Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/11125
DC Field | Value | Language |
---|---|---|
dc.date.accessioned | 2018-03-12T10:06:13Z | en |
dc.date.available | 2018-03-12T10:06:13Z | en |
dc.date.issued | 2018-03-15 | en |
dc.identifier.uri | http://hdl.handle.net/2122/11125 | en |
dc.description.abstract | A fraction of the volcanic activity occurs intraplate, challenging our models of melting and magma transfer to the Earth's surface. A prominent example is Mt. Etna, eastern Sicily, offset from the asthenospheric tear below the Malta Escarpment proposed as its melt source. The nearby Hyblean volcanism, to the south, and the overall northward migration of the eastern Sicilian volcanism are also unexplained. Here we simulate crustal magma pathways beneath eastern Sicily, accounting for regional stresses and decompression due to the increase in the depth of the Malta Escarpment. We find non-vertical magma pathways, with the competition of tectonic and loading stresses controlling the trajectories' curvature and its change in time, causing the observed migration of volcanism. This suggests that the Hyblean and Etnean volcanism have been fed laterally from a melt pooling region below the Malta Escarpment. The case of eastern Sicily shows how the reconstruction of the evolution of magmatic provinces may require not only an assessment of the paleostresses, but also of the contribution of surface loads and their variations; at times, the latter may even prevail. Accounting for these competing stresses may help shed light on the distribution and wandering of intraplate volcanism | en |
dc.language.iso | English | en |
dc.relation.ispartof | Earth and Planetary Science Letters | en |
dc.relation.ispartofseries | /486 (2018) | en |
dc.subject | intraplate volcanism | en |
dc.subject | fault scarp | en |
dc.subject | dike propagation | en |
dc.subject | Malta Escarpment | en |
dc.subject | Hyblean volcanism | en |
dc.subject | Etna | en |
dc.title | Etnean and Hyblean volcanism shifted away from the Malta Escarpment by crustal stresses | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 15-22 | en |
dc.subject.INGV | Mechanical models of magma transfer are used to backtrack the surface volcanism in Eastern Sicily. | en |
dc.subject.INGV | Our models account for regional stresses and decompression due to the deepening of the Malta Escarpment | en |
dc.subject.INGV | Both the Hyblean and Etnean volcanism has been laterally fed by a melt pooling region below the Malta Escarpment | en |
dc.subject.INGV | The Malta Escarpment played an active role in steering the shifting of Etnean and Hyblean volcanism | en |
dc.identifier.doi | 10.1016/j.epsl.2018.01.006 | en |
dc.description.obiettivoSpecifico | 1V. Storia eruttiva | en |
dc.description.obiettivoSpecifico | 2V. Struttura e sistema di alimentazione dei vulcani | en |
dc.description.journalType | JCR Journal | en |
dc.contributor.author | Neri, Marco | en |
dc.contributor.author | Rivalta, Eleonora | en |
dc.contributor.author | Maccaferri, Francesco | en |
dc.contributor.author | Acocella, Valerio | en |
dc.contributor.author | Cirrincione, Rosolino | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | GFZ German Research Center for Geosciences, Potsdam, Germany | en |
dc.contributor.department | GFZ German Research Center for Geosciences, Potsdam, Germany | en |
dc.contributor.department | Dipartimento Scienze Roma Tre, Roma, Italy | en |
dc.contributor.department | Dipartimento di Scienze Biologiche, Geologiche e Ambientali – Università di Catania C.so Italia 57, 95129 Catania, Italy | 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 | GFZ German Research Center for Geosciences, Potsdam, Germany | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Università Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy | - |
crisitem.author.dept | Dipartimento di Scienze Biologiche, Geologiche e Ambientali – Università di Catania C.so Italia 57, 95129 Catania, Italy | - |
crisitem.author.orcid | 0000-0002-5890-3398 | - |
crisitem.author.orcid | 0000-0001-8245-0504 | - |
crisitem.author.orcid | 0000-0002-2023-837X | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | Existing users please Login |
---|---|---|---|---|
2018 Neri et al Malta Escarp EPSL 2018.pdf | Article | 3.93 MB | Adobe PDF | |
Neri et al EPSL 2018.pdf | Open Access | 1.59 MB | Adobe PDF | View/Open |
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