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 22 março 2025
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
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
Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps - 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
Recycling of heterogeneous material in the subduction factory: evidence from the sedimentary mélange of the Internal Ligurian Units, 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
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
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
Field occurrence of the Epiligurian Succession (a-h) and
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
PDF) Structural Setting of Western Monferrato (Alps-Apennines Junction Zone, NW 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
PDF] Redefinition of the Ligurian Units at the Alps–Apennines junction (NW Italy) and their role in the evolution of the Ligurian accretionary wedge: constraints from mélanges and broken formations

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