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3 results for “Earthquake source parameter”
Source parameter of hydraulic-fracturing-induced earthquakes in the Kiskatinaw area, northeast British Columbia
<p>Source parameter of 2475 hydraulic-fracturing-induced earthquakes (1927 events using P-wave estimates and 1882 events using S-wave estimates) in the Kiskatinaw area, northeast British Columbia between 1 July 2017 to 31 July 2020. The Study area covers parts of the Montney Formation, a major shale gas play within the Western Canada Sedimentary Basin. Source parameters include seismic moment, moment magnitude, spectral corner frequency, and static stress drop values using three different approaches (single spectrum fitting, a clustered event approach, and spectral-ratio method). Detailed information about the methods are stated in the corresponding publication:</p> <p>Roth, M. P., K. B. Kemna, R. M. Harrington, and Y. Liu (2022). Source properties of hydraulic-fracturing-induced earthquakes in the Kiskatinaw area, British Columbia, Canada. Journal of Geophysical Research: Solid Earth. <a href="https://doi.org/10.1029/2021JB022750">https://doi.org/10.1029/2021JB022750</a></p>
Tsunami Initial Profile and Maximum Runup through Earthquake Source Parameters
<p>The fitting database for 7840 earthquake (tsunami) source scenarios and corresponding N-wave parameters.</p>
Source Parameters and Ground Motion Simulation of the 2023 MW 5.5 Pingyuan Earthquake in the North China Plain
<p>Broadband seismic waveform data used for determining the focal mechanism and depth of the 2023 <em>M</em><sub>W</sub> 5.5 Pingyuan earthquake</p>
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International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.