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Fault Information and Seismicity for the Portland Basin Deep Direct-Use Feasibility Study
Included in this dataset is a spreadsheet with the primary fault information used in the basin model, a spreadsheet with earthquake magnitude estimates, and a figure showing location of faults and microseismicity in the Portland Basin
Resources
3 resources available
-
EQ Magnitudes.xlsx
XLSX -
Fault Information.xlsx
XLSX -
Faulting and Microseismic Locations.pdf
PDF
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Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[ "019:20" ] |
| contactPoint |
{ "fn": "John Bershaw", "@type": "vcard:Contact", "hasEmail": "mailto:bershaw@pdx.edu" } |
| dataQuality |
true
|
| description | Included in this dataset is a spreadsheet with the primary fault information used in the basin model, a spreadsheet with earthquake magnitude estimates, and a figure showing location of faults and microseismicity in the Portland Basin |
| distribution |
[ { "@type": "dcat:Distribution", "title": "EQ Magnitudes.xlsx", "format": "xlsx", "accessURL": "https://gdr.openei.org/files/1106/EQ_Magnitudes_12042018%20%281%29.xlsx", "mediaType": "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet", "description": "Included in this table is all of the faults in the Portland and Tualatin Basins with lengths from the Quaternary Fold and Fault Database, and depths calculated from focal mechanisms, obtained from the Pacific Northwest Seismic Network. Regressions from Wells and Coppersmith (1994) are used to estimate the maximum magnitude earthquake (for strike-slip and reverse faults) that would be generated if a rupture were to occur along the entire length of the fault. Minimum fault depths calculated from focal mechanisms are used to calculate fault area and a regression from Hanks and Bakken (2002) for all fault types is used to calculate another magnitude estimate." }, { "@type": "dcat:Distribution", "title": "Fault Information.xlsx", "format": "xlsx", "accessURL": "https://gdr.openei.org/files/1106/Fault_Information_12042018%20%281%29.xlsx", "mediaType": "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet", "description": "Included in this table is all faults in the study area with information on dip, sense of motion, length, and depth with sources for this information. " }, { "@type": "dcat:Distribution", "title": "Faulting and Microseismic Locations.pdf", "format": "pdf", "accessURL": "https://gdr.openei.org/files/1106/PDX_eqs_faults_12042018%20%281%29.pdf", "mediaType": "application/pdf", "description": "This file is a figure of the Portland and Tualatin Basins with faults included in this study as well as microseismicity. " } ] |
| DOI | 10.15121/1495394 |
| identifier | https://data.openei.org/submissions/7255 |
| issued | 2018-12-04T07:00:00Z |
| keyword |
[ "Beaverton Fault", "Bolton Fault", "Canby-Molalla Fault", "DDU", "DDU-TES", "East Bank Fault", "Frontal Fault", "Gales Creek Fault", "Helvetia Fault", "Mount Angel Fault", "Newberg Fault", "OR", "Oatfield Fault", "Oregon", "Portland", "Sherwood Fault", "basin", "deep direct-use", "dip angle", "dip direction", "earthquake", "energy", "event", "fault", "fault length", "feasibility", "geothermal", "magnitude", "microseismicity", "model", "seismicity", "structural geology", "thermal energy storage" ] |
| landingPage | https://gdr.openei.org/submissions/1106 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2020-03-06T23:03:36Z |
| programCode |
[ "019:006" ] |
| projectLead | Arlene Anderson |
| projectNumber | EE0008104 |
| projectTitle | Portland Deep Direct-Use Thermal Energy Storage (DDU-TES) Feasibility Study |
| publisher |
{ "name": "Portland State University", "@type": "org:Organization" } |
| spatial |
"{"type":"Polygon","coordinates":[[[-123.1222703125,44.88720992512],[-121.90288906249998,44.88720992512],[-121.90288906249998,46.129796490417],[-123.1222703125,46.129796490417],[-123.1222703125,44.88720992512]]]}"
|
| title | Fault Information and Seismicity for the Portland Basin Deep Direct-Use Feasibility Study |
