Channel‐lobe transition zone development in tectonically active settings: Implications for hybrid bed development
Author:
Affiliation:
1. EMR – Geological Institute RWTH Aachen University Aachen Germany
2. Department of Earth Sciences Chiba University Chiba Japan
3. School of Earth and Environment University of Leeds Leeds UK
Funder
Japan Society for the Promotion of Science London
Publisher
Wiley
Subject
Paleontology,Stratigraphy,Geology,Environmental Science (miscellaneous),Oceanography
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/dep2.180
Reference178 articles.
1. Gravel overpassing on humpback bars supplied with mixed sediment: examples from the Lower Old Red Sandstone, southern Britain
2. The influence of bend amplitude and planform morphology on flow and sedimentation in submarine channels
3. Anatomy of turbidites and linked debrites based on long distance (120 x 30 km) bed correlation, Marnoso Arenacea Formation, Northern Apennines, Italy
4. Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud-sand) sediment flows
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