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Deep-water channel-lobe transition zone dynamics: Processes and depositional architecture, an example from the Karoo Basin, South Africa

Geological Society of America bulletin, 2018-09, Vol.130 (9-10), p.1723-1746

2018

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Origin, evolution and anatomy of silt-prone submarine external levées

Sedimentology, 2014-10, Vol.61 (6), p.1734-1763

2014

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Mud-Dominated Basin-Margin Progradation: Processes and Implications

Journal of sedimentary research, 2016-08, Vol.86 (8), p.863-878

2016

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Entangled external and internal controls on submarine fan evolution: an experimental perspective

The depositional record, 2020-09, Vol.6 (3), p.605-624

2020

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Sedimentologic and stratigraphic criteria to distinguish between basin‐floor and slope mudstones: Implications for the delivery of mud to deep‐water environments

The depositional record, 2022-06, Vol.8 (2), p.958-988

2022

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Driving a channel through a levee when the levee is high: An outcrop example of submarine down-dip entrenchment

Marine and petroleum geology, 2013-03, Vol.41, p.134-145

2013

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Time-Transgressive Confinement On the Slope and the Progradation of Basin-Floor Fans: Implications For the Sequence Stratigraphy of Deep-Water Deposits

Journal of sedimentary research, 2016-02, Vol.86 (2), p.73-86

2016

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U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

International geology review, 2015-03, Vol.57 (4), p.393-410

2015

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Exhumed lateral margins and increasing flow confinement of a submarine landslide complex

Sedimentology, 2018-06, Vol.65 (4), p.1067-1096

2018

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Integrating outcrop and subsurface data to assess the temporal evolution of a submarine channel–levee system

AAPG bulletin, 2016-11, Vol.100 (11), p.1663-1691

2016

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Palaeovalleys in foreland ramp settings: what happens as accommodation decreases down dip?

Basin research, 2017-12, Vol.29 (6), p.747-774

2017

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Spatial and Temporal Evolution of a Permian Submarine Slope Channel-Levee System, Karoo Basin, South Africa

Journal of sedimentary research, 2011-08, Vol.81 (8), p.579-599

2011

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Confined to unconfined: Anatomy of a base of slope succession, Karoo Basin, South Africa

Marine and petroleum geology, 2013-03, Vol.41, p.206-221

2013

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Clinoform architecture and along‐strike facies variability through an exhumed erosional to accretionary basin margin transition

Basin research, 2019-10, Vol.31 (5), p.920-947

2019

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Sedimentology, Stratigraphic Architecture, and Depositional Context of Submarine Frontal-Lobe Complexes

Journal of sedimentary research, 2014-09, Vol.84 (9), p.763-780

2014

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Heterogeneity of fill within an incised channel: The Oligocene Grès du Champsaur, SE France

Marine and petroleum geology, 2007-06, Vol.24 (6), p.529-539

2007

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Experimental Modeling of the Spatial Distribution of Grain Size Developed in a Fill-and-Spill Mini-Basin Setting

Journal of sedimentary research, 2004-05, Vol.74 (3), p.438-446

2004

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Disentangling tectonic and eustatic controls on forearc basin stratigraphy, Talara Basin, Peru

Sedimentary geology, 2022-12, Vol.442, p.106277, Article 106277

2022

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Evolution and architecture of an exhumed ocean‐facing coarse‐grained submarine canyon fill, Baja California, Mexico

Sedimentology, 2024-10

2024

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Anatomy of a mixed-influence shelf edge delta, Karoo Basin, South Africa

Geological Society special publication, 2017, Vol.444 (1), p.393-418

2017

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Disconnected submarine lobes as a record of stepped slope evolution over multiple sea-level cycles

Geosphere (Boulder, Colo.), 2018-08, Vol.14 (4), p.1753-1779

2018

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Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2500 km2 area

Geosphere (Boulder, Colo.), 2014-12, Vol.10 (6), p.1076-1093

2014

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Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2500 km super(2) area

Geosphere (Boulder, Colo.), 2014-12, Vol.10 (6), p.1076-1093

2014

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Deep-water channel-lobe transition zone dynamics: Processes and depositional architecture, an example from the Karoo Basin, South Africa

Origin, evolution and anatomy of silt-prone submarine external levées

Mud-Dominated Basin-Margin Progradation: Processes and Implications

Entangled external and internal controls on submarine fan evolution: an experimental perspective

Sedimentologic and stratigraphic criteria to distinguish between basin‐floor and slope mudstones: Implications for the delivery of mud to deep‐water environments

Driving a channel through a levee when the levee is high: An outcrop example of submarine down-dip entrenchment

Time-Transgressive Confinement On the Slope and the Progradation of Basin-Floor Fans: Implications For the Sequence Stratigraphy of Deep-Water Deposits

U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

Exhumed lateral margins and increasing flow confinement of a submarine landslide complex

Integrating outcrop and subsurface data to assess the temporal evolution of a submarine channel–levee system

Palaeovalleys in foreland ramp settings: what happens as accommodation decreases down dip?

Spatial and Temporal Evolution of a Permian Submarine Slope Channel-Levee System, Karoo Basin, South Africa

Confined to unconfined: Anatomy of a base of slope succession, Karoo Basin, South Africa

Clinoform architecture and along‐strike facies variability through an exhumed erosional to accretionary basin margin transition

Sedimentology, Stratigraphic Architecture, and Depositional Context of Submarine Frontal-Lobe Complexes

Heterogeneity of fill within an incised channel: The Oligocene Grès du Champsaur, SE France

Experimental Modeling of the Spatial Distribution of Grain Size Developed in a Fill-and-Spill Mini-Basin Setting

Disentangling tectonic and eustatic controls on forearc basin stratigraphy, Talara Basin, Peru

Evolution and architecture of an exhumed ocean‐facing coarse‐grained submarine canyon fill, Baja California, Mexico

Anatomy of a mixed-influence shelf edge delta, Karoo Basin, South Africa

Disconnected submarine lobes as a record of stepped slope evolution over multiple sea-level cycles

Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2500 km2 area

Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2500 km super(2) area

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