024  (17)
  • 1985-1989  (5)
  • 1950-1954
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  • 1
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    Lawrence Livermore National Laboratory
    In:  Proceedings of the 1986 RSTN/NORESS Research Symposium, Luxembourg, Lawrence Livermore National Laboratory, vol. 76, no. 1, pp. 33-58, pp. B05311, (ISSN: 1340-4202)
    Publication Date: 1986
    Keywords: Seismology ; Detectors ; Seismic arrays
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  • 2
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    Lawrence Livermore National Laboratory
    In:  1986 RSTN / NORESS Research Symposium, Berkeley, Lawrence Livermore National Laboratory, vol. C 560, 183 pp., no. 89-0684, 26 pp., pp. 59-76, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Seismology ; Seismic arrays ; Data analysis / ~ processing ; Kvaerna
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  • 3
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    Lawrence Livermore National Laboratory
    In:  report, Arlington, Virginia, Lawrence Livermore National Laboratory, vol. 10, no. UCID-21047, pp. 484-486, (ISBN 3-933346-037)
    Publication Date: 1987
    Keywords: Nuclear explosion ; Frequency ; NOISE ; Seismology
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  • 4
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    Lawrence Livermore National Laboratory
    In:  Proceedings of the 1986 RSTN/NORESS Research Symposium, Hannover, Lawrence Livermore National Laboratory, vol. C 560, 183 pp., no. AFGL-TR-88-0149, pp. 77-99, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Seismology ; Detectors ; Seismic arrays
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  • 5
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    Lawrence Livermore National Laboratory
    In:  informal report, Livermore, Lawrence Livermore National Laboratory, vol. 339-350, no. UCID-20642, pp. 344, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Seismology ; Discrimination ; Nuclear explosion ; Magnitude
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  • 6
    Publication Date: 2023-02-09
    Description: Abstract
    Description: In September 2017 three crustal-scale seismic profiles were acquired in southern Iran covering the subaerial accretionary wedge of the western part of the Makran Subduction zone. Each of the roughly north-south trending profiles was approximately 200 km long, and on each profile 9 to 10 artificial shots with charges between 400 and 800 kg of explosives were fired. The seismic signals were observed by 300 autonomous digital recorders with geophones on each profile. This dataset consists of the raw (continuous) data of the recorders (in proprietary cube format and MSEED-format) and the shot records in SEGY-format (standard exchange formats).
    Description: Other
    Description: The Geophysical Instrument Pool Potsdam (GIPP) provides field instruments for (temporary) seismological studies (both controlled source and earthquake seismology) and for magnetotelluric (electromagnetic) experiments. The GIPP is operated by the GFZ German Research Centre for Geosciences. The instrument facility is open for academic use. Instrument applications are evaluated and ranked by an external steering board. See Haberland and Ritter (2016) and https://www.gfz-potsdam.de/gipp for more information.
    Keywords: subduction zone ; accretionary wedge ; Makran ; deep seismic sounding ; crustal structure ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WIDE-ANGLE_REFLECTION_REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 EXPLOSION_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WEIGHT-DROP_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 CRUSTAL_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REGIONAL_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 DSS ; SENSOR 〉 GEOPHONE ; SENSOR 〉 VERTICAL_COMPONENT ; LAND ; SEG-Y_DATA_FORMAT ; MINISEED_DATA_FORMAT ; SEISMIC_WAVEFORM_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 RAW_DATA ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE ; In Situ/Laboratory Instruments 〉 Profilers/Sounders 〉 SEISMIC REFLECTION PROFILERS
    Type: Dataset , Dataset
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  • 7
    Publication Date: 2023-03-31
    Description: Abstract
    Description: This data repository contains the IGMAS+ (Gotze and Lahmeyer, 1988; Schmidt et al., 2011, 2020) files of the four end-member structural and density models used to analyze the rift architecture of the Red Sea. The user can directly open the files in IGMAS+ (https://igmas.git-pages.gfz-potsdam.de/igmas-pages/, accessed 12.08.2022) to explore the gravity response of these configurations. The end-member scenarios include two end-type margin architectures following Huismans and Beaumont (2011): Type I - outlined by narrow regions (less than about 100 km wide) of thinned continental crust and exhumed (and serpentinized) continental lithospheric mantle along the continent-ocean transition, and Type II - outlined by (ultra)wide regions (up to 500 km) of thin continental crust and the removal of the lithospheric mantle. In addition, we include two options for distribution of oceanic crust in the Red Sea: limited - confined only to regions of magnetic stripes following Schettino et al. (2016), and extended - in which oceanic crust is available in vast areas within the basin, following Augustin et al. (2021).
