On the mechanical behaviour of a low-angle normal fault: the Alto Tiberina fault (Northern Apennines, Italy) system case study
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[1] Enrico Serpelloni,et al. Creep and locking of a low‐angle normal fault: Insights from the Altotiberina fault in the Northern Apennines (Italy) , 2016 .
[2] C. Collettini,et al. Heterogeneous strength and fault zone complexity of carbonate-bearing thrusts with possible implications for seismicity , 2014 .
[3] L. Valoroso. Seismic Activity Along a Low-Angle Normal Fault: The Case Study of the Alto Tiberina Fault (Northern Apennines, Italy). , 2014 .
[4] C. Collettini,et al. The Alto Tiberina Near Fault Observatory (northern Apennines, Italy) , 2014 .
[5] L. Vadacca. Numerical modeling of the Alto Tiberina low angle normal fault , 2014 .
[6] E. Serpelloni,et al. Active tectonic extension across the Alto Tiberina normal fault system from GPS data modeling and InSAR velocity maps: new perspectives within TABOO Near Fault Observatory , 2014 .
[7] S. Barba,et al. Interpreting the interseismic deformation of the Altotiberina Fault (central Italy) through 2D modelling , 2014 .
[8] F. Brozzetti,et al. Tectonic evolution of a low‐angle extensional fault system from restored cross‐sections in the Northern Apennines (Italy) , 2011 .
[9] C. Collettini. The mechanical paradox of low-angle normal faults: Current understanding and open questions , 2011 .
[10] S. Hickman,et al. Low strength of deep San Andreas fault gouge from SAFOD core , 2011, Nature.
[11] D. Faulkner,et al. Laboratory measurements of the frictional properties of the Zuccale low-angle normal fault, Elba Island, Italy , 2010 .
[12] L. Jolivet,et al. The North Cycladic Detachment System , 2010 .
[13] M. Barchi,et al. Seismic images of an extensional basin, generated at the hangingwall of a low-angle normal fault: The case of the Sansepolcro basin (Central Italy) , 2009 .
[14] C. Collettini,et al. Fault zone fabric and fault weakness , 2009, Nature.
[15] L. Chiaraluce,et al. A decade of passive seismic monitoring experiments with local networks in four Italian regions , 2009 .
[16] N. D’Agostino,et al. Contemporary crustal extension in the Umbria–Marche Apennines from regional CGPS networks and comparison between geodetic and seismic deformation , 2009 .
[17] S. Hreinsdóttir,et al. Active aseismic creep on the Alto Tiberina low-angle normal fault, Italy , 2009 .
[18] Robert E. Holdsworth,et al. Development of interconnected talc networks and weakening of continental low-angle normal faults , 2009 .
[19] E. Tinti,et al. Modelling deformation rates in the western Gulf of Corinth: rheological constraints , 2008 .
[20] D. Lockner,et al. Talc friction in the temperature range 25°–400 °C: relevance for fault-zone weakening , 2008 .
[21] E. Stucchi,et al. Insights on the seismogenic layer thickness from the upper crust structure of the Umbria‐Marche Apennines (central Italy) , 2008 .
[22] C. Collettini,et al. Architecture and mechanics of an active low‐angle normal fault: Alto Tiberina Fault, northern Apennines, Italy , 2007 .
[23] T. Mitchell,et al. Slip on 'weak' faults by the rotation of regional stress in the fracture damage zone , 2006, Nature.
[24] Paolo Baldi,et al. Crustal velocity and strain-rate fields in Italy and surrounding regions: new results from the analysis of permanent and non-permanent GPS networks , 2005 .
[25] C. Collettini,et al. Fault zone weakening and character of slip along low-angle normal faults: insights from the Zuccale fault, Elba, Italy , 2004, Journal of the Geological Society.
[26] S. Merlini,et al. The Gubbio normal fault (Central Italy): geometry, displacement distribution and tectonic evolution , 2004 .
