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| Titel |
Potential field and bathymetric constraints on volcanism and tectonics at the submarine Monowai cone and caldera (Kermadec arc) |
| VerfasserIn |
M. Paulatto, A. B. Watts, C. Peirce, J. Hunter, D. Basset, W. Stratford, L. M. Kalnins |
| Konferenz |
EGU General Assembly 2012
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 14 (2012) |
| Datensatznummer |
250065694
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| Zusammenfassung |
| Repeat swath-bathymetric surveys have been carried out over the Monowai volcanic centre
since 1998. The system is one of the most active in the Tonga-Kermadec arc and
comprises an active submarine stratovolcano (the Monowai cone) and a hydrothermally
active submarine mafic caldera (the Monowai caldera), the largest known mafic
caldera on Earth. During a recent survey in April-June 2011 on board R/V Sonne we
collected additional bathymetric data as well as, for the first time, marine gravity and
magnetic data over the volcanic centre. The Monowai caldera is characterised by a
Bouguer gravity anomaly high, corresponding to a mass excess of ~1.5-
1013 kg.
Forward modelling and inversion of the anomaly require a shallow body with a
high-density contrast of several tens of km3. The body likely represents an igneous
intrusion, perhaps a system of sills, of about 4-5 km radius and 1-2 km thick. The
intrusive body is slightly elongate in a direction perpendicular to the strike of a
system of extensive faults that dissects the northwestern part of the volcanic arc.
Conversely, the Monowai cone is characterised by a Bouguer gravity anomaly low,
indicating the absence of a high density core common at many stratovolcanoes,
and perhaps the presence of melt in the uppermost part of the crust. A relatively
low-density edifice may be indicative of a fast formation mechanism, as suggested by
repeat bathymetric observations of very fast growth at the summit of Monowai
cone. The orientation of bathymetric features, faults and gravity anomalies, and the
southward migration of volcanic activity by about 400 m over the past 8 years,
are indicative of a close interplay between volcanism and tectonics at Monowai. |
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