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
Descrição
PDF) A tectonically-induced Eocene sedimentary mélange in the West Ligurian Alps, Italy
Recycling of heterogeneous material in the subduction factory: evidence from the sedimentary mélange of the Internal Ligurian Units, Italy
PDF] Structural anatomy of the Ligurian accretionary wedge (Monferrato, NW Italy), and evolution of superposed mélanges
Contatto stratigrafico fra il till di alloggiamento della conca del
Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts - ScienceDirect
a Chirp (2-7 kHz) profile showing the acoustic characters of the
Distribution of the large-scale mass-wasting complexes, m.w.c. (I to
Flaking of concretion matrix during formation of lenticular shrinkage
Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps - ScienceDirect
Basal shear zones of recurrent mass transport deposits serve as potential reservoirs for gas hydrates in the Central Canyon area, South China Sea - ScienceDirect
Recycling of heterogeneous material in the subduction factory: evidence from the sedimentary mélange of the Internal Ligurian Units, Italy