    Keywords: Red Sea ; Lithospheric configuration ; Rift architecture ; 3D gravity models ; EARTH SCIENCE ; EARTH SCIENCE 〉 OCEANS 〉 MARINE GEOPHYSICS 〉 MARINE GRAVITY FIELD ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS
    Type: Model , Model
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  • 8
    Publication Date: 2023-06-12
    Description: Abstract
    Description: This dataset includes paleomagnetic and rock magnetic analyses from four sediment cores collected on continental slope of Storfjorden (EG-02, EG-03, SV-04) and Kveithola (GeoB17603-3) trough‐mouth fans and two cores collected at the crest of the Bellsund (GS191-01PC) and Isfjorden (GS191-02PC) sediment drifts (NW Barents Sea). The dataset gave the opportunity to reconstruct variation of past geomagnetic field at high latitude for the last 22 kya and define the path of the virtual geomagnetic pole (VGP). Data are presented as two metadata table: one with definitions of the column heads and one with the core details; six tables with the data on the measured rock magnetic and paleomagnetic parameters and 3 tables with the results of data analyses and elaboration. List of tables is as follows: 1) Metadata: definition of columns heads; 2) Metadata: core details; 3) GS191-01PC: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core GS191-01PC; 4) GS191-02PC: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core GS191-02PC; 5) EG03: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core EG03; 6) EG02: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core EG02; 7) SV04: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core SV04; 8) GeoB17603-3: down-core variation of rock magnetic and paleomagnetic parameters [k (10E-05 SI); ARM (A/m); MDF (mT); NRM (A/m); MAD (°); Incl PCA (°); Decl PCA (°)] for Core GeoB17603-3; 9) Cores Correlation: GS191-01PC depth (cm) and ARM (A/m) down-core variations for core GS191-01PC (master core); GS191-02PC depth (cm), GS191-02PC depth transferred to GS191-01PC depth (cm), ARM (A/m) down-core for core GS191-02PC and correlation tie points; GeoB17603-3 depth (cm), GeoB17603-3 depth transferred to GS191-01PC depth (cm), ARM (A/m) down-core for core GeoB17603-3 and correlation tie points; EG02 depth (cm), EG02 depth transferred to GS191-01PC depth (cm), ARM (A/m) down-core for core EG02 and correlation tie points; EG03 depth (cm), EG03 depth transferred to GS191-01PC depth (cm), ARM (A/m) down-core and correlation tie points; SV04 depth (cm), SV04 transferred to GS191-01PC (cm), ARM (A/m) down-core for core SV04 and correlation tie points; 10) Age model: age model for Core GS191-01PC; GS191-02PC; EG02; EG03; SV04 and correlation tie points; 11) NBS stack: paleomagnetic inclination, declination and RPI variations for NBS22.2k stack. In order to define high-resolution correlation between the cores the along-core variation of rock magnetic and paleomagnetic parameters (Sagnotti et al., 2011; Caricchi et al., 2018; Caricchi et al., 2019) have been integrated with the distribution of characteristic lithofacies (Lucchi et al., 2013), and the available age constraints (Sagnotti et al., 2011; Caricchi et al., 2018, Caricchi et al., 2019; Caricchi et al., 2020). Core to core correlation has been reconstructed by means of the StratFit software (Sagnotti and Caricchi, 2018), which is based on the Excel forecast function and linear regression between subsequent couples of selected tie-points. The data are presented as one Excel sheet with eleven tables and in tab-delimited ASCII format in the zip folder: 2022-028_Caricchi-et-al_data-txt.zip.
    Description: SeriesInformation
    Description: Supplement to Caricchi, C., Campuzano S.A., Sagnotti L., Macrì P., Lucchi R.G. (2022) Reconstruction of the Virtual Geomagnetic Pole (VGP) path at high latitude for the last 22 kyr: the role of radial field flux patches as VGP attractor. EPSL
    Keywords: Geomagnetic paleosecular variation ; Relative paleointensity ; Flux lobes ; Levantine Iron Age Anomaly ; Marine sediment cores ; Arctic region ; Paleomagnetism ; Rock magnetism ; EPOS ; multi-scale laboratories ; Core ; Quaternary ; Paleomagnetic data ; Demagnetization type AF ; sedimentary core ; Barents Sea ; Svalbard Arcipelago ; Fram Straits ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 PALEOMAGNETIC DATA ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 STRATIGRAPHIC SEQUENCE ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 MAGNETIC FIELD ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 PALEOMAGNETISM ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 SEDIMENTS
    Type: Dataset , Dataset
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  • 9
    Publication Date: 2023-06-12
    Description: Abstract
    Description: During the 2018 “Mackenzie Delta Permafrost Field Campaign” (mCan2018), a test campaign within the “Modular Observation solutions for Earth Systems” (MOSES) program, ambient seismic noise recordings at the sea bottom were acquired along two 300 m long transects from the shoreline to shallow marine area close to Tuktoyaktuk Island (Canada). In total, 21 measurements were taken. Raw data is provided in proprietary “Cube” format and standard mseed format.
    Keywords: MOSES ; Modular Observation solutions for Earth Systems ; submarine permafrost ; ambient seismic noise ; H/V measurements ; Mackenzie Delta ; PASSIVE_SEISMIC 〉 STATIONS ; SENSOR 〉 OCEAN_BOTTOM_SEISMOMETER ; SENSOR 〉 3-C ; MARINE ; MINISEED_DATA_FORMAT ; SEISMIC_WAVEFORM_DATA ; EARTH SCIENCE 〉 CRYOSPHERE 〉 FROZEN GROUND 〉 PERMAFROST ; EARTH SCIENCE 〉 OCEANS 〉 MARINE GEOPHYSICS ; EARTH SCIENCE 〉 SOLID EARTH ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Dataset
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  • 10
    Publication Date: 2023-06-21
    Description: Abstract
    Description: This data publication contains part of a seismic survey collected across the Ivrea Zone, Italy, in October 2020. Within the research project SEIZE (SEismic Imaging of the Ivrea ZonE), this high-resolution seismic campaign investigates the upper 5 km of the subsurface under and around the commune of Balmuccia (Val Sesia, Piemont region). The aim is to provide the best in situ geophysical image and physical properties of the subsurface as well as to calibrate future observations made during the planned ICDP drilling (https://www.icdp-online.org/projects/by-continent/europe/dive-italy, http://www.dive2ivrea.org/). Seismic Data, including raw, mini-seed and SEG-Y files, of a part of a controlled-source 3D survey in Northern Italy, Ivrea Zone, based on 432 Vibroseis sources recorded by a fixed spread of 110 receivers.
