eprintid: 1742 rev_number: 9 eprint_status: archive userid: 6 dir: disk0/00/00/17/42 datestamp: 2016-09-15 12:24:33 lastmod: 2017-02-08 12:21:44 status_changed: 2016-09-15 12:24:33 type: article metadata_visibility: show creators_name: Zollo, Aldo creators_name: Orefice, Antonella creators_name: Convertito, Vincenzo corp_creators: Dipartimento di Scienze Fisiche, Università di Napoli “Federico II”, Naples, Italy corp_creators: Dipartimento di Scienze Fisiche, Università di Napoli “Federico II”, Naples, Italy corp_creators: Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Naples, Italy title: Source parameter scaling and radiation efficiency of microearthquakes along the Irpinia fault zone in southern Apennines, Italy subjects: MP1 subjects: RIt full_text_status: none abstract: We analyzed the P and S wave displacement spectra of 717 microearthquakes in the moment range 4 × 109 − 2 × 1014 N m recorded at the dense networks operating in southern Apennines (Italy) and deployed along the 1980 Ms 6.9 Irpinia earthquake fault zone. Source, attenuation, and site parameters are estimated by using a parametric modeling approach, which is combined with a multistep, nonlinear inversion strategy. We found that in the analyzed frequency band, an attenuation model with constant Q has to be preferred to frequency-dependent Q models. Consistent estimates of the median P and S quality factors inline image (90; 296) and inline image (114; 417) are obtained from two different techniques and relatively high values of QS/QP (median value 1.3, (0.8; 2.1)) are found in the same depth range where high VP/VS and a peak in seismicity distribution are observed. This is the evidence for a highly fractured, partially, or completely fluid-saturated medium embedding the Irpinia fault zone, down to crustal depths of 15–20 km. A nearly constant stress drop (inline image, (0.4; 5.0)) and apparent stress (inline image, (0.03, 0.4)) scaling of P and S corner frequencies and seismic energies is observed above a seismic moment value of about 1011 N m. The measured radiation efficiency is low (inline image), e.g., the radiated energy is only a small fraction of the whole energy spent by friction and fracture development. A large positive dynamic overshoot (high dynamic shear strength) can be the dominant mechanism controlling the microearthquake fractures along the Irpinia fault zone. date: 2014-04 date_type: published publication: Journal of Geophysical Research: Solid Earth volume: 119 number: 4 publisher: John Wiley & Sons pagerange: 3256-3275 id_number: doi:10.1002/2013JB010116 issn: 2169-9313 official_url: http://doi.org/10.1002/2013JB010116 access_IS-EPOS: limited owner: Publisher citation: Zollo, Aldo and Orefice, Antonella and Convertito, Vincenzo (2014) Source parameter scaling and radiation efficiency of microearthquakes along the Irpinia fault zone in southern Apennines, Italy. Journal of Geophysical Research: Solid Earth, 119 (4). pp. 3256-3275. DOI: https://doi.org/10.1002/2013JB010116