An integrated process‐based model of flutes and tool marks in deep‐water environments: Implications for palaeohydraulics, the Bouma sequence and hybrid event beds

Author:

Peakall Jeff1ORCID,Best Jim2ORCID,Baas Jaco H.3,Hodgson David M.1ORCID,Clare Michael A.4ORCID,Talling Peter J.5,Dorrell Robert M.6ORCID,Lee David R.1ORCID

Affiliation:

1. School of Earth and Environment University of Leeds Leeds LS2 9JT UK

2. Departments of Geology, Geography and GIS Mechanical Science and Engineering Ven Te Chow Hydrosystems Laboratory University of Illinois at Urbana‐Champaign Urbana IL 61801 USA

3. School of Ocean Sciences Bangor University Bangor, Menai Bridge Wales LL59 5AB UK

4. National Oceanography Centre European Way Southampton SO14 3ZH UK

5. Departments of Earth Sciences and Geography University of Durham Durham DH1 3LE UK

6. Energy and Environment Institute University of Hull Hull HU6 7RX UK

Funder

Natural Environment Research Council

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference359 articles.

1. Flute Marks and Flute Separation

2. Erosional current marks of weakly cohesive beds;Allen J.R.L.;J. Sed. Petrol.,1969

3. Transverse erosional marks of mud and rock: their physical basis and geological significance

4. Mixing at turbidity current heads, and its geological implications;Allen J.R.L.;J. Sed. Petrol.,1971

5. Development of flute-mark assemblages, 1. Evolution of pairs of defects

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