    Keywords: Geophysics ; controlled-source seismic survey ; Alps ; Vibroseis ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REFLECTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WIDE-ANGLE_REFLECTION_REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 VIBRO_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 LOCAL_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 RESERVOIR_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 NEAR_SURFACE ; SENSOR 〉 GEOPHONE ; SENSOR 〉 VERTICAL_COMPONENT ; SENSOR 〉 3-C ; SEG-Y_DATA_FORMAT ; SEISMIC_WAVEFORM_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 RAW_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 CORRELATED_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 VERTICALLY_STACKED_DATA ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE
    Type: Dataset , Dataset
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  • 11
    Publication Date: 2023-09-01
    Description: Abstract
    Description: We present a new, consistently processed seismicity catalogue for the Eastern and Southern Alps, based on the temporary dense Swath-D monitoring network. The final catalogue includes 6,053 earthquakes for the time period 2017-2019 and has a magnitude of completeness of −1.0ML. The smallest detected and located events have a magnitude of −1.7ML. Aimed at the low to moderate seismicity in the study region, we generated a multi-level, mostly automatic workflow which combines a priori information from local catalogues and waveform-based event detection, subsequent efficient GPU-based event search by template matching, P & S arrival time pick refinement and location in a regional 3-D velocity model. The resulting seismicity distribution generally confirms the previously identified main seismically active domains, but provides increased resolution of the fault activity at depth. In particular, the high number of small events additionally detected by the template search contributes to a more dense catalogue, providing an important basis for future geological and tectonic studies in this complex part of the Alpine orogen.
    Description: TableOfContents
    Description: Seismicity catalogue Python codes & metadata Seismicity cross-sections
    Keywords: Seismology ; Seismic Waveform Analysis ; Eastern Alps ; Earthquake ; Geophysics ; Template matching ; 4DMB ; 4D Mountain Building ; EARTH SCIENCE ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE MAGNITUDE/INTENSITY ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES ; geophysics ; seismology ; surface processes ; tectonics
    Type: Dataset , Dataset
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  • 12
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    GFZ Data Services
    Publication Date: 2023-10-10
    Description: Abstract
    Description: In order to test the feasibility of density and viscosity models suitable to explain geoid and dynamic topography in West Antarctica, we perform computations of a thermal plume that enters at the base of a cartesian box corresponding to a region in the upper mantle, as well as some whole-mantle thermal plume models, as well as some instantaneous disk models, with ASPECT. The plume models have typically a narrow conduit and the plume tends to only become wider as it spreads beneath the lithosphere, typically shallower than ~300 km. These results are most consistent with a shallow disk model with reduced uppermost mantle viscosity, hence providing further support for such low viscosities beneath West Antarctica. The data are a supplement to the following article: Steinberger, B., Grasnick, M.-L. & Ludwig, R., Exploring the Origin of Geoid Low and Topography High in West Antarctica: Insights from Density Anomalies and Mantle Convection Models, Tektonika, https://doi.org/10.55575/tektonika2023.1.2.35
    Keywords: mantle plume ; hotspot ; mantle flow ; mantle processes ; West Antarctica ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE SERVICES 〉 MODELS
    Type: Dataset , Dataset
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  • 13
    Publication Date: 2023-10-18
    Description: Abstract
    Description: This data publication contains (i) a slab model of the Cascadia subduction zone, derived from receiver functions, parameterized as depth to the three interfaces: t (top), c (central) and m (Moho), in NetCDF format; (ii) the station measurements of all parameters in the model in tabular and Raysum model file format; (iii) the raw receiver functions in SAC format; and (iv) auxiliary scripts for loading and plotting the data. A total of 45,601 individual receiver functions recorded at 298 seismic stations distributed across the Cascadia forearc contributed to the slab model. For each station, 100 s recordings symmetric about the P -wave arrival (i.e. 50 s noise and 50 s signal) of earthquakes with magnitudes between 5.5 and 8, in the distance range between 30 and 100 degree, were downloaded from the Incorporated Research Institutions for Seismology (IRIS) data center, the Northern California Earthquake Data Center (NCEDC), and the Natural Resources Canada Data Center (NRCAN). After quality control, radial and transverse receiver functions were computed through frequency-domain simultaneous deconvolution, with an optimal damping factor found through generalized cross validation. The continental forearc and subducting slab were parameterized as three layers over a mantle half-space, with the subduction stratigraphy bounding interfaces labeled as t (top), c (central) and m (Moho). Synthetic receiver functions were calculated through ray-theoretical modeling of plane-wave scattering at the model interfaces. The thickness, S -wave velocity (VS) and P - to S -wave velocity ratio (VP/VS) of each layer, as well as the common strike and dip of the bottom two layers and the top of the half space (in total 11 parameters) were optimized simultaneously through a simulated annealing global parameter search scheme. The misfit was defined as the anti-correlation (1 minus the cross-correlation coefficient) between the observed and predicted receiver functions, bandpass filtered between 2 and 20 s period duration. In total, 171, 143 and 137 quality A nodes were determined to constrain the t, c and m interfaces, respectively. At the trench, 105 nodes at 3 km below the local bathymetry were inserted to constrain the t and c interfaces, and at 6.5 km deeper to constrain the m interface, representing typical sediment and igneous crustal thicknesses. A spline surface was fitted to these nodes to yield margin-wide depth models. The spline coefficients were found using singular value decomposition, with the nominal depth uncertainties supplied as weights. The solution was damped by retaining the 116, 117, and 116 largest singular values for the t, c and m interfaces, respectively, based on analysis of L-curves and the Akaike information criterion. The data set is the supplemental material to Bloch, W., Bostock, M. G., Audet, P. (2023) A Cascadia Slab Model from Receiver Functions. Geochemistry, Geophysics, Geosystems.
