Diagnostic features and field-criteria in recognition of tectonic, sedimentary and diapiric mélanges in orogenic belts and exhumed subduction-accretion complexes
Multiple episodes of deformation during the tectonic evolution of orogenic belts and ancient
subduction-accretion complexes cause obfuscation of primary block-in-matrix fabric of …
subduction-accretion complexes cause obfuscation of primary block-in-matrix fabric of …
How sediments become mobilized
AJ Maltman, A Bolton - Geological Society, London, Special …, 2003 - lyellcollection.org
Geological sediments tend to strengthen during progressive burial but the interplay of
porosity and permeability, strain and effective stress gives rise to numerous circumstances in …
porosity and permeability, strain and effective stress gives rise to numerous circumstances in …
Structure and composition of the plate-boundary slip zone for the 2011 Tohoku-Oki earthquake
The mechanics of great subduction earthquakes are influenced by the frictional properties,
structure, and composition of the plate-boundary fault. We present observations of the …
structure, and composition of the plate-boundary fault. We present observations of the …
Mélanges and mélange-forming processes: a historical overview and new concepts
Mélanges represent a significant component of collisional and accretionary orogenic belts
and occur widely around the world. Since its first introduction and use, the term has evolved …
and occur widely around the world. Since its first introduction and use, the term has evolved …
Turbidites and turbidity currents from Alpine 'flysch'to the exploration of continental margins
E Mutti, D Bernoulli, FR Lucchi, R Tinterri - Sedimentology, 2009 - Wiley Online Library
The concept of turbidite has evolved so much since its original definition by Kuenen and
Migliorini in 1950–ie the deposit of turbidity currents exemplified by the sandy flysch …
Migliorini in 1950–ie the deposit of turbidity currents exemplified by the sandy flysch …
Shear zones in clay-rich fault gouge: A laboratory study of fabric development and evolution
Clay-rich fault rocks have long been recognized to host distinctive fabric elements, and fault
rock fabric is increasingly thought to play a fundamental role in fault mechanical behaviour …
rock fabric is increasingly thought to play a fundamental role in fault mechanical behaviour …
Deformation responses of slow moving landslides to seasonal rainfall in the Northern Apennines, measured by InSAR
Slow moving landslides are widespread geomorphological features in the Northern
Apennines of Italy where they represent one of the main landscape forming processes. The …
Apennines of Italy where they represent one of the main landscape forming processes. The …
Architecture and permeability structure of the Sibillini Mts. Thrust and influence upon recent, extension-related seismicity in the central Apennines (Italy) through fault …
The central Apennines are a fold-thrust belt currently affected by post-orogenic extensional
seismicity. To constrain the influence that the inherited thrust-related structures exert on the …
seismicity. To constrain the influence that the inherited thrust-related structures exert on the …
Review of major shale-dominated detachment and thrust characteristics in the diagenetic zone: Part I, meso-and macro-scopic scale
There is considerable variability in the thickness, structure, and macroscopic deformation
style within shale-prone major thrust zones, which also impacts the structural style in the …
style within shale-prone major thrust zones, which also impacts the structural style in the …
Can fault leakage occur before or without reactivation? Results from an in situ fault reactivation experiment at Mont Terri
We conducted fluid injection tests in four packed-off borehole intervals across the Mont Terri
clay-rich fault zone which is an analogue to a minor fault that would hardly be detectable …
clay-rich fault zone which is an analogue to a minor fault that would hardly be detectable …