Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8495
DC Field | Value | Language |
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dc.contributor.authorall | Carbone, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Poland, M.; U.S. Geological Survey, Hawaiian Volcano Observatory, PO Box 51, Hawaii National Park, Hawaii 96718-0051, USA | en |
dc.date.accessioned | 2013-01-23T13:22:03Z | en |
dc.date.available | 2013-01-23T13:22:03Z | en |
dc.date.issued | 2012-06-29 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8495 | en |
dc.description.abstract | Convection in magma chambers is thought to play a key role in the activity of persistently active volcanoes, but has only been inferred indirectly from geochemical observations or simulated numerically. Continuous microgravity measurements, which track changes in subsurface mass distribution over time, provide a potential method for characterizing convection in magma reservoirs. We recorded gravity oscillations with a period of ~150 s at two continuous gravity stations at the summit of Kīlauea Volcano, Hawai‘i. The oscillations are not related to inertial accelerations caused by seismic activity, but instead indicate variations in subsurface mass. Source modeling suggests that the oscillations are caused by density inversions in a magma reservoir located ~1 km beneath the east margin of Halema‘uma‘u Crater in Kīlauea Caldera—a location of known magma storage. | en |
dc.language.iso | English | en |
dc.publisher.name | Geological Society of America | en |
dc.relation.ispartof | Geology (Geological Society of America) | en |
dc.relation.ispartofseries | 9/40 (2012) | en |
dc.subject | gravity oscillation | en |
dc.subject | shallow magma convection | en |
dc.title | Gravity fluctuations induced by magma convection at Kılauea, Hawai‘i | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 803-806 | en |
dc.identifier.URL | http://geology.gsapubs.org/content/early/2012/06/21/G33060.1.abstract?rss=1 | en |
dc.subject.INGV | 04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes | en |
dc.subject.INGV | 04. Solid Earth::04.02. Exploration geophysics::04.02.02. Gravity methods | en |
dc.identifier.doi | 10.1130/G33060.1 | en |
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Welch, P.D., 1967, The use of fast Fourier transform for the estimation of power spectra: A method based on time averaging over short, modifi ed periodograms: IEEE Transactions on Audio and Electroacoustics, v. 15, p. 70–73, doi:10.1109/TAU.1967.1161901. | en |
dc.description.obiettivoSpecifico | 3.6. Fisica del vulcanismo | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 0091-7613 | en |
dc.relation.eissn | 1943-2682 | en |
dc.contributor.author | Carbone, D. | en |
dc.contributor.author | Poland, M. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | U.S. Geological Survey, Hawaiian Volcano Observatory, PO Box 51, Hawaii National Park, Hawaii 96718-0051, USA | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Hawaiian Volcano Observatory, U.S. Geological Survey, Hawaii, USA | - |
crisitem.author.orcid | 0000-0003-2566-6290 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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