    Keywords: Seismology ; Cascadia ; North America ; Reveiver Functions ; Subduction ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 PLATE BOUNDARIES ; lithosphere ; The Present
    Type: Dataset , Dataset
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  • 14
    Publication Date: 2023-10-30
    Description: Abstract
    Description: This data set contains measurements of an underground hydraulic fracture experiment at Äspö Hard Rock Laboratory in May and June 2015. The experiment tested various injection schemes for rock fracture stimulation and monitored the resulting seismicity. The primary purpose of the experiment is to identify injection schemes that provide rock fracturing while reducing seismicity or at least mitigate larger seismic events. In total, six tests with three different injection schemes were performed in various igneous rock types. Both the injection process and the accompanied seismicity were monitored. For injection monitoring, the water flow and pressure are provided and additional tests for rock permeability. The seismicity was monitored in both triggered and continuous mode during the tests by high-resolution acoustic emission sensors, accelerometers and broadband seismometers. Both waveform data and seismicity catalogs are provided.
    Keywords: hydraulic experiments ; broadband seismic data ; acoustic emissions ; Äspö Hard Rock Laboratory ; borehole images ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
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  • 15
    Publication Date: 2023-12-06
    Description: Abstract
    Description: The Northeast Atlantic (NEA) region has long been a subject of interest due to its complex geological history, particularly regarding the interaction between the Iceland plume and the lithospheric plates. In this data publication, we present a comprehensive three-dimensional structural and density model of the NEA crust and uppermost mantle, consolidating and integrating a wide range of previously fragmented data sets. Our model highlights the influence of the Iceland plume on the region's geological evolution, shedding light on the mechanisms that facilitated the continental breakup between Europe and Laurentia during the earliest Eocene period. The whole workflow and methods are described in Gomez Dacal et al. (2023) and its Supplementary Information.
    Description: TechnicalInfo
    Description: Model coordinates: Model coordinates are given in Equidistant Conic North Atlantic (ECNA): • Projection: Equidistant conic • 1st Standard parallel: 80 • 2st Standard parallel: 70 • Central meridian: -9 • Origin Latitude: 90 • False easting: 805000 • False northing: 3140000 Model dimensions: The horizontal dimensions of the model are 2000 km x 2500 km. The total depth of the model is 300 km. Model bounds in ECNA: Easting: from 0 m to 2000000 m Northing: from 0 m to 2500000 m Model bounds in longitude/latitude (WGS 84): Longitude: from -61° to 54° Latitude: from 60° to 84° Extended model bounds in ECNA: Easting: from -500000 m to 2500000 m Northing: from -500000 m to 3000000 m File description: We provide a set of grid files that collectively allow recreating the 3D geological model which covers the North East Atlantic Ocean and its adjacent areas, including the easternmost area of Greenland, the western coast of Norway, Iceland and Svalbard. The provided structural model consists of 11 units including: (i) sea water and ice; (ii) two layers of sedimentary cover: a shallow and a deep unit; (iii) five crystalline crust units composed of an upper and a lower continental crustal, an oceanic crust and two units of lower crustal bodies (LCB); (iv) two lithospheric mantle units: a continental and an oceanic layer. The structural model has a dimension of 2000 km x 2500 km x 300 km and is provided in regularly spaced grids of 10 km, which are identical for all model units. For the gravity modelling the model limits have been extended by 500 km horizontally in all directions including constraining information for the extended region. The extended model horizons are represented in the density model. Additionally, we provide gravity data, density voxel cube and related tomography data. Files are subdivided into five categories: 1. Structural interface 2. Density model horizon 3. Gravity data 4. Density voxel cube 5. Tomography data
    Keywords: North East Atlantic ; 3D structural model ; georeferenced grids ; crustal structure ; subsurface geology ; layer thickness ; crystalline crust ; lithospheric mantle ; gravity ; tomography ; density ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY ANOMALIES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE 〉 SEISMIC BODY WAVES ; EARTH SCIENCE SERVICES 〉 MODELS ; EARTH SCIENCE SERVICES 〉 MODELS 〉 GEOLOGIC/TECTONIC/PALEOCLIMATE MODELS
    Type: Dataset , Dataset
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  • 16
    Publication Date: 2023-12-09
    Description: Abstract
    Description: IGMAS+ is a software combining 3-D forward and inverse modeling, interactive visualization and interdisciplinary interpretation of potential fields and their applications under geophysical and geological data constrains. The software has a long history starting 1988 and has seen continuous improvement since then with input by many contributors. Since 2019, IGMAS+ is maintained and developed at The Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences by the staff of Section 4.5 – Basin Modelling and Section 5.2 – eScience Centre with strong ongoing support by H.-J. Götze and S. Schmidt from CAU Kiel. The official webpage of IGMAS+ is available at https://www.gfz-potsdam.de/igmas. Each major version of IGMAS+ is assigned with a DOI. Intermediate releases including changelog can be found at https://git.gfz-potsdam.de/igmas/igmas-releases/-/releases/.
