SEARCH

SEARCH BY CITATION

References

  • Adams, D. A., and R. E. Abercrombie (1998), Seismic attenuation above 10 Hz in southern California from coda waves recorded in the Cajon Pass borehole, J. Geophys. Res., 103, 24,25724,270.
  • Aki, K. (1967), Scaling law of seismic spectrum, J. Geophys. Res., 72, 12171231.
  • Aloisi, M., O. Cocina, G. Neri, B. Orecchio, and E. Privitera (2002), Seismic tomography of the crust underneath the Etna volcano, Sicily, Phys. Earth Planet. Inter., 134, 139155.
  • Atkinson, G. M. (1995), Attenuation and source parameters of earthquakes in the Cascadia region, Bull. Seismol. Soc. Am., 85, 13271342.
  • Berckhemer, H., W. Kampfmann, E. Aulbach, and H. Schmeling (1982), Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experiments, Phys. Earth Planet. Inter., 29, 3041.
  • Boitnott, G. N. (1995), Laboratory measurements on reservoir rocks from The Geyser geothermal field, paper presented at 20th Workshop on Geothermal Reservoir Engineering, Stanford Univ., Stanford, Calif.
  • Boitnott, G. N., and P. J. Boyd (1996), Permeability, electrical impedance, and acoustic velocities on reservoir rocks from The Geysers geothermal field, paper presented 21st Workshop on Geothermal Reservoir Engineering, Stanford Univ., Stanford, Calif.
  • Bonaccorso, A., and P. M. Davis (2004), Modeling of ground deformation associated with recent lateral eruptions: Mechanics of magma ascent and intermediate storage at Mount Etna, in Mount Etna: Volcano Laboratory, Geophys. Monogr. Ser., vol. 143, edited by S. Calvari et al., pp. 293306, AGU, Washington, D.C.
  • Bourbiè, T., O. Coussy, and B. Zinszner (1987), Acoustics of Porous Media, Gulf Publ. Co., Houston, Tex.
  • Brune, J. N. (1970), Tectonic stress and the spectra of seismic shear waves from earthquakes, J. Geophys. Res., 75, 49975009.
  • Budetta, G., D. Carbone, F. Greco, and H. Rymer (2004), Microgravity studies at Mount Etna (Italy), in Mount Etna: Volcano Laboratory, Geophys. Monogr. Ser., vol. 143, edited by S. Calvari et al., pp. 221240, AGU, Washington, D.C.
  • Chiarabba, C., A. Amato, and E. Boschi (2000), Recent seismicity and tomographic modeling of the Mount Etna plumbing system, J. Geophys. Res., 105, 10,92310,938.
  • Chiarabba, C., P. De Gori, and D. Patanè (2004), The Mount Etna plumbing system: The contribution of seismic tomography, in Mount Etna: Volcano Laboratory, Geophys. Monogr. Ser., vol. 143, edited by S. Calvari et al., pp. 191204, Washington, D.C.
  • Clawson, S. R., R. B. Smith, and H. M. Benz (1989), P wave attenuation of the Yellowstone Caldera from three-dimensional inversion of spectral decay using explosion source seismic data, J. Geophys. Res., 94, 72057222.
  • Corsaro, R. A., and M. Pompilio (2004), Dynamics of magmas at Mount Etna, in Mt. Etna: Volcano Laboratory, Geophys. Monogr. Ser., vol. 143, edited by S. Calvari et al., pp. 91110, AGU, Washington, D.C.
  • Del Pezzo, E., and D. Patanè (1992), Coda Q dependence on time, frequency and coda duration interval at Mt. Etna, Sicily, in Volcanic Seismology, edited by P. Gasparini, R. Scarpa, and K. Aki, IAVCEI Proc. Volcanol., 3, 109119.
  • Del Pezzo, E., S. Gresta, D. Patanè, G. Patanè, and S. Scarcella (1987), Attenuation of short period seismic waves at Etna as compared to other volcanic areas, Pure Appl. Geophys., 125, 10391050.
  • Eberhart-Phillips, D., and M. Chadwick (2002), Three-dimensional attenuation model of the shallow Hikurangi subduction zone in the Raukumara Peninsula, New Zealand, J. Geophys. Res., 107(B2), 2033, doi:10.1029/2000JB000046.
  • Evans, J. R., and J. J. Zucca (1993), Active source, high-resolution (NeHT) tomography: Velocity and Q, in Seismic Tomography: Theory and Practice, edited by H. Iyer, and K. Hirahara, pp. 695732, CRC Press, Boca Raton, Fla.
  • Giampiccolo, E., S. Gresta, and G. Ganci (2003), Attenuation of body waves in Southeastern Sicily (Italy), Phys. Earth Planet. Inter., 135, 267279.
  • Gunasekera, R. C., G. R. Foulger, and B. R. Julian (2003), Reservoir depletion at The Geysers geothermal area, California, shown by four-dimensional seismic tomography, J. Geophys. Res., 108(B3), 2134, doi:10.1029/2001JB000638.
  • Haberland, C., and A. Rietbrock (2001), Attenuation tomography in the western central Andes: A detailed insight into the structure of a magmatic arc, J. Geophys. Res., 106, 11,15111,167.
  • Hirn, A., A. Nercessian, M. Sapin, F. Ferrucci, and G. Wittlinger (1991), Seismic activity accompanying the outbreak of the 1991–1993 eruption of Mt. Etna, Geophys. J. Int., 105, 139153.
