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Citation: M. Dragoni et al., STRESS-FIELD AT A TRANSCURRENT PLATE BOUNDARY IN THE PRESENCE OF FRICTIONAL HEAT-PRODUCTION AT DEPTH (VOL 150, PG 181, 1997), Pure and Applied Geophysics, 152(2), 1998, pp. 377-377
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Citation: M. Dragoni et al., MAGNETIC-ANISOTROPY PRODUCED BY MAGMA FLOW - THEORETICAL-MODEL AND EXPERIMENTAL-DATA FROM FERRAR DOLERITE SILLS (ANTARCTICA), Geophysical journal international, 128(1), 1997, pp. 230-240
Citation: M. Dragoni et al., STRESS-FIELD AT A TRANSCURRENT PLATE BOUNDARY IN THE PRESENCE OF FRICTIONAL HEAT-PRODUCTION AT DEPTH, Pure and Applied Geophysics, 150(2), 1997, pp. 181-201
Citation: M. Dragoni et A. Tallarico, A MODEL FOR THE OPENING OF EPHEMERAL VENTS IN A STATIONARY LAVA FLOW, Journal of volcanology and geothermal research, 74(1-2), 1996, pp. 39-47
Citation: M. Dragoni et al., EVALUATION OF STRESSES IN 2 GEODYNAMICALLY DIFFERENT AREAS - STABLE FORELAND AND EXTENSIONAL BACKARC, Pure and Applied Geophysics, 146(2), 1996, pp. 319-341
Citation: M. Dragoni et A. Tallarico, THE EFFECT OF CRYSTALLIZATION ON THE RHEOLOGY AND DYNAMICS OF LAVA FLOWS, Journal of volcanology and geothermal research, 59(3), 1994, pp. 241-252
Citation: M. Dragoni et al., RHEOLOGICAL CONSEQUENCES OF THE LITHOSPHERIC THERMAL STRUCTURE IN THEFENNOSCANDIAN SHIELD, Global and planetary change, 8(3), 1993, pp. 113-126
Citation: M. Dragoni et al., A VISCOELASTIC SHEAR ZONE MODEL OF COMPRESSIONAL AND EXTENSIONAL PLATE BOUNDARIES, Pure and Applied Geophysics, 140(3), 1993, pp. 471-491
Citation: M. Dragoni et A. Piombo, PROPAGATION OF AN ASEISMIC DISLOCATION THROUGH ASPERITIES WITH SMOOTHBORDERS, Physics of the earth and planetary interiors, 80(1-2), 1993, pp. 1-11
Authors:
BANFI S
DRAGONI M
MONTANARI F
POZZI G
QUICI S
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