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http://hdl.handle.net/10261/214226
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Campo DC | Valor | Lengua/Idioma |
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dc.contributor.author | Shirzaei, Manoochehr | es_ES |
dc.contributor.author | Ellsworth, William L. | es_ES |
dc.contributor.author | Tiampo, Kristy F. | es_ES |
dc.contributor.author | González, Pablo J. | es_ES |
dc.contributor.author | Manga, Michael | es_ES |
dc.date.accessioned | 2020-06-12T11:21:24Z | - |
dc.date.available | 2020-06-12T11:21:24Z | - |
dc.date.issued | 2016-09-23 | - |
dc.identifier.citation | Science 353(6306): 1416-1419 (2016) | es_ES |
dc.identifier.issn | 0036-8075 | - |
dc.identifier.uri | http://hdl.handle.net/10261/214226 | - |
dc.description.abstract | Observations that unequivocally link seismicity and wastewater injection are scarce. Here we show that wastewater injection in eastern Texas causes uplift, detectable in radar interferometric data up to >8 kilometers from the wells. Using measurements of uplift, reported injection data, and a poroelastic model, we computed the crustal strain and pore pressure. We infer that an increase of >1 megapascal in pore pressure in rocks with low compressibility triggers earthquakes, including the 4.8–moment magnitude event that occurred on 17 May 2012, the largest earthquake recorded in eastern Texas. Seismic activity increased even while injection rates declined, owing to diffusion of pore pressure from earlier periods with higher injection rates. Induced seismicity potential is suppressed where tight confining formations prevent pore pressure from propagating into crystalline basement rocks. | es_ES |
dc.description.sponsorship | RADARSAT-2 images were acquired under SOAR-E (Science and Operational Applications Research–Education) project 5226 of the Canadian Space Agency (www.asc-csa.gc.ca/eng/). ALOS data were obtained through Alaska Satellite Facilities (www.asf.alaska.edu/). M.S.’s contribution was supported by U.S. Geological Survey grant G13AP00040. K.F.T. was supported by a Discovery Grant from the Natural Sciences and Engineering Research Council of Canada. W.L.E. was supported by the Stanford Center for Induced and Triggered Seismicity. M.M. was supported by U.S. NSF grant EAR-1344424. P.J.G. was supported by the UK Natural Environment Research Council projects COMET and NE/K011006/1. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | American Association for the Advancement of Science | es_ES |
dc.relation.isversionof | Postprint | es_ES |
dc.rights | closedAccess | es_ES |
dc.subject | Surface uplift | es_ES |
dc.subject | Time-dependent seismic | es_ES |
dc.subject | Fluid injection | es_ES |
dc.subject | Texas | es_ES |
dc.title | Surface uplift and time-dependent seismic hazard due to fluid injection in eastern Texas | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1126/science.aag0262 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | https://doi.org/10.1126/science.aag0262 | es_ES |
dc.identifier.e-issn | 1095-9203 | - |
dc.rights.license | https://creativecommons.org/licenses/by/4.0/ | es_ES |
dc.contributor.funder | Canadian Space Agency | es_ES |
dc.contributor.funder | Natural Sciences and Engineering Research Council of Canada | es_ES |
dc.contributor.funder | Natural Environment Research Council (UK) | es_ES |
dc.relation.csic | No | es_ES |
oprm.item.hasRevision | no ko 0 false | * |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000270 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000038 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000016 | es_ES |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.grantfulltext | none | - |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | No Fulltext | - |
item.languageiso639-1 | en | - |
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