| human | Q5 |
| P6178 | Dimensions author ID | 01103731653.69 |
| P496 | ORCID iD | 0000-0001-6446-5577 |
| P1053 | ResearcherID | N-2683-2014 |
| P1153 | Scopus author ID | 56726827900 |
| P166 | award received | Roland Goldring Award | Q102320912 |
| P69 | educated at | Delft University of Technology | Q752663 |
| Utrecht University | Q221653 | ||
| HZ University of Applied Sciences | Q2518381 | ||
| P108 | employer | Utrecht University | Q221653 |
| Durham University | Q458393 | ||
| National Oceanography Centre | Q12812368 | ||
| P735 | given name | Matthieu | Q18091814 |
| Matthieu | Q18091814 | ||
| P106 | occupation | researcher | Q1650915 |
| Q58419793 | A General Model for the Helical Structure of Geophysical Flows in Channel Bends |
| Q102323344 | A comparative study of sediment waves and cyclic steps based on geometries, internal structures and numerical modeling |
| Q57978350 | A new model for turbidity current behavior based on integration of flow monitoring and precision coring in a submarine canyon |
| Q98891462 | Author Correction: Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution |
| Q102323081 | Character, spatial and temporal variation of turbidity currents on a source-to-sink scale |
| Q102323335 | Concentration-Dependent Flow Stratification In Experimental High-Density Turbidity Currents and Their Relevance To Turbidite Facies Models |
| Q97447570 | Cyclic steps along the South Taiwan Shoal and West Penghu submarine canyons on the northeastern continental slope of the South China Sea |
| Q64291547 | Daily bathymetric surveys document how stratigraphy is built and its extreme incompleteness in submarine channels |
| Q92365845 | Direct Monitoring Reveals Initiation of Turbidity Currents From Extremely Dilute River Plumes |
| Q102323061 | Direct evidence of a high-concentration basal layer in a submarine turbidity current |
| Q102323204 | Direct monitoring of active geohazards: emerging geophysical tools for deep-water assessments |
| Q102323100 | Evolution of a carbonate delta generated by gateway‐funnelling of episodic currents |
| Q102323228 | Flow Behaviour of a Giant Landslide and Debris Flow Entering Agadir Canyon, NW Africa |
| Q102323051 | Global monitoring data shows grain size controls turbidity current structure |
| Q57967651 | How to recognize crescentic bedforms formed by supercritical turbidity currents in the geologic record: Insights from active submarine channels |
| Q57866484 | Key Future Directions For Research On Turbidity Currents and Their Deposits |
| Q102323234 | Large-scale sediment waves and scours on the modern seafloor and their implications for the prevalence of supercritical flows |
| Q100252692 | Lessons learned from the monitoring of turbidity currents and guidance for future platform designs |
| Q101249162 | Linking Direct Measurements of Turbidity Currents to Submarine Canyon-Floor Deposits |
| Q102323166 | Linking submarine channel-levee facies and architecture to flow structure of turbidity currents: insights from flume tank experiments |
| Q61042163 | Long-term record of Barents Sea Ice Sheet advance to the shelf edge from a 140,000 year record |
| Q102323311 | MassFLOW-3DTMas a simulation tool for turbidity currents |
| Q102323173 | Morphodynamics and depositional signature of low-aggradation cyclic steps: New insights from a depth-resolved numerical model |
| Q102323318 | Morphodynamics and sedimentary structures of bedforms under supercritical-flow conditions: New insights from flume experiments |
| Q102323239 | Morphodynamics of Supercritical Turbidity Currents in the Channel-Lobe Transition Zone |
| Q36713184 | Morphodynamics of submarine channel inception revealed by new experimental approach |
| Q102322581 | Mud-clast armoring and its implications for turbidite systems |
| Q102323244 | Multiple Flow Slide Experiment in the Westerschelde Estuary, The Netherlands |
| Q114650509 | Near‐Bed Structure of Sediment Gravity Flows Measured by Motion‐Sensing “Boulder‐Like” Benthic Event Detectors (BEDs) in Monterey Canyon |
| Q90339926 | New flow relaxation mechanism explains scour fields at the end of submarine channels |
| Q41978248 | Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons. |
| Q61042160 | Origin of spectacular fields of submarine sediment waves around volcanic islands |
| Q57893979 | Physical theory for near-bed turbulent particle suspension capacity |
| Q57022723 | Powerful turbidity currents driven by dense basal layers |
| Q102323255 | Preconditioning and triggering of offshore slope failures and turbidity currents revealed by most detailed monitoring yet at a fjord-head delta |
| Q102323263 | Quantification of tsunami-induced flows on a Mediterranean carbonate ramp reveals catastrophic evolution |
| Q102322218 | Quantifying the three‐dimensional stratigraphic expression of cyclic steps by integrating seafloor and deep‐water outcrop observations |
| Q96609307 | Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution |
| Q102323328 | Recognition of cyclic steps in sandy and gravelly turbidite sequences, and consequences for the Bouma facies model |
| Q102323185 | Sediment Volume and Grain-Size Partitioning Between Submarine Channel−Levee Systems and Lobes: An Experimental Study |
| Q102323355 | Structureless, coarse-tail graded Bouma Ta formed by internal hydraulic jump of the turbidity current? |
| Q63645974 | Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream |
| Q102323107 | Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream |
| Q58082781 | Supercritical and subcritical turbidity currents and their deposits--A synthesis |
| Q58078878 | Supercritical-flow structures on a Late Carboniferous delta front: Sedimentologic and paleoclimatic significance |
| Q58079400 | Supercritical-flow structures on a Late Carboniferous delta front: sedimentologic and paleoclimatic significance: REPLY |
| Q102323135 | Supplementary material to "Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream" |
| Q59875942 | The influence of turbidity currents and contour currents on the distribution of deep-water sediment waves offshore eastern Canada |
| Q117737497 | Turbidity Currents Can Dictate Organic Carbon Fluxes Across River‐Fed Fjords: An Example From Bute Inlet (BC, Canada) |
| Q58419787 | Wave Ripple Development on Mixed Clay-Sand Substrates: Effects of Clay Winnowing and Armoring |
| Q73305912 | What controls submarine channel development and the morphology of deltas entering deep‐water fjords? |
| Q79155925 | What determines the downstream evolution of turbidity currents? |
| Q102323159 | Which Triggers Produce the Most Erosive, Frequent, and Longest Runout Turbidity Currents on Deltas? |
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