    Description: Methods
    Description: In IGMAS+, the analytical solution of the volume integral for the gravity and magnetic effects of a homogeneous body relies on reducing the three-folded integral to an integral over the bounding polyhedrons (in IGMAS+, polyhedrons are constructed using triangles). The algorithm encompass all elements of the gravity and magnetic tensors. Optimized storage facilitates extremely fast inversion of material parameters and changes to the model geometry. This flexibility simplifies handling geometry changes, as the model geometry is promptly updated, and the field components are recalculated after each modification. The additional ability to invert for the geometry of the individual body interface extends the inverse modelling capabilities. Thanks to its triangular model structure, IGMAS+ effectively manages complex structures, such as the overhangs of salt domes. The software accommodates remanent and induced magnetization of geological bodies and finds application in interpreting borehole gravity and magnetics. The modeling process is guided by constrains from independent data sources, such as structural information, geological maps and seismic data, and is crucial for the genuine integration of 3D thermal modeling and/or full waveform inversion results. IGMAS+ is largely used in the creation of 3-D data-constrained subsurface structural density and susceptibility models at different spatial scales. Both large-scale models (thousands of square km) and regional (hundreds of square km), are important for understanding the drivers of geohazards. In this case IGMAS+ is versatile, capable of handling both flat (regional) and spherical models (global, when it is necessary to consider the curvature of the Earth) in 3D. Medium-scale models support studies on the usage of the subsurface as thermal, electrical or material storage in the context of energy transition. Small-scale (tens of square km) models are largely used in applied geophysics, typically in sub-salt and sub-basalt settings.
    Description: TechnicalInfo
    Description: List of changes for Release 1.4.8840 Added • Import of lines (#124, #188) • Interface inversion functionality (#135) • Bounding box for interface inversion (#142) • Export of quality and standard deviation values per iteration after interface inversion (#146, #171) • Nearest neighbour interpolation for empty voxels while importing voxel cubes (#158) • Special panel for empty voxel cells after importing a voxel cube (#162) Changed • Colours and line styles for fields in the 2D view (#126) • Triangulation check message corrected to Topology check (#156) • Misleading wording in the voxelization panel: "cubes" changed to "cells" (#165) • Redesign of the sectioning wizard (#44, #173, #217, #236, #242) • Title of new model wizard (#174) • Default header for imported CSV files (#219) Fixed • Incorrect 3D rendering of intersecting bitmaps with enabled transparency/alpha channel (#128, #192) • Graphical issue after deletion of the stations (#136) • Issues during interface inversion (#137, #143, #147, #151, #159, #170, #179) • Problem with voxel import while using grouping option (#141) • Exception in MarchingCubesPlugin (#144) • Problem with density geoid inversion (#145) • Problem with missing anomaly field after loading the project (#148) • Visualization of crossing triangles in the 2D view (#149) • Errors in voxelization resulting in voxels with zero density (#153) • Problem with creating a project using horizon import (#154) • Wrong effective density value in the information tab (#161, #246) • Problem with SVG export from the Multiple Cutter View (#166) • Coordinate issues while creating new project using import of horizons (#168, #169) • Wrong voxel visualization in 2D View when using non•square voxel cells (#175) • Bug with re-installation of older version on top of the newer (#176) • Incorrect calculation of the border effect in case when the density of the model units is not given in t/m3 (#178) • Wrong name for the standard deviation in linear parameter inversion, voxel effect (#189) • Error in distance unit conversion while loading voxel cubes (#190) • Incorrect vertical placement of loaded bitmaps in the Multiple Cutter View (#208) • Not updating body volume values after automatic correction of polygon orientation (#216) • Problem while loading horizons with identical points as CSV files (#218) • Incorrect parsing of headers of certain TSURF GOCAD files (#220, #221) • New body added to a model is not assigned the existing properties (#224) • Installer is not creating shortcuts on Linux (#222) • Wrong calculation of voxel effect when combined with triangulation (#227) • Bug while rendering images in the WorldWind plugin (#230) • Effective density in information tab is shown even outside of the voxel cube (#231) • Wrong application of default voxel function to the bodies deactivated during the voxel import (#232) • Voxel cube is not visible in the 2D View (#233) • Wrong assignment of the voxel cells to bodies after geometry changes (#239) • Image files with names containing space are not reloaded with project (#240) • Problem with visualization and calculation after loading voxel cubes of susceptibility type (#243) • Problem with loading projects created with earlier versions (#244) • Wrong effective density in information tab while voxel factor is not equal to 1 (#246) List of changes for Release 1.4.8707 Added • An option to change the font size of the axes and colour bars in 2D Map View (#45) • Reversed colour maps from the scientific colour map set (#45) • An option to set up manually