Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian accretionary wedge (NW Italy) and relationships with tectonics, global climate change and the dissociation of gas hydrates

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Last updated 25 outubro 2024
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
PDF] Structural anatomy of the Ligurian accretionary wedge (Monferrato, NW Italy), and evolution of superposed mélanges
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Tectono‐sedimentary evolution of the Tertiary Piedmont Basin (NW Italy) within the Oligo–Miocene central Mediterranean geodynamics - Maino - 2013 - Tectonics - Wiley Online Library
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Geosciences, Free Full-Text
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
PDF) Tectonic and climatic control on deposition of seep-carbonates: The case of middle-late miocene salsomaggiore ridge (Northern Apennines, Italy)
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Formation of ophiolite-bearing tectono-sedimentary mélanges in accretionary wedges by gravity driven submarine erosion: Insights from analogue models and case studies - ScienceDirect
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Basal shear zones of recurrent mass transport deposits serve as potential reservoirs for gas hydrates in the Central Canyon area, South China Sea - ScienceDirect
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
SE - Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian accretionary wedge (NW Italy) and relationships with tectonics, global climate change and the dissociation of gas hydrates
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Distribution of the large-scale mass-wasting complexes, m.w.c. (I to
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
PDF) Note illustrative della Carta Geologica d'Italia a scala 1:50.000. Foglio N. 219 “Sassuolo”
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Comparative Analysis of the Sedimentary Cover Units of the Jurassic Western Tethys Ophiolites in the Northern Apennines and Western Alps (Italy): Processes of the Formation of Mass-Transport and Chaotic Deposits during Seafloor
Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian  accretionary wedge (NW Italy) and relationships with tectonics, global  climate change and the dissociation of gas hydrates
Lithostratigraphy of the main External Ligurids: Ottone Unit

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