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

Por um escritor misterioso
Last updated 26 dezembro 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
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
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
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
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) A tectonically-induced Eocene sedimentary mélange in the West Ligurian Alps, 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
Photographs of outcrops within the out-of-sequence thrust (OOST) zone
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
a) Diagrams showing mesoscale data (Schmidt net, lower hemisphere) of
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
Ages of Antola Unit (Cabella Ligure, Bargagli and Genova areas) 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
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
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
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
Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts - ScienceDirect

© 2014-2024 jeart-turkiye.com. All rights reserved.