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37 results for “induced seismicity”
Fig. 2 in A seismically induced onshore surge deposit at the KPg boundary. North Dakota
Fig. 2. Tanis site stratigraphy and fossil distribution. Stratigraphic section of Tanis, outlining the lithological subdivisions and grain-size profile for the Event Deposit, abundance and primary stratigraphic distribution for a selection of continental and marine fossils, abundance of marine palynomorphs (palyno %), select impact-derived materials, and flow direction.
Fig. 3 in A seismically induced onshore surge deposit at the KPg boundary. North Dakota
Fig. 3. Chicxulub tonstein capping the Event Deposit at Tanis and representative impact-derived materials. (A) Iridium-enriched tonstein in situ atop the Event Deposit. (B) Shocked mineral with multiple intersecting planar deformation features (FAU.DGS.ND.161.977.T). (c) Clay-altered ejecta spherules (FAU.DGS.ND.161.33.T), some with prominent schlieren. (D) Micro-CT of a clay-altered ejecta spherule with unaltered glass core (FAU.DGS.ND.161.11.T). (E) Shards of unaltered impact glass (FAU.DGS.ND.161.45.T).
Seismic dataset in "Source-Independent Passive Seismic Reverse-time Structure Imaging with Grouping Imaging Condition: Method and Application to Microseismic Events Induced by Hydraulic Fracturing"
<p>This dataset contains the seismic data and the velocity model used in the manuscript entitled "Source-Independent Passive Seismic Reverse-time Structure Imaging with Grouping Imaging Condition: Method and Application to Microseismic Events Induced by Hydraulic Fracturing" submitted to Journal of Geophysical Research-Solid Earth.</p>
Contrasting Crustal Signatures across the 2021 MS6.0 Luxian (China) Induced Earthquake Revealed by Dense Seismic and Magnetotelluric Data
<p>This is the main dataset supporting the 2021 Luxian (China) MS6.0 Earthquake paper</p> <p>MT folder contains MT data used in the inversion of the MT resistivity model and the final 3-D electrical resistivity model file (i.e., MT_resistivity.model)</p> <p>Seismic folder contains the continuous seismic waveforms (i.e., Continuous_seismic_waveforms.zip), the cross-correlation functions (i.e., Cross-correlation_Functions.zip), the final 3-D velocity model file (i.e., 3-D_VS_model.dat) and the our relocated earthquake catalogue (i.e., Relocated_earthquake_catalogue.dat)</p>
Pre-existing Structures and Stress Variations Jointly Control the Induced Seismicity in Enhanced Geothermal System of Gonghe Basin, China
<p>This is the dataset available for the article titled "Pre-existing Structures and Stress Variations Jointly Control the Induced Seismicity in Enhanced Geothermal System of Gonghe Basin, China", including phase information, earthquake catalog, waveforms of earthquakes and resolved focal mechanisms, 1D velocity model.</p>
Induced seismicity within the Groningen gas field
<p>The data set used in the Bourne & Oates article: 'Extreme threshold failures within a heterogeneous elastic thin-sheet and the spatial-temporal development of induced seismicity within the Groningen gas field'.</p>
Forecasting ocean wave-induced seismic noise; supporting dataset
<p>Dataset supporting the manuscript "Forecasting ocean wave-induced seismic noise".</p>
Data files for 'Tan et al., (2020). Hydraulic fracturing induced seismicity in the southern Sichuan Basin due to fluid diffusion inferred from seismic and injection data analysis'
<p>CEDC catalog.xlsx : the seismic catalog from China Earthquake Data Center (https://data.earthquake.cn/)</p> <p>Local network catalog.xlsx : the seismic catalog of the local seismic network</p> <p>Injection data of N5&N7.xlsx : the injection data of N5 and N7 (with permission of the operator)</p>
Output datasets from model for the paper "On the potential role of viscoelasticity in fluid-induced seismicity"
<p>Output datasets from model for "On the potential role of viscoelasticity in fluid-induced seismicity" </p>
Data from: Frictional stability of metamorphic epidote in granitoid faults under hydrothermal conditions and implications for injection-induced seismicity