the limits and the step of isolines or contours (#45) • An option to set up the colour bar position (#45) • A possibility to load local KML/KMZ files in the WorldWind plugin (#123) • An option in the object tree to show/hide fields in different views (#130) • An option to remove the components and fields (#131) • Added a WMS service (in the WorldWind plugin) by GFZ Potsdam based on maps.gfz-potsdam.de (#133) Changed • Flatlaf updated to 1.1.2 Fixed • All visibility settings of calculated and measured fields are synchronised for comparability (#45) • By default the colour bar for each field in 2D Maps View is placed horizontally below each panel (#45) • Rounding of the contour (isoline) labels (#132) • Adjustment of colour bar position in 2D Maps View (#125) • Sorting and storing of the list of model parameters in body manager (#122) List of changes for Release 1.4.8690 Added • 58 new themes from JFormDesginer (#113) • Possibility to select colormaps for fields and residuals from scientific colormap set (#45) • Possibility to change contours for fields and residuals Changed • Old icon in wizards was replaced with new IGMAS icon (#108) • Colormaps of the fields and residuals (#45) • Mirrored residual colorbar limits to ensure white zero values (#45) • Field rendering options are saved for each project (#45) Fixed • Wrong symbols in the license text due to encoding (#106) • Problem with license wizard after installation (#112) • Starting from icon in macOS (#107) • Issue with mouse pointer (#118) related to working sections (#35) List of changes for Release 1.4.8671 Added • A possibility to choose units other than t/m3 during voxel import (#21) • An option to perform update check (#96) Changed • GFZ logo in the starting view • License attributes (#93, #98) Fixed • Bug with wrong calculation of anomaly if the voxel density unit is not t/m^3 (#74) • Calculation of the body volumes (#32) • Exception after closing a project (#95) • Padding in the installer (#14) • Update check wrongly notified that there is a newer version (#94) • Installer link in popup update notification (#92)
    Keywords: gravity ; potential field ; magnetics ; modelling ; software ; EARTH SCIENCE ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 MAGNETIC FIELD ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; science 〉 natural science 〉 earth science 〉 geophysics
    Type: Software , Software
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  • 17
    Publication Date: 2023-12-09
    Description: Abstract
    Description: IGMAS+ is a software combining 3-D forward and inverse modeling, interactive visualization and interdisciplinary interpretation of potential fields and their applications under geophysical and geological data constrains. The software has a long history starting 1988 and has seen continuous improvement since then with input by many contributors. Since 2019, IGMAS+ is maintained and developed at The Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences by the staff of Section 4.5 – Basin Modelling and Section 5.2 – eScience Centre with strong ongoing support by H.-J. Götze and S. Schmidt from CAU Kiel. The official webpage of IGMAS+ is available at https://www.gfz-potsdam.de/igmas. Each major version of IGMAS+ is assigned with a DOI. Intermediate releases including changelog can be found at https://git.gfz-potsdam.de/igmas/igmas-releases/-/releases/. This is a collection DOI referring to all versions of IGMAS+. Links to each published version are redundantly available via the "Files" section and the Related Work section ("includes").
    Description: Methods
    Description: In IGMAS+, the analytical solution of the volume integral for the gravity and magnetic effects of a homogeneous body relies on reducing the three-folded integral to an integral over the bounding polyhedrons (in IGMAS+, polyhedrons are constructed using triangles). The algorithm encompass all elements of the gravity and magnetic tensors. Optimized storage facilitates extremely fast inversion of material parameters and changes to the model geometry. This flexibility simplifies handling geometry changes, as the model geometry is promptly updated, and the field components are recalculated after each modification. The additional ability to invert for the geometry of the individual body interface extends the inverse modelling capabilities. Thanks to its triangular model structure, IGMAS+ effectively manages complex structures, such as the overhangs of salt domes. The software accommodates remanent and induced magnetization of geological bodies and finds application in interpreting borehole gravity and magnetics. The modeling process is guided by constrains from independent data sources, such as structural information, geological maps and seismic data, and is crucial for the genuine integration of 3D thermal modeling and/or full waveform inversion results. IGMAS+ is largely used in the creation of 3-D data-constrained subsurface structural density and susceptibility models at different spatial scales. Both large-scale models (thousands of square km) and regional (hundreds of square km), are important for understanding the drivers of geohazards. In this case IGMAS+ is versatile, capable of handling both flat (regional) and spherical models (global, when it is necessary to consider the curvature of the Earth) in 3D. Medium-scale models support studies on the usage of the subsurface as thermal, electrical or material storage in the context of energy transition. Small-scale (tens of square km) models are largely used in applied geophysics, typically in sub-salt and sub-basalt settings.
