A High-Resolution Seismic Catalog for the Initial 2019 Ridgecrest Earthquake Sequence
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| Field | Value |
|---|---|
| accessLevel | public |
| bureauCode | {010:12} |
| catalog_@context | https://project-open-data.cio.gov/v1.1/schema/catalog.jsonld |
| catalog_conformsTo | https://project-open-data.cio.gov/v1.1/schema |
| catalog_describedBy | https://project-open-data.cio.gov/v1.1/schema/catalog.json |
| identifier | USGS:5dd715f3e4b0695797650d18 |
| metadata_type | geospatial |
| modified | 20200818 |
| old-spatial | -180.0, -90.0, 180.0, 90.0 |
| publisher | U.S. Geological Survey |
| publisher_hierarchy | Department of the Interior > U.S. Geological Survey |
| resource-type | Dataset |
| source_datajson_identifier | true |
| source_hash | 1d5349d74aeccb262ce2624fa8e790aea124d25a |
| source_schema_version | 1.1 |
| spatial | {"type": "Polygon", "coordinates": [[[-180.0, -90.0], [-180.0, 90.0], [ 180.0, 90.0], [ 180.0, -90.0], [-180.0, -90.0]]]} |
| theme | {geospatial} |
| Groups |
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| Tags |
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| isopen | False |
| license_id | notspecified |
| license_title | License not specified |
| maintainer | U.S. Geological Survey - ScienceBase |
| maintainer_email | sciencebase@usgs.govplace |
| metadata_created | 2025-11-22T23:48:41.965971 |
| metadata_modified | 2025-11-22T23:48:41.965975 |
| notes | I use template matching and precise relative relocation techniques to develop a high-resolution earthquake catalog for the initial portion of the 2019 Ridgecrest earthquake sequence, from July 4-16, encompassing the foreshock sequence and the first 10+ days of aftershocks following the Mw 7.1 mainshock. Using 13,525 routinely cataloged events as waveform templates, I detect and precisely locate a total of 34,091 events. Precisely located earthquakes reveal numerous cross-cutting fault structures with dominantly perpendicular SW- and NW-strikes. Foreshocks of the Mw 6.4 event appear to align on a NW-striking fault. Aftershocks of the Mw 6.4 event suggest that it further ruptured this NW-striking fault, as well as the SW-striking fault where surface rupture was observed. Finally, aftershocks of the Mw 7.1 show a highly complex distribution, illuminating a primary NW-striking fault zone consistent with surface rupture, but also numerous cross-cutting SW-striking faults. Aftershock relocations suggest that the Mw 7.1 event ruptured adjacent to the previous NW-striking rupture of the Mw 6.4, perhaps activating a subparallel structure southwest of the earlier rupture. Both the NW and SE rupture termini of the Mw 7.1 rupture exhibited multiple-fault branching, with particularly high rates of aftershocks and multiple fault orientations in the dilatational quadrant NE of the NW rupture terminus. |
| num_resources | 2 |
| num_tags | 12 |
| title | A High-Resolution Seismic Catalog for the Initial 2019 Ridgecrest Earthquake Sequence |