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 setembro 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
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
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
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
X-radiographs a – c and photographs d , e of sedimentary facies from
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
Polygenetic mélanges: a glimpse on tectonic, sedimentary and diapiric recycling in convergent margins
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
a) Stratigraphic range of selected taxa from the Late Cretaceous
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
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
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
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
Regional structural sketch map (a) of the northwestern part of Northern

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