What controls the remobilization and deformation of surficial sediment by seismic shaking? Linking lacustrine slope stratigraphy to great earthquakes in South

What controls the remobilization and deformation of surficial sediment by seismic shaking? Linking lacustrine slope stratigraphy to great earthquakes in South–Central Chile

Published:2021-05-06 Issue:6 Volume:68 Page:2365-2396
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Molenaar Ariana¹^ORCID,Van Daele Maarten²^ORCID,Vandorpe Thomas³^ORCID,Degenhart Gerald¹⁴^ORCID,De Batist Marc²^ORCID,Urrutia Roberto⁵^ORCID,Pino Mario⁶^ORCID,Strasser Michael¹^ORCID,Moernaut Jasper¹^ORCID

Affiliation:

1. Institute of Geology University of Innsbruck Innrain 52, 6020 Innsbruck Austria

2. Renard Centre of Marine Geology Ghent University Sint‐Pietersnieuwstraat 33, 9000 Ghent Belgium

3. Flanders Marine Institute (VLIZ) Wandelaarkaai 7, 8400 Oostende Belgium

4. Department of Radiology Core facility Micro CT Medical University of Innsbruck Christoph‐Probst‐Platz 1, Innrain 52 A, 6020 Innsbruck Austria

5. Faculty of Environmental Sciences EULA‐Center University of Concepción Barrio Universitario s/n Concepción Chile

6. Inst. Ciencias de la Tierra Transdisciplinary Center for Quaternary Research in the South of Chile Universidad Austral de Chile Valdivia Chile

Funder

Austrian Science Fund

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12856

Reference90 articles.

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3. A large-scale radial pattern of seismogenic slumping towards the Dead Sea Basin

4. Seismogenic slump folds formed by gravity-driven tectonics down a negligible subaqueous slope

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