Item talk:Q322754

{

 "id": "10.5066/p9k7qldl",
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     {
       "name": "Goldman, Mark R",
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       "name": "Nevitt, Johanna M",
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       "givenName": "Johanna M",
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       "name": "Chan, Joanne H",
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       "name": "Sickler, Robert R",
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       "name": "Criley, Coyn J",
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         "United States Geological Survey"
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     {
       "name": "Clarke, Timothy J",
       "nameType": "Personal",
       "givenName": "Timothy J",
       "familyName": "Clarke",
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     },
     {
       "name": "Brooks, Benjamin A",
       "nameType": "Personal",
       "givenName": "Benjamin A",
       "familyName": "Brooks",
       "affiliation": [
         "United States Geological Survey"
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     {
       "name": "Ericksen, Todd L",
       "nameType": "Personal",
       "givenName": "Todd L",
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         "United States Geological Survey"
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   ],
   "titles": [
     {
       "title": "High-resolution seismic imaging data acquired in 2021 across a trace of the San Andreas Fault at Mee Ranch, Monterey County, California"
     }
   ],
   "publisher": "U.S. Geological Survey",
   "container": {},
   "publicationYear": 2023,
   "subjects": [
     {
       "subject": "Seismology"
     }
   ],
   "contributors": [],
   "dates": [
     {
       "date": "2023",
       "dateType": "Issued"
     }
   ],
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   "types": {
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   "descriptions": [
     {
       "description": "In April of 2021, the U.S. Geological Survey conducted a high-resolution seismic survey at Mee Ranch in Monterey County, California. Both passive- and active-source seismic data were acquired using DTCC SmartSolo 3-component nodal seismograph systems (\"nodes\"), which continuously recorded data at rates up to 2000 samples per second. For passive-source acquisition, a 6x5 grid of nodes was deployed for several weeks before and during the active source shooting. For active-source acquisition, 395 nodes were deployed 1 meter apart (2 meters apart near the endpoints) along a southwest-northeast trend to create an approximately 500-m-long linear array. Additional nodes were deployed at 1 or 2 meter spacing along 25- and 50-m-long linear arrays centered about a known section of the fault. P-wave data were generated near each recording station of the main linear array using a Betsy seisgun firing an 8-gauge blank shotgun shell. P-wave data were also generated every 20 stations along the main linear array using approximately one/third pound of buried explosives. Fault-zone-guided-wave data were generated using explosive sources that were placed within a mapped trace of the San Andreas Fault zone and close to the shorter linear arrays. Finally, S-wave data were generated at each station using an aluminum block struck by a sledgehammer. Shot gathers were created in SEG-Y format (Barry et al, 1975) by extracting several seconds of data from each node for each recorded shot time. The passive grid data were converted to gain-corrected miniseed day files (Ahern and Dost, 2012). This report provides the metadata needed to analyze the seismic data. References: Ahern, T. and Dost, B., 2012, Standard for the Exchange of Earthquake Data (SEED) Manual: International Federation of Digital Seismograph Networks Incorporated Research Institutions for Seismolog, version, 2.4. Barry, K.M., Cavers, D.A., and Kneale, C.W., 1975, Recommended standards for digital tape formats: Geophysics, vol. 40, no.2, p.344-352.",
       "descriptionType": "Abstract"
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   "url": "https://www.sciencebase.gov/catalog/item/6323af07d34e71c6d67accf8",
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   "created": "2023-09-26T21:57:06Z",
   "registered": "2023-09-26T21:57:07Z",
   "published": null,
   "updated": "2023-09-26T21:58:55Z"
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