[27] S. Pondrelli,et al. An improved stress map for Italy and surrounding regions (central Mediterranean) , 2004 .
[28] D. Pantosti,et al. Geomorphology of the Gubbio Basin (Central Italy): understanding the active tectonics and earthquake potential , 2003 .
[29] C. Marone,et al. Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts , 2003 .
[30] C. Federico,et al. Elastic modeling of the Alto Tiberina normal fault (central Italy): geometry and lithological stratification influences on the local stress field , 2003 .
[31] A. Kopf,et al. Compositional and Fluid Pressure Controls on the State of Stress on the Nankai Subduction Thrust , 2003 .
[32] C. Collettini,et al. The Gubbio fault: can different methods give pictures of the same object? , 2003 .
[33] J. Knott,et al. Quaternary low-angle slip on detachment faults in Death Valley, California , 2003 .
[34] D. Faulkner,et al. On the internal structure and mechanics of large strike-slip fault zones: field observations of the Carboneras fault in southeastern Spain , 2001 .
[35] R. Sibson,et al. Normal faults, normal friction? , 2001 .
[36] Giusy Lavecchia,et al. Architecture and seismotectonics of a regional low‐angle normal fault zone in central Italy , 2000 .
[37] N. Voulgaris,et al. Microseismicity and faulting geometry in the Gulf of Corinth (Greece) , 2000 .
[38] R. Westaway. The mechanical feasibility of low-angle normal faulting , 1999 .
[39] A. Deschamps,et al. A microseismic study in the western part of the Gulf of Corinth (Greece): implications for large‐scale normal faulting mechanisms , 1996 .
[40] F. Scherbaum,et al. Seismic slip on a low angle normal fault in the Gulf of Corinth: Evidence from high‐resolution cluster analysis of microearthquakes , 1996 .
[41] J. Boatwright,et al. Frictional constraints on crustal faulting , 1996 .
[42] J. Dieterich. A constitutive law for rate of earthquake production and its application to earthquake clustering , 1994 .
[43] W. Buck,et al. Effect of lithospheric thickness on the formation of high- and low-angle normal faults , 1993 .
[44] B. John,et al. Structural and thermal constraints on the initiation angle of detachment faulting in the southern Basin and Range: The Chemehuevi Mountains case study , 1993 .
[45] Terry Engelder,et al. Stress Regimes in the Lithosphere , 1992 .
[46] Rob Westaway,et al. Seismological and field observations of the 1984 Lazio‐Abruzzo earthquakes: implications for the active tectonics of Italy , 1989 .
[47] R. Console,et al. The Perugia (Italy) earthquake of 29, April 1984: A microearthquake survey , 1988 .
[48] M. Zoback,et al. New Evidence on the State of Stress of the San Andreas Fault System , 1987, Science.
[49] J. Byerlee. Friction of rocks , 1978 .
[50] R. Holdsworth,et al. Lithological controls on the deformation mechanisms operating within carbonate-hosted faults during the seismic cycle. , 2014 .
[51] Massimiliano Stucchi,et al. CPTI11, the 2011 version of the Parametric Catalogue of Italian Earthquakes , 2011 .
[52] C. Collettini,et al. The microstructural character and mechanical significance of fault rocks associated with a continental low-angle normal fault: the Zuccale Fault, Elba Island, Italy , 2011 .
[53] T. Mitchell,et al. On the structure and mechanical properties of large strike-slip faults , 2008 .
[54] About this title ‐ The Internal Structure of Fault Zones: Implications for Mechanical and Fluid-Flow Properties , 2008 .
[55] Agust Gudmundsson,et al. Effects of Young's modulus on fault displacement , 2004 .
[56] J. Jackson,et al. Normal faulting in the upper continental crust: observations from regions of active extension , 1989 .
[57] G. Lister,et al. The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region, U.S.A. , 1989 .
[58] R. Sibson. A note on fault reactivation , 1985 .