<p>The effect of low-grade metamorphic epidote on fault stability in granitoids at shallow depth is not well understood. We present structured laboratory observations of epidote and simulated Pohang granodiorite (an EGS site) gouges and mixtures to evaluate their frictional responses. The experiments were performed on powdered rock gouges at a constant confining pressure of 110 <i>MPa</i>, pore fluid pressures of 42 and 63 <i>MPa</i>, temperatures of 100-250℃ and epidote percentages in the range of 0-100 <i>vol</i>.%. Results show that the simulated Pohang granodiorite gouge is frictionally strong (friction coefficient of ~0.71) but exhibits a transition from velocity-strengthening to velocity-weakening behavior at <i>in-situ</i> temperatures >150℃. Epidote gouge displays similar frictional strength to the simulated granodiorite gouge but a stronger velocity-weakening response at 150℃. Increasing the epidote content in the homogeneously mixed gouges maintains the high frictional strength but increases velocity-weakening response approximately proportionately with epidote content. Modes of epidote precipitation likely control patch dimension and this in turn potentially changes the response of the 50:50 epidote-granodiorite mixed gouges in different geometric configurations. However, 50:50 mixtures that are variously homogeneously mixed, encapsulated and checkerboarded in their architectures are insensitive to their various geometries – all reflect the high frictional strength and strong velocity-weakening response of 100:0 pure epidote. This suggests that small volume percentages of epidote present as thin coatings on fractures and faults can impart velocity-weakening behavior, independent of individual patch size and can thereby support the potential seismic reactivation of faults. Considering the frictional and stability properties of epidote at conditions typical of shallow depths, the presence of low-grade metamorphism exerts a potentially important control on fault stability in granitoids with relevance as a marker mineral for susceptibility to injection-induced seismicity.</p>
Data from: Frictional stability of metamorphic epidote in granitoid faults under hydrothermal conditions and implications for injection-induced seismicity
Open the record for dataset details and reuse information.
Seismic data for 'Hu et al., The productivity of induced seismicity is controlled by injection fluid volume and preexisting faults in the southern Sichuan basin'
<p>Datasets presented in Hu's manuscript entitled 'The productivity of induced seismicity is controlled by injection fluid volume and preexisting faults in the southern Sichuan basin'</p>
High-speed-train-induced seismic signals recorded in Wuhan, 2020
<p>High-speed-train-induced seismic signals recorded in Wuhan, 2020</p>
Fig. 6 in A seismically induced onshore surge deposit at the KPg boundary. North Dakota
Fig. 6. Acipenseriform fish with ejecta clustered in the gill region. (A) X-ray of a fossil sturgeon head (outlined, pointing left; FAU.DGS.ND.161.115.T). (B) Magnified image of the X-ray in A showing numerous ejecta spherules clustered within the gill region (arrows). (c and D) Micro-CT images of another fish specimen (paddlefish; FAU.DGS.ND.161.29.T), with microtektites embedded between the gill rakers in the same fashion.
Fig. 5 in A seismically induced onshore surge deposit at the KPg boundary. North Dakota
Fig. 5. Chicxulub impact glass from Tanis, and geochemical comparison. (A) Magnified view of spherules within amber (FAU.DGS.ND.161.77.T). (B) Exposed unaltered spherule, in situ within amber (FAU.DGS.ND.161.735.T). (c) Thin section of unaltered glassy spherule recovered from amber (FAU.DGS.ND.161.997.T). (D) CI-normalized geochemistry highlighting the strong match between the ranges for Chicxulub black glass and the Tanis specimens.
Subducted Water-Induced Diamond Genesis and Seismic Anomalies in Earth's Deep Lower Mantle
<p>There the <span>thermodynamic properties</span> of dimond, FeH, FeO, pyrite-type FeOOH, phase H, Fe3C, MgSiO3, and elasticity of diamond,fcc FeH, FeOOH at mantle conditions.</p>
Dataset for "Depletion-induced seismicity at the Groningen gas field: Coulomb rate-and-state models including differential compaction effect"
<p>Data package used for the article of Candela et al. : “Depletion-induced seismicity at the Groningen gas field: Coulomb rate-and-state models including differential compaction effect”.</p>
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