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Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake

Science (American Association for the Advancement of Science), 2013-12, Vol.342 (6163), p.1208-1211

2013

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Geological record of fluid flow and seismogenesis along an erosive subducting plate boundary

Nature, 2008-02, Vol.451 (7179), p.699-703

2008

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Does subduction of mass transport deposits (MTDs) control seismic behavior of shallow–level megathrusts at convergent margins?

Gondwana research, 2018-08, Vol.60, p.186-193

2018

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Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts

Geosystems and geoenvironment, 2022-05, Vol.1 (2), p.100030, Article 100030

2022

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Stress State in the Largest Displacement Area of the 2011 Tohoku-Oki Earthquake

Science (American Association for the Advancement of Science), 2013-02, Vol.339 (6120), p.687-690

2013

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Structure and lithology of the Japan Trench subduction plate boundary fault

Tectonics (Washington, D.C.), 2015-01, Vol.34 (1), p.53-69

2015

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Geology of the High Sillaro Valley (Northern Apennines of Italy)

Journal of maps, 2020-12, Vol.16 (2), p.805-817

2020

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Fluid history related to the early Eocene-middle Miocene convergent system of the Northern Apennines (Italy): Constraints from structural and isotopic studies

Journal of Geophysical Research: Solid Earth, 2010-05, Vol.115 (B5), p.n/a

2010

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Deformation structures in the frontal prism near the Japan Trench: Insights from sandbox models

Journal of geodynamics, 2015-09, Vol.89, p.29-38

2015

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Internal structure and tectonic evolution of an underthrust tectonic mélange: the Sestola-Vidiciatico tectonic unit of the Northern Apennines, Italy

Geodinamica acta, 2007-01, Vol.20 (1-2), p.37-51

2007

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From soft sediment deformation to fluid assisted faulting in the shallow part of a subduction megathrust analogue: the Sestola Vidiciatico tectonic Unit (Northern Apennines, Italy)

Geological magazine, 2018-02, Vol.155 (2), p.438-450

2018

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Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments

Science (American Association for the Advancement of Science), 2013-12, Vol.342 (6163), p.1211-1214

2013

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Low Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature Measurements

Science (American Association for the Advancement of Science), 2013-12, Vol.342 (6163), p.1214-1217

2013

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Incrementally developed slickenfibers — Geological record of repeating low stress-drop seismic events?

Tectonophysics, 2011-10, Vol.510 (3), p.381-386

2011

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Toward a dynamic concept of the subduction channel at erosive convergent margins with implications for interplate material transfer

Geochemistry, geophysics, geosystems : G3, 2012-02, Vol.13 (2), p.np-n/a

2012

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Frictional properties of fault zone gouges from the J-FAST drilling project (M sub(w) 9.0 2011 Tohoku-Oki earthquake)

Geophysical research letters, 2015-04, Vol.42 (8), p.2691-2699

2015

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Chapter 3 Aseismic-Seismic Transition and Fluid Regime along Subduction Plate Boundaries and a Fossil Example from the Northern Apennines of Italy

International Geophysics, 2009, Vol.94, p.37-68

2009

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Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake

Geological record of fluid flow and seismogenesis along an erosive subducting plate boundary

Does subduction of mass transport deposits (MTDs) control seismic behavior of shallow–level megathrusts at convergent margins?

Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts

Stress State in the Largest Displacement Area of the 2011 Tohoku-Oki Earthquake

Structure and lithology of the Japan Trench subduction plate boundary fault

Geology of the High Sillaro Valley (Northern Apennines of Italy)

Fluid history related to the early Eocene-middle Miocene convergent system of the Northern Apennines (Italy): Constraints from structural and isotopic studies

Deformation structures in the frontal prism near the Japan Trench: Insights from sandbox models

Internal structure and tectonic evolution of an underthrust tectonic mélange: the Sestola-Vidiciatico tectonic unit of the Northern Apennines, Italy

From soft sediment deformation to fluid assisted faulting in the shallow part of a subduction megathrust analogue: the Sestola Vidiciatico tectonic Unit (Northern Apennines, Italy)

Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments

Low Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature Measurements

Incrementally developed slickenfibers — Geological record of repeating low stress-drop seismic events?

Toward a dynamic concept of the subduction channel at erosive convergent margins with implications for interplate material transfer

Frictional properties of fault zone gouges from the J-FAST drilling project (M sub(w) 9.0 2011 Tohoku-Oki earthquake)

Chapter 3 Aseismic-Seismic Transition and Fluid Regime along Subduction Plate Boundaries and a Fossil Example from the Northern Apennines of Italy

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