Item talk:Q301659
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "A retrospective look at the February 1993 east rift zone intrusion at K\u012blauea volcano, Hawaii", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70211480", "url": "https://pubs.usgs.gov/publication/70211480" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70211480 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.jvolgeores.2018.05.017", "url": "https://doi.org/10.1016/j.jvolgeores.2018.05.017" } ], "journal": { "@type": "Periodical", "name": "Journal of Volcanology and Geothermal Research", "volumeNumber": "358", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Journal of Volcanology and Geothermal Research" } ], "datePublished": "2018", "dateModified": "2020-07-28", "abstract": "The February 1993 dike intrusion in the East\u00a0Rift Zone\u00a0(ERZ) of K\u012blauea\u00a0Volcano, Hawai'i, was recognized from tilt and\u00a0seismic data, but ground-based\u00a0geodetic data\u00a0were too sparse to constrain the characteristics of the intrusion. Analysis of Interferometric Synthetic Aperture Radar (InSAR) from the Japan Aerospace Exploration Agency (JAXA)\u00a0JERS-1\u00a0satellite reveals a maximum of ~30\u202fcm of line-of-sight (LOS) displacement occurring near Makaopuhi\u00a0Crater\u00a0in the middle ERZ of K\u012blauea. We model this deformation signal as a subvertical dike using a 3D-Mixed\u00a0Boundary Element Method\u00a0(3D-MBEM) paired with a nonlinear inversion algorithm to find the best-fit model. The best-fit dike is located just to the west of Makaopuhi Crater striking N50\u00b0W, extends to within 100\u202fm of the surface, is ~1.3\u202fkm in length by ~4.2\u202fkm in width along strike, and has a total volume of ~7.4\u202f\u00d7\u202f106\u202fm3. In addition, a post-intrusion\u00a0interferogram\u00a0from JERS-1 spanning 1993\u20131997 was analyzed. Guided by previous results, our model for the 4-year period consists of opening of the deep rift zones by about 0.5\u202fm at 3\u20138.5\u202fkm depth beneath the Southwest Rift Zone (SWRZ), ERZ and the summit. A sub-horizontal\u00a0detachment fault\u00a0is connected to the seaward side of the vertical dike-like source to mimic the\u00a0d\u00e9collement\u00a0known to exist beneath the volcano. We classify the 1993 dike intrusion as a passive intrusion similar to those that occurred in 1997 and 1999. Passive intrusions lack precursory inflation at K\u012blauea's summit, and the likely triggering mechanism is persistent deep rift opening combined with seaward motion of the south flank along the basal d\u00e9collement. Passive intrusions make forecasting and hazard assessment difficult since they are not preceded by inflation nor by large increases in\u00a0seismicity.", "description": "114 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Conway, Sarah", "givenName": "Sarah", "familyName": "Conway", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-1953-5550", "url": "https://orcid.org/0000-0003-1953-5550" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] }, { "@type": "Person", "name": "Wauthier, Christelle", "givenName": "Christelle", "familyName": "Wauthier" }, { "@type": "Person", "name": "Fukushima, Yo", "givenName": "Yo", "familyName": "Fukushima" }, { "@type": "Person", "name": "Poland, Michael P. mpoland@usgs.gov", "givenName": "Michael P.", "familyName": "Poland", "email": "mpoland@usgs.gov", 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