Item talk:Q318141
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{
"DOI": { "doi": "10.5066/p13jcj2i", "identifiers": [], "creators": [ { "name": "David R Shelly", "nameType": "Personal", "affiliation": [ "United States Geological Survey" ], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0003-2783-5158", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Yongsoo Park", "nameType": "Personal", "affiliation": [ "Los Alamos National Lab" ], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": null, "nameIdentifierScheme": "ORCID" } ] } ], "titles": [ { "title": "Correlation-derived seismic phase arrival times from matched-filter studies of Yellowstone (Wyoming) 2017, Kilauea volcano (Hawaii) 2018, and Ridgecrest (California) 2019: A dataset for developing phase-picking neural networks" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2024, "subjects": [ { "subject": "seismic" }, { "subject": "earthquake" }, { "subject": "earthquake hazards" }, { "subject": "machine learning" }, { "subject": "Geophysics" }, { "subject": "FOS: Earth and related environmental sciences", "schemeUri": "http://www.oecd.org/science/inno/38235147.pdf", "subjectScheme": "Fields of Science and Technology (FOS)" }, { "subject": "Volcanology" }, { "subject": "Seismology" }, { "subject": "USGS" }, { "subject": "GHSC" }, { "subject": "plate tectonics" }, { "subject": "template matching" } ], "contributors": [], "dates": [], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [], "relatedItems": [], "sizes": [], "formats": [ "xml", "csv" ], "version": null, "rightsList": [ { "rights": "Creative Commons Zero v1.0 Universal", "rightsUri": "https://creativecommons.org/publicdomain/zero/1.0/legalcode", "schemeUri": "https://spdx.org/licenses/", "rightsIdentifier": "cc0-1.0", "rightsIdentifierScheme": "SPDX" } ], "descriptions": [ { "description": "This dataset contains correlation-derived seismic phase arrival times from three different studies:\n1. Maple Creek Earthquake Swarm, Yellowstone, Wyoming, June 11 to September 6, 2017:\nShelly, D. R., & J. L. Hardebeck (2019). Illuminating faulting complexity of the 2017 Yellowstone Maple Creek earthquake swarm. Geophysical Research Letters, 46, 2544\u2013 2552. https://doi.org/10.1029/2018GL081607\n\n2. Kilauea summit eruption earthquake sequence, Hawaii, April 29 to August 6, 2018:\nShelly, D. R., & W. A. Thelen (2019). Anatomy of a caldera collapse: K\u012blauea 2018 summit seismicity sequence in high resolution. Geophysical Research Letters, 46, 14395\u2013 14403. https://doi.org/10.1029/2019GL085636\nShelly, D.R., and W. A. Thelen, 2020, High resolution earthquake catalogs from the 2018 Kilauea eruption sequence: U.S. Geological Survey data release, https://doi.org/10.5066/P9DMIFMW\n\n3. Ridgecrest earthquake sequence, California, July 4-16, 2019:\nShelly, D. R. (2020) A High\u2010Resolution Seismic Catalog for the Initial 2019 Ridgecrest Earthquake Sequence: Foreshocks, Aftershocks, and Faulting Complexity. Seismological Research Letters, 91 (4): 1971\u20131978. doi: https://doi.org/10.1785/0220190309\nShelly, D.R., 2020, A High-Resolution Seismic Catalog for the Initial 2019 Ridgecrest Earthquake Sequence: U.S. Geological Survey data release, https://doi.org/10.5066/P9JN6H0N.\n\nOne comma separated value (CSV) file is uploaded for each sequence.\u00a0 Each\u00a0file contains the following fields:\n\u00a0\ntemplate_id:\u00a0 The assigned ID for the template\n\u00a0\nmatch_id: the assigned ID for the detected event\n\u00a0\nnetwork: The network code for the seismic station\n\u00a0\nstation: The name of the seismic station\n\u00a0\nphase: Seismic phase, P or S\n\u00a0\narrival: The arrival time, calculated based on the template phase pick time and the correlation-derived differential time, given in epoch time (seconds since January 1, 1970, UTC)\n\u00a0\nweight: The weighting assigned in the original study, (0.1 +3ccdiff)ccmax2 (see explanations of ccdiff and ccmax below)\n\u00a0\nmag: The magnitude determined for the detected event (see original study for details)\n\u00a0\nccmax: The peak cross-correlation coefficient (the largest absolute value correlation coefficient, including its sign)\n\u00a0\nccdiff: The difference between the absolute value of ccmax and the second largest absolute value correlation peak\n\u00a0\nchanloc: The seismic channel and location codes, separated by \u201c.\u201d\n\u00a0", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/667b1415d34e6151c9d6bcfd", "contentUrl": null, "metadataVersion": 1, "schemaVersion": "http://datacite.org/schema/kernel-4", "source": "api", "isActive": true, "state": "findable", "reason": null, "viewCount": 0, "downloadCount": 0, "referenceCount": 0, "citationCount": 0, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2024-08-06T15:52:32Z", "registered": "2024-08-06T15:52:33Z", "published": null, "updated": "2024-08-06T15:52:37Z" }
}