Publikationsdatum:
2017-04-04
Beschreibung:
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of
Mt. Etna. We take thirty soundings along two profiles oriented in the N-S and NW-SE
directions, and from these data recover two 2D resistivity models of the subsurface.
Both models reveal three major layers in a resistive-conductive-resistive sequence, the
deepest extending to 14 km bsl. The shallow layer corresponds to the volcanic cover, and
the intermediate conductive layer corresponds to underlying sediments segmented by
faults. These two electrical units are cut by E-W-striking faults. The third layer
(basement) is interpreted as mainly pertinent to the Apennine-Maghrebian Chain associated
with SW-NE-striking regional faults. The detailed shapes of the resistivity profiles
clearly show that the NE Rift is shallow-rooted ( 0–1 km bsl), thus presumably fed by
lateral dikes from the central volcano conduit. The NW-SE profile suggests by a series of
listric faults reaching up to 3 km bsl, then becoming almost horizontal. Toward the SE, the
resistive basement dramatically dips (from 3 km to 10 km bsl), in correspondence with
the Timpe Fault System. Several high-conductivity zones close to the main faults suggest
the presence of hydrothermal activity and fluid circulation that could enhance flank
instability. Our results provide new findings about the geometry of the unstable Etna flank
and its relation to faults and subsurface structures.
Beschreibung:
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of
Mt. Etna. We take thirty soundings along two profiles oriented in the N-S and NW-SE
directions, and from these data recover two 2D resistivity models of the subsurface.
Both models reveal three major layers in a resistive-conductive-resistive sequence, the
deepest extending to 14 km bsl. The shallow layer corresponds to the volcanic cover, and
the intermediate conductive layer corresponds to underlying sediments segmented by
faults. These two electrical units are cut by E-W-striking faults. The third layer
(basement) is interpreted as mainly pertinent to the Apennine-Maghrebian Chain associated
with SW-NE-striking regional faults. The detailed shapes of the resistivity profiles
clearly show that the NE Rift is shallow-rooted ( 0–1 km bsl), thus presumably fed by
lateral dikes from the central volcano conduit. The NW-SE profile suggests by a series of
listric faults reaching up to 3 km bsl, then becoming almost horizontal. Toward the SE, the
resistive basement dramatically dips (from 3 km to 10 km bsl), in correspondence with
the Timpe Fault System. Several high-conductivity zones close to the main faults suggest
the presence of hydrothermal activity and fluid circulation that could enhance flank
instability. Our results provide new findings about the geometry of the unstable Etna flank
and its relation to faults and subsurface structures.
Beschreibung:
Published
Beschreibung:
B03216
Beschreibung:
1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
Beschreibung:
3.2. Tettonica attiva
Beschreibung:
3.3. Geodinamica e struttura dell'interno della Terra
Beschreibung:
3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
Beschreibung:
JCR Journal
Beschreibung:
restricted
Schlagwort(e):
Etna
;
magnetotelluric
;
flank instability
;
volcano
;
04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneous
;
04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneous
;
04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methods
;
04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous
;
04. Solid Earth::04.04. Geology::04.04.09. Structural geology
;
04. Solid Earth::04.05. Geomagnetism::04.05.99. General or miscellaneous
;
04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous
;
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
;
04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
Repository-Name:
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Materialart:
article
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