Response of unconfined turbidity current to deep‐water fold and thrust belt topography: Orthogonal incidence on solitary and segmented folds-Reference-Cited by-同舟云学术

Response of unconfined turbidity current to deep‐water fold and thrust belt topography: Orthogonal incidence on solitary and segmented folds

Published:2019-05-30 Issue:6 Volume:66 Page:2425-2454
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Howlett Danielle M.¹^ORCID,Ge Zhiyuan¹^ORCID,Nemec Wojciech¹^ORCID,Gawthorpe Rob L.¹^ORCID,Rotevatn Atle¹^ORCID,Jackson Christopher A.‐L.²^ORCID

Affiliation:

1. Department of Earth Science University of Bergen Bergen 5007 Norway

2. Department of Earth Science and Engineering Imperial College London SW7 2BP UK

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12602

Reference134 articles.

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3. Forward modelling as a method for predicting the distribution of deep-marine sands: an example from the Peïra Cava Sub-basin

4. Three-dimensional numerical simulation of turbidity currents in a submarine channel on the seafloor of the Niger Delta slope

5. Observations on experimental, nonchannelized high‐concentration turbidity currents and variations in deposits around obstacles;Alexander J.;J. Sed. Res.,1994

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