about
Precursory changes in seismic velocity for the spectrum of earthquake failure modesThe role of fluid pressure in induced vs. triggered seismicity: insights from rock deformation experiments on carbonates.Aftershocks driven by a high-pressure CO2 source at depthHeterogeneous strength and fault zone complexity of carbonate-bearing thrusts with possible implications for seismicityA novel and versatile apparatus for brittle rock deformationFrictional strength and healing behavior of phyllosilicate-rich faultsFault-surface geometry controlled by faulting mechanisms: Experimental observations in limestone faultsEarthquakes and fault zone structureThermal decomposition along natural carbonate faults during earthquakesFault strength in thin-skinned tectonic wedges across the smectite-illite transition: Constraints from friction experiments and critical tapersDevelopment of interconnected talc networks and weakening of continental low-angle normal faultsFriction and scale-dependent deformation processes of large experimental carbonate faultsDeformation Processes, Textural Evolution and Weakening in Retrograde SerpentinitesFault structure, frictional properties and mixed-mode fault slip behaviorChapter 4 Fault Zone Structure and Deformation Processes along an Exhumed Low-Angle Normal FaultFault zone fabric and fault weaknessLooking at fault reactivation matching structural geology and seismological dataFaults smooth gradually as a function of slipFrictional Properties of a Low-Angle Normal Fault Under In Situ Conditions: Thermally-Activated Velocity WeakeningFrictional properties and slip stability of active faults within carbonate–evaporite sequences: The role of dolomite and anhydriteStabilization of fault slip by fluid injection in the laboratory and in situCan grain size sensitive flow lubricate faults during the initial stages of earthquake propagation?Fault architecture and deformation mechanisms in exhumed analogues of seismogenic carbonate-bearing thrustsThe mechanical paradox of low-angle normal faults: Current understanding and open questionsComment on “Structural controls on a carbon dioxide-driven mud volcano field in the Northern Apennines (Pieve Santo Stefano, Italy): Relations with pre-existing steep discontinuities and seismicity”Growth and deformation mechanisms of talc along a natural fault: a micro/nanostructural investigationThe Internal Structure of Dilational Stepovers in Regional Transtension ZonesA mechanical model for complex fault patterns induced by evaporite dehydration and cyclic changes in fluid pressureA slip tendency analysis to test mechanical and structural control on aftershock rupture planesA low-angle normal fault in the Umbria region (Central Italy): a mechanical model for the related microseismicitySeismic expression of active extensional faults in northern Umbria (Central Italy)
P50
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P50
description
researcher ORCID ID = 0000-0002-4828-2516
@en
wetenschapper
@nl
name
Cristiano Collettini
@ast
Cristiano Collettini
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Cristiano Collettini
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Cristiano Collettini
@nl
type
label
Cristiano Collettini
@ast
Cristiano Collettini
@en
Cristiano Collettini
@es
Cristiano Collettini
@nl
prefLabel
Cristiano Collettini
@ast
Cristiano Collettini
@en
Cristiano Collettini
@es
Cristiano Collettini
@nl
P106
P1153
6603213906
P21
P31
P496
0000-0002-4828-2516