  • Ibanez, J. M., E. Del Pezzo, M. Martini, D. Patanè, F. De Miguel, F. Vidal, and J. Morales (1993), Estimates of coda-Q using a non-linear regression, J. Phys. Earth, 41, 203219.
  • Ito, H., J. DeVilbiss, and A. Nur (1979), Compressional and shear waves in saturated rocks during steam-water transition, J. Geophys. Res., 84, 47314735.
  • Knopoff, K. (1964), Q, Rev. Geophys, 2, 625660.
  • Laigle, M., H. Hirn, M. Sapin, and J. C. Lepine (2000), Mount Etna dense array local earthquake P and S tomography and implications for volcanic plumbing, J. Geophys. Res., 105, 21,63321,646.
  • Lees, J. M., and G. T. Lindley (1994), Three-dimensional attenuation tomography at Loma-Prieta: Inversion of t* for Q, J. Geophys. Res., 99, 68436863.
  • Mavko, G. M. (1980), Velocity and attenuation in partially molten rocks, J. Geophys. Res., 85, 51735189.
  • Mavko, G. M., and A. Nur (1979), Wave attenuation in partially saturated rocks, Geophysics, 44, 161178.
  • Menke, W., D. Witte, and R. Chen (1985), Laboratory test of apparent attenuation formula, Bull. Seismol. Soc. Am., 75, 13831393.
  • Michelini, A., and T. V. McEvilly (1991), Seismological studies at Parkfield, I, Simultaneous inversion for velocity structure and hypocentres using cubic b-splines parameterization, Bull. Seismol. Soc Am., 81, 524552.
  • Murase, T., and A. R. McBirney (1973), Properties of some common igneous rocks and their melts at high temperatures, Geol. Soc. Am. Bull., 84, 35633592.
  • Nur, A., J. D. Walls, K. Winkler, and J. De Vilbiss (1980), Effects of fluid saturation on waves in porous rock and relations to hydraulic permeability, SPE J., 20, 450458.
  • Patanè, D., and E. Giampiccolo (2004), Faulting processes and earthquake source parameters at Mt. Etna: State of the art and perspectives, in Mt. Etna: Volcano Laboratory, Geophys. Monogr. Ser., vol. 143, edited by S. Calvari et al., pp. 167189, Washington, D.C.
  • Patanè, D., F. Ferrucci, and S. Gresta (1994), Spectral features of microeartquakes in volcanic area: Attenuation in the crust and amplitude response of the site at Mt. Etna, Italy, Bull. Seismol. Soc. Am., 84, 18421860.
  • Patanè, D., F. Ferrucci, E. Giampiccolo, and L. Scaramuzzino (1997), Source scaling of microeartquakes at Mt. Etna volcano and in the Calabrian Arc (southern Italy), Geophys. Res. Lett., 24, 18791882.
  • Patané, D., C. Chiarabba, O. Cocina, P. De Gori, M. Moretti, and E. Boschi (2002), Tomographic images and 3D earthquake locations of the seismic swarm preceding the 2001 Mt. Etna eruption: Evidence for a dyke intrusion, Geophys. Res. Lett., 29(10), 1497, doi:10.1029/2001GL014391.
  • Patanè, D., P. De Gori, C. Chiarabba, and A. Bonaccorso (2003), Magma Ascent and the Pressurization of Mount Etna's Volcanic System, Science, 299, 20612063, doi:10.1126/science.1080653.
  • Reyners, M., D. Eberhart-Phillips, and G. Stuart (1999), A three-dimensional image of shallow subduction: Crustal structure of the Raukumara Peninsula, New Zealand, Geophys. J. Int., 137, 873890.
  • Rietbrock, A. (2001), P wave attenuation structure in the fault area of the 1995 Kobe earthquake, J. Geophys. Res., 106, 41414154.
  • Sanders, C. O., S. C. Ponko, L. D. Nixon, and E. A. Schwartz (1995), Seismological evidence for magmatic and hydrothermal structure in Long Valley caldera from local earthquake attenuation and velocity tomography, J. Geophys. Res., 100, 83118326.
  • Sato, H., I. S. Sacks, T. Murase, G. Muncill, and H. Fukuyama (1989), Qp-melting temperature relation in peridotite at high pressure and temperature: Attenuation mechanism and implications for mechanical properties of the upper mantle, J. Geophys. Res., 94, 10,64710,661.
  • Scherbaum, F. (1990), Combined inversion for the three-dimensional Q structure and source parameters using microearthquake spectra, J. Geophys. Res., 95, 12,42312,438.
  • Thurber, C. H. (1993), Local earthquake tomography: velocity and Vp/Vs theory, in Seismic Tomography: Theory and Practice, edited by H. Iyer, and K. Hirahara, pp. 563580, CRC Press, Boca Raton, Fla.
  • Tomatsu, T., H. Kumagai, and P. B. Dawson (2001), Tomographic inversion of P-wave velocity and Q structures beneath the Kirishima volcanic complex, southern Japan, based on finite difference calculations of complex traveltimes, Geophys. J. Int., 146, 781794.
  • Um, J., and C. H. Thurber (1987), A fast algorithm for two-point seismic ray tracing, Bull. Seismol. Soc. Am., 77, 972986.
  • Winkler, K., and A. Nur (1979), Pore fluids and seismic attenuation in rocks, Geophys. Res. Lett., 6, 14.