    Keywords: gravity ; potential field ; magnetics ; modelling ; software ; EARTH SCIENCE ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 MAGNETIC FIELD ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; science 〉 natural science 〉 earth science 〉 geophysics
    Type: Collection , Collection
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  • 18
    Publication Date: 2023-12-09
    Description: Abstract
    Description: IGMAS+ is a software for 3-D modelling of potential fields and its derivatives under the condition of constraining data and independent information. It comes with tools for forward and inverse modelling. IGMAS+ has a long history starting 1988 and has seen continuous improvement since then with input by many contributors. Since 2019, IGMAS+ is maintained and developed at The Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences by the staff of Section 4.5 – Basin Modelling and ID2 – eScience Centre with strong ongoing support by H.-J. Götze and S. Schmidt from CAU Kiel. The official webpage of IGMAS+ is available at https://www.gfz-potsdam.de/igmas/. Each major version of IGMAS+ will be assigned with a new DOI. Intermediate releases including changelog can be found at https://git.gfz-potsdam.de/igmas/igmas-releases/-/releases/.
    Description: Methods
    Description: In IGMAS+ the analytical solution of the volume integral for the gravity and magnetic effect of a homogeneous body is based on the reduction of the three-folded integral to an integral over the bounding polyhedrons (in IGMAS polyhedrons are built by triangles). The original algorithm has been extended to cover all elements of the gravity and magnetic tensors as well. Optimized storage enables extreme fast inversion of material parameters and changes to the model geometry and this flexibility makes geometry changes easy. Immediately after each change, model geometry is updated and the field components are recalculated. Because of the triangular model structure, IGMAS+ can handle complex structures (multi Z surfaces) like the overhangs of salt domes very well. It handles remanent and induced magnetisation of geological bodies and was applied to the interpretation of borehole gravity and magnetics. Modelling is constrained by structural input from independent data sources, such as seismic data, and is essential toward true integration of 3D thermal modelling or even Full Waveform Inversion. Geophysical investigations may cover huge areas of several thousand square kilometres but also models of Applied Geophysics at a meter scale. Due to the curvature of the Earth, the use of spherical geometries and calculations is necessary. IGMAS+ can be used for both flat (regional) and spherical models (global) in 3D.
    Description: TechnicalInfo
    Description: List of changes for Release 1.3.8656 Fixed •Custom projection using GeoTools (#22) •Voxel density units (#74) •Dark/light theme selector not working for the first start (#83) •The size of windows for text input (#76) •Consistent user experience for all ptaforms (#69) •Build problem (#65) •Bug with reading "calculated (measured) Geoid" from ".station" format (#38) •Build problem (#59) •Spherical calculation settings of "Max. Length" (#37) •An error occured when section was defined with normal (0, -1) (#35) •Bug when save project button is disabled while reaching recent items directory (#4) •EPSG codes not appearing in projection lists (#28) •Multiple cutter showed anomaly field in white (#36) •Residual field is in mGal/km when the gradients are calculated in Eötvös (#36) •Wrong factor for magnetic field calculation with mT (#29) •Bug related to memory settings (#31) •Image export •WorldWind renderer •Linux executables Added •GFZ branding in installer (#14) •Calculation of body volume (#32) •GeoTools gt-referencing projection (#78) •New flatlaf design themes •Integrate update check (#43) •Notification about missing coordinate system when starting spherical approximation (#16) •2-D View icon to the toolbar •Warning for the missing projection •This changelog Changed •Migrated to latest JOGL bindings (#84) •Name of the app after installation changed to IGMAS+ (#81) •About window (#53) •Switch from JSyntaxPane to RSyntaxTextArea (#71) •Migrated to new truelicense version v4 (#56) •Using "imported" instead of "measured" for Geoid for export/import (#41) •Disabled SSL certificate validation for WorldWind tile server •Viewboard logo - GFZ logo is used now (#14) •Switched to latest jython 2.7.2b2 •Switched to java8 as minimum requirement •Switched to the latest parsii library •Swtiched to the latest proj4j library •Updated main logo •Updated installer •Version numbers will now be generated following [major].[minor].[ci_pipeline_id]-[commit_hash]-[testing]. Removed •toolbox3d dependency (#57) •Geometry inversion from installer (#33) •Unsupported cluster installer
    Keywords: gravity ; potential field ; magnetics ; modelling ; software ; EARTH SCIENCE ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 MAGNETIC FIELD ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; science 〉 natural science 〉 earth science 〉 geophysics
    Type: Software , Software
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  • 19
    Publication Date: 2024-02-23
    Description: Abstract
    Description: The main aim of this project is to investigate the crustal and mantle structure beneath the Longmenshan fault zone in China, based on a very dense passive seismology profile. The Longmenshan fault zone hosted the Wenchuan earthquake of May 2008 with a magnitude (Mw) of 7.9 and the Lushan earthquake of June 2013 with a magnitude (Mw) of 6.6. It is planned to mainly use the receiver-function method, to investigate the crustal and mantle structure beneath the Longmenshan fault zone. Waveform data are available from the GEOFON data center, under network code 4O, and are embargoed until February 2024.
