Interpretation of tectonic versus magmatic processes for resetting apatite fission track ages in the Niğde Massif, Turkey |
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| Authors: | Annia K Fayon Donna L Whitney |
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| Institution: | aDep. Estructura i Dinàmica de la Terra, Institut de Ciències de la Terra ‘Jaume Almera’ IJA-CSIC, Solé i Sabaris s/n. 08028 Barcelona, Spain |
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| Abstract: | A network of 10 OBS operating in continuous recording mode was deployed in June 2003 in the Galicia passive Margin, surrounding the sinking zone of the ‘Prestige’ oil tanker. The OBSs recorded very different signals, including air-gun shots, seismic events, whale vocalizations or noise associated to ships, as well as two sets of atypical seismic signals that are the object of this contribution and can be described as harmonic tremors and short-duration events. Harmonic tremors appear in most sites as intense monochromatic signals lasting for up to 4 h, with coherent polarization and a wide range of amplitudes. Even if they may be recorded at different sites within a time interval, their envelopes are not correlated, suggesting a source origin at the vicinity of each receiver. A time periodicity close to 6 h is observed, suggesting a correlation with the tidal variation. Most OBSs show also a large number of impulsive events of short-duration, between 1 and 2 s, a very regular decrease of amplitude in the signal coda and characteristic frequency spectrum with one or two narrow peaks. As for the tremors, those events are detected only in individual sites, suggesting very local source zones. We favor the interpretation of both seismic features as coming from the resonance of fluid-filled cracks induced by impulsive pressure transients, in agreement with the theoretical model of Chouet Chouet, B. 1988. Resonance of a fluid-driven crack: radiation properties and implications for the source of long-period events and harmonic tremor. J. Geophys. Res., 93, 4375–4400.]. The observed harmonic tremors would be the result of sustained pressure fluctuations, probably related to the stress variations induced by the tidal change of the oceanic load, while the short duration events are interpreted as the impulse response to the tremor-generating system. |
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| Keywords: | Atypical seismic signals Galicia passive margin Harmonic tremors Tidal correlation Short-duration events Resonance of fluid-filled cracks |
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