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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Alps
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Western Alps
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Ligurian Alps (1)
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-
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Southern Europe
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Iberian Peninsula
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Spain
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Aragon Spain (1)
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-
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Italy
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Apennines (1)
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Liguria Italy
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Ligurian Alps (1)
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Western Europe
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France (1)
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Mediterranean Sea
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West Mediterranean (1)
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geologic age
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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Annot Sandstone (1)
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upper Eocene
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Priabonian (1)
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Paleocene (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Campanian (1)
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Maestrichtian (1)
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metamorphic rocks
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turbidite (4)
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Primary terms
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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Annot Sandstone (1)
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upper Eocene
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Priabonian (1)
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-
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Paleocene (1)
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data processing (1)
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deformation (1)
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ecology (1)
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Europe
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Alps
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Western Alps
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Ligurian Alps (1)
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-
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Southern Europe
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Iberian Peninsula
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Spain
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Aragon Spain (1)
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-
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Italy
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Apennines (1)
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Liguria Italy
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Ligurian Alps (1)
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-
-
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Western Europe
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France (1)
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-
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geophysical methods (1)
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Mediterranean Sea
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West Mediterranean (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Campanian (1)
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Maestrichtian (1)
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-
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ocean floors (2)
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sedimentary rocks
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clastic rocks
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sandstone (2)
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sedimentary structures
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planar bedding structures
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bedding (1)
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turbidity current structures (1)
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sedimentation (3)
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sediments
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clastic sediments (1)
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tectonics (1)
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sedimentary rocks
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flysch (1)
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sedimentary rocks
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clastic rocks
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sandstone (2)
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siliciclastics (1)
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turbidite (4)
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sedimentary structures
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channels (1)
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sedimentary structures
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planar bedding structures
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bedding (1)
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turbidity current structures (1)
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-
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sediments
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sediments
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clastic sediments (1)
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siliciclastics (1)
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turbidite (4)
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Hybrid event bed distribution in a mixed siliciclastic-calcareous turbidite succession: a cross-current perspective from the Bordighera Sandstone, Ligurian Alps, NW Italy
Syndepositional tectonics and mass-transport deposits control channelized, bathymetrically complex deep-water systems (Aínsa depocenter, Spain)
A consistent global approach for the morphometric characterization of subaqueous landslides
Abstract Landslides are common in aquatic settings worldwide, from lakes and coastal environments to the deep sea. Fast-moving, large-volume landslides can potentially trigger destructive tsunamis. Landslides damage and disrupt global communication links and other critical marine infrastructure. Landslide deposits act as foci for localized, but important, deep-seafloor biological communities. Under burial, landslide deposits play an important role in a successful petroleum system. While the broad importance of understanding subaqueous landslide processes is evident, a number of important scientific questions have yet to receive the needed attention. Collecting quantitative data is a critical step to addressing questions surrounding subaqueous landslides. Quantitative metrics of subaqueous landslides are routinely recorded, but which ones, and how they are defined, depends on the end-user focus. Differences in focus can inhibit communication of knowledge between communities, and complicate comparative analysis. This study outlines an approach specifically for consistent measurement of subaqueous landslide morphometrics to be used in the design of a broader, global open-source, peer-curated database. Examples from different settings illustrate how the approach can be applied, as well as the difficulties encountered when analysing different landslides and data types. Standardizing data collection for subaqueous landslides should result in more accurate geohazard predictions and resource estimation.