    Keywords: Broadband seismic waveforms ; Seismology ; temporary local seismic experiment ; Earthquake ; Receiver functions ; Crustal and mantle structure ; China ; Monitoring system ; EARTH SCIENCE 〉 SOLID EARTH ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~1T
    Format: .mseed
    Format: XML
    Location Call Number Expected Availability
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  • 20
    Publication Date: 2024-02-22
    Description: Abstract
    Description: This field campaign aimed at densifying the station coverage on the Armutlu Peninsula in the eastern Sea of Marmara. The Armutlu peninsula is directly crossed by the Armutlu fault, located roughly ~50 km away from the Istanbul metropolitan region. The main objective of this experiment is to characterize the seismic and aseismic deformation of this region. Waveform data are available from the GEOFON data centre, under network code 9P.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; temporary local seismic network ; Monitoring system ; EARTH SCIENCE 〉 SOLID EARTH ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~600G
    Format: .mseed
    Format: XML
    Location Call Number Expected Availability
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  • 21
    Publication Date: 2024-05-21
    Description: Abstract
    Description: Continuous passive seismic monitoring is carried out between September 2017 and December 2021 around the Theistareykir geothermal area located at the intersection between the active Northern Rift Zone and the active Tjörnes Fracture Zone in NE Iceland. This experiment, in addition to an extensive gravimetric monitoring survey, was conducted in the framework of the MicroGraviMoTiS project for a better understanding of the structures and behavior of the local geothermal system under exploitation and for further development of local and regional geothermal resources. 14 broadband stations (Trillium C-120s) recording at 200 Hz comprise the temporary network, that is installed to complement stations of the national seismological network of IMO and stations of Landsvirkjun, the National Power Company of Iceland. The stations were placed in and around the producing zone to primarily retrieve local natural and/or induced seismicity associated to the injection and production operations. The retrieved seismic data is also used for obtaining a representative 1D velocity model of the region, for computing a seismic ambient noise tomography, and for monitoring the system using coda wave interferometry techniques. Funding for this project is provided by the German Federal Ministry for Education and Research (MicroGraviMoTiS , BMBF, grant: 03G0858A), the Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences and Landsvirkjun. Waveform data are available from the GEOFON data center, under network code 3P, and are embargoed until December 2025.
    Keywords: Broadband seismic waveforms ; Seismology ; temporary local seismic experiment ; Monitoring system ; EARTH SCIENCE 〉 SOLID EARTH ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS ; Passive seismic ; Seismometers ; Velocity ; MiniSEED ; GIPP ; MESI ; Volcano
    Type: Dataset , Seismic Network
    Format: 783GB
    Format: .mseed
    Format: XML
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  • 22
    Publication Date: 2024-06-18
    Description: Abstract
    Description: The dataset contains the seismic weight drop data acquired in Private Reserve Santa Gracia, Chile. The data acquisition was conducted as a part of the EarthShape project in the subproject of Geophysical Imaging of the Deep EarthShape (GIDES). The seismic line was setup to cut across an existing borehole location with core and geophysical logging data available (Krone et al., 2021; Weckmann et al., 2020). The data was acquired to image the deep weathering zone identified by the borehole data across the seismic profile. Included in the datasets are the raw data of the CUBE data logger, SEG-Y data of the recorded shots, and the shot and receiver geometry data. A vital aspect of comprehending the interplay between geological and biological processes lies in the imaging of the critical zone, located deep beneath the surface, where the transition from unaltered bedrock to fragmented regolith occurs. It had been hypothesized that the depth of such weathering zone is dependent on the climate condition of the area. A more humid climate with higher precipitation will result in a deeper weathering front. As a part of the EarthShape project (SPP-1803 ‘EarthShape: Earth Surface Shaping by Biota’), specifically the Geophysical Imaging of the Deep EarthShape (GIDES - Grant No. KR 2073/5-1), we aim to image the weathering zone using the geophysical approach. Using the seismic method, we can differentiate different weathered layers based on the seismic velocity while also providing a 2D subsurface image of the critical zone. We conducted a seismic weight drop experiment in the Private Reserve Santa Gracia, Chile, to observe the depth of the weathering zone in a semi-arid climate and compare the resulting model with existing borehole data (Krone et al., 2021; Weckmann et al., 2020). The acquired data can then be used for multiple seismic imaging techniques, including body wave tomography and multichannel analysis of surface waves.
    Description: Other
    Description: The DFG Priority Program 1803 "EarthShape - Earth Surface Shaping by Biota" (2016-2022; https://www.earthshape.net/) explored between scientific disciplines and includes geoscientists and biologists to study from different viewpoints the complex question how microorganisms, animals, and plants influence the shape and development of the Earth’s surface over time scales from the present-day to the young geologic past. All study sites are located in the north-to-south trending Coastal Cordillera mountains of Chile, South America. These sites span from the Atacama Desert in the north to the Araucaria forests approximately 1300 km to the south. The site selection contains a large ecological and climate gradient ranging from very dry to humid climate conditions.
    Keywords: Geophysics ; seismic ; weight drop ; weathering zone ; critical zone ; bedrock ; granite ; passive seismic ; 3C sensor ; EarthShape ; Chile ; Coastal Cordillera ; Private Reserve Santa Gracia ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WEIGHT-DROP_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 NEAR_SURFACE ; PASSIVE_SEISMIC 〉 STATIONS ; SENSOR 〉 GEOPHONE ; SENSOR 〉 3-C ; LAND ; SEG-Y_DATA_FORMAT ; MINISEED_DATA_FORMAT ; CONTROLLED_SOURCE_SEISMOLOGY 〉 RAW_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 VERTICALLY_STACKED_DATA ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE
    Type: Dataset , Dataset
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