Feedback processes between magmatic events and flank movement at Mount Etna (Italy) during the 2002-2003 eruption
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Thomas R. Walter | Falk Amelung | Valerio Acocella | Marco Neri | F. Amelung | M. Neri | V. Acocella | T. Walter
[1] Roger P. Denlinger,et al. SPREADING VOLCANOES 1 , 2000 .
[2] F. Amelung,et al. Rift zone reorganization through flank instability in ocean island volcanoes: an example from Tenerife, Canary Islands , 2005 .
[3] Rosa Anna Corsaro,et al. Paleo-environmental and volcano-tectonic evolution of the southeastern flank of Mt. Etna during the last 225 ka inferred from the volcanic succession of the ‘Timpe’, Acireale, Sicily , 2002 .
[4] S. L. Crouch. Boundary element methods in solid mechanics: With applications in rock mechanics and geological engineering , 1983 .
[5] I. Selwyn Sacks,et al. Triggering of volcanic eruptions , 1998, Nature.
[6] M. Neri,et al. The boundaries of large-scale collapse on the flanks of Mount Etna, Sicily , 1996, Geological Society, London, Special Publications.
[7] Boris Behncke,et al. The role of the Pernicana Fault System in the spreading of Mt. Etna (Italy) during the 2002–2003 eruption , 2004 .
[8] M. Ohtake,et al. Tidal triggering of earthquakes in Japan related to the regional tectonic stress , 2004 .
[9] S. L. Crouch,et al. Boundary element methods in solid mechanics , 1983 .
[10] A. Bonaccorso,et al. Etna 2002 eruption imaged from continuous tilt and GPS data , 2003 .
[11] S. Hickman,et al. Pore fluid pressure, apparent friction, and Coulomb failure , 2000 .
[12] E. Casarotti,et al. Modeling the stress variations induced by great earthquakes on the largest volcanic eruptions of the 20th century , 2002 .
[13] Donald A. Swanson,et al. Displacement of the south flank of Kilauea Volcano; the result of forceful intrusion of magma into the rift zones , 1976 .
[14] B. Behncke,et al. Nested zones of instability in the Mount Etna volcanic edifice, Italy , 2005 .
[15] Max Wyss,et al. The locations of magma chambers at Mt. Etna, Italy, mapped by b‐values , 1999 .
[16] Christopher R. J. Kilburn,et al. Multiscale fracturing as a key to forecasting volcanic eruptions , 2003 .
[17] Carlos Alberto Brebbia,et al. The Boundary Element Method in Engineering Practice , 1984 .
[18] Eugenio Sansosti,et al. Gravity and magma induced spreading of Mount Etna volcano revealed by satellite radar interferometry , 2004 .
[19] Boris Behncke,et al. Contrasting triggering mechanisms of the 2001 and 2002-2003 eruptions of Mount Etna (Italy) , 2005 .
[20] A. Borgia,et al. Importance of gravitational spreading in the tectonic and volcanic evolution of Mount Etna , 1992, Nature.
[21] F. Amelung,et al. Influence of volcanic activity at Mauna Loa, Hawaii, on earthquake occurrence in the Kaoiki Seismic Zone , 2004 .
[22] Warner Marzocchi,et al. Two‐way coupling between Vesuvius eruptions and southern Apennine earthquakes, Italy, by elastic stress transfer , 1998 .
[23] G. Fornaro,et al. Coupled magma chamber inflation and sector collapse slip observed with synthetic aperture radar interferometry on Mt. Etna volcano , 2003 .
[24] M. Neri,et al. What makes flank eruptions? The 2001 Etna eruption and its possible triggering mechanisms , 2003 .
[25] Boris Behncke,et al. Cycles and trends in the recent eruptive behaviour of Mount Etna (Italy) , 2003 .
[26] M. Burton,et al. High spatial resolution radon measurements reveal hidden active faults on Mt. Etna , 2004 .
[27] F. Pollitz,et al. Earthquake–Volcano Interactions , 2002 .
[28] J. Dieterich,et al. Stress changes before and during the Pu'u 'ō'Ō-KŪpaianaha eruption , 2003 .
[29] S. Saunders,et al. Recent dyke-induced large-scale block movement at Mount Etna and potential slope failure , 1990, Nature.
[30] G. Puglisi,et al. Ground deformation patterns on Mount Etna, 1992 to 1994, inferred from GPS data , 2001 .
[31] Coupling of eruptions and earthquakes at Mt. Etna (Sicily, Italy): A case study from the 1981 and 2001 events , 2005 .
[32] H. Kanamori,et al. A single-force model for the 1975 Kalapana, Hawaii, Earthquake , 1987 .
[33] Salvatore D'Amico,et al. Link between major flank slip and 2002–2003 eruption at Mt. Etna (Italy) , 2003 .
[34] J. Dieterich. Growth and persistence of Hawaiian volcanic rift zones , 1988 .
[35] F. Greco,et al. Intrusive mechanism of the 2002 NE‐Rift eruption at Mt. Etna (Italy) inferred through continuous microgravity data and volcanological evidences , 2003 .
[36] Maria Comninou,et al. The angular dislocation in a half space , 1975 .
[37] M. Neri,et al. Structural features of an active strike-slip fault on the sliding flank of Mt. Etna (Italy) , 2005 .
[38] R. Stein. The role of stress transfer in earthquake occurrence , 1999, Nature.
[39] B. Behncke,et al. Lava flow hazard at Mount Etna (Italy): New data from a GIS-based study , 2005 .
[40] Giuseppe Puglisi,et al. Magma uprising and flank dynamics on Mount Etna volcano, studied using GPS data (1994–1995) , 2003 .
[41] E. Roeloffs. Poroelastic Techniques in the Study of Earthquake-Related Hydrologic Phenomena , 1996 .
[42] L. Siebert. Threats from debris avalanches , 1992, Nature.
[43] A. Tibaldi,et al. Volcano-tectonic activity along structures of the unstable NE flank of Mt. Etna (Italy) and their possible origin , 2002 .
[44] J. C. Savage,et al. Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula, Japan , 1982 .
[45] Claudio Chiarabba,et al. Magma Ascent and the Pressurization of Mount Etna's Volcanic System , 2003, Science.
[46] Ruth A. Harris,et al. Introduction to Special Section: Stress Triggers, Stress Shadows, and Implications for Seismic Hazard , 1998 .
[47] D. Patanè,et al. High‐precision locations of the microseismicity preceding the 2002–2003 Mt. Etna eruption , 2004 .