2014 - Member of Academia Europaea
His main research concerns Seismology, Slip, Stress, Fault and Aftershock. His Seismology study frequently links to related topics such as Geophysics. The study incorporates disciplines such as Fracture mechanics, Scaling and Geodesy in addition to Slip.
His research in Stress intersects with topics in Fluid dynamics, Magnitude and Magma chamber. His Fault research integrates issues from Induced seismicity and Stress field. His work deals with themes such as Seismotectonics, Focal mechanism and Crust, which intersect with Aftershock.
His scientific interests lie mostly in Seismology, Slip, Aftershock, Fault and Induced seismicity. His biological study spans a wide range of topics, including Stress, Magnitude and Geodesy. His study in Slip is interdisciplinary in nature, drawing from both Shear and Fracture mechanics.
His Foreshock study, which is part of a larger body of work in Aftershock, is frequently linked to Coulomb, bridging the gap between disciplines. Massimo Cocco combines subjects such as Stress field, Geophysics and Sequence with his study of Fault. In general Induced seismicity, his work in Focal mechanism is often linked to Perturbation, Rate change and State dependent linking many areas of study.
Massimo Cocco mainly investigates Seismology, Slip, L aquila, Service provision and Fault. The concepts of his Seismology study are interwoven with issues in Geodetic datum and Geodesy. His Slip research is multidisciplinary, incorporating elements of Normal fault and Shear.
His studies deal with areas such as Magnitude, Microseism and Extensional fault as well as Fault. His Earthquake rupture course of study focuses on Tsunami earthquake and Finite element method. Massimo Cocco has researched Seismic moment in several fields, including Aftershock, Structural geology, Scaling and Scale invariance.
His primary areas of investigation include Seismology, Slip, Geodetic datum, Global Positioning System and Kinematic inversion. His work on Earthquake rupture and Induced seismicity is typically connected to Observatory and Exponential decay as part of general Seismology study, connecting several disciplines of science. Massimo Cocco interconnects Fault, Seismometer and Scaling in the investigation of issues within Slip.
His Geodetic datum research incorporates elements of Tsunami earthquake, Episodic tremor and slip, Finite element method and Seismic slip. His Global Positioning System research is multidisciplinary, incorporating perspectives in Seafloor spreading, Submarine pipeline and Subduction. Massimo Cocco has included themes like Normal fault, Hypocenter, Ground shaking and Geodesy in his Kinematic inversion study.
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Aftershocks driven by a high-pressure CO2 source at depth.
Stephen A. Miller;Cristiano Collettini;Lauro Chiaraluce;Massimo Cocco.
Nature (2004)
Fault lubrication during earthquakes
G. Di Toro;G. Di Toro;R. Han;T. Hirose;N. De Paola.
Nature (2011)
Fault interaction by elastic stress changes: New clues from earthquake sequences
G.C.P. King;M. Cocco.
Advances in Geophysics (2001)
The 1997 Umbria‐Marche, Italy, Earthquake Sequence: A first look at the main shocks and aftershocks
A. Amato;R. Azzara;C. Chiarabba;G. Cimini.
Geophysical Research Letters (1998)
Pore pressure and poroelasticity effects in Coulomb stress analysis of earthquake interactions
Massimo Cocco;James R. Rice.
Journal of Geophysical Research (2002)
Limited overlap between the seismic gap and coseismic slip of the great 2010 Chile earthquake
S. Lorito;F. Romano;S. Atzori;X. Tong.
Nature Geoscience (2011)
Introduction to special section: Stress transfer, earthquake triggering, and time‐dependent seismic hazard
Sandy Steacy;Joan Gomberg;Massimo Cocco.
Journal of Geophysical Research (2005)
Frictional constraints on crustal faulting
John Boatwright;Massimo Cocco.
Journal of Geophysical Research (1996)
Rupture history of the 2009 L'Aquila (Italy) earthquake from non‐linear joint inversion of strong motion and GPS data
A. Cirella;A. Piatanesi;M. Cocco;E. Tinti.
Geophysical Research Letters (2009)
Two‐way coupling between Vesuvius eruptions and southern Apennine earthquakes, Italy, by elastic stress transfer
Concetta Nostro;Ross S. Stein;Massimo Cocco;Maria Elina Belardinelli.
Journal of Geophysical Research (1998)
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