Zoe Cumberpatch
YOU?
Author Swipe
View article: Flow‐process controls on grain type distribution in an experimental turbidity current deposit: Implications for detrital signal preservation and microplastic distribution in submarine fans
Flow‐process controls on grain type distribution in an experimental turbidity current deposit: Implications for detrital signal preservation and microplastic distribution in submarine fans Open
Deep‐water depositional systems are the ultimate sink for vast quantities of terrigenous sediment, organic carbon and anthropogenic pollutants, forming valuable archives of environmental change. Our understanding of the distribution of the…
View article: Halokinetic modulation of sedimentary thickness and architecture: A numerical modelling approach
Halokinetic modulation of sedimentary thickness and architecture: A numerical modelling approach Open
Subsurface salt flow can deform overlying strata and influence contemporaneous sedimentary systems. Studying salt‐sediment interactions is challenging in the subsurface due to poor imaging adjacent to salt, and in the field due to the diss…
View article: External signal preservation in halokinetic stratigraphy: A discrete element modeling approach
External signal preservation in halokinetic stratigraphy: A discrete element modeling approach Open
Subsurface salt movement in the absence of external tectonic forces can affect contemporaneous sediment deposition, mask allocyclic signals, and deform older strata. We used a discrete element model (DEM) to better understand salt-related …
View article: Halokinetic modulation of sedimentary thickness and architecture: a numerical modelling approach
Halokinetic modulation of sedimentary thickness and architecture: a numerical modelling approach Open
Subsurface salt flow can deform overlying strata and influence contemporaneous sedimentary processes. Studying salt-sediment interactions is challenging in the subsurface due to poor imaging adjacent to salt, and in the field due to the di…
View article: Supplemental Material: External signal preservation in halokinetic stratigraphy: A discrete element modeling approach
Supplemental Material: External signal preservation in halokinetic stratigraphy: A discrete element modeling approach Open
Modeled parameters and Figure S1.
View article: Supplemental Material: External signal preservation in halokinetic stratigraphy: A discrete element modeling approach
Supplemental Material: External signal preservation in halokinetic stratigraphy: A discrete element modeling approach Open
Modeled parameters and Figure S1.
View article: Interactions between deep-water gravity flows and active salt tectonics
Interactions between deep-water gravity flows and active salt tectonics Open
Behavior of sediment gravity flows can be influenced by seafloor topography associated with salt structures; this can modify the depositional architecture of deep-water sedimentary systems. Typically, salt-influenced deep-water successions…
View article: The Influence of Confining Topography Orientation on Experimental Turbidity Currents and Geological Implications
The Influence of Confining Topography Orientation on Experimental Turbidity Currents and Geological Implications Open
Turbidity currents distribute sediment across the seafloor, forming important archives of tectonic and climatic change on the Earth’s surface. Turbidity current deposition is affected by seafloor topography, therefore understanding the int…
View article: Evolution of a mixed siliciclastic‐carbonate deep‐marine system on an unstable margin: The Cretaceous of the Eastern Greater Caucasus, Azerbaijan
Evolution of a mixed siliciclastic‐carbonate deep‐marine system on an unstable margin: The Cretaceous of the Eastern Greater Caucasus, Azerbaijan Open
Mixed siliciclastic‐carbonate deep‐marine systems (mixed systems) are less documented in the geological record than pure siliciclastic systems. The similarities and differences between these systems are, therefore, poorly understood. A wel…
View article: Collapse processes in abandoned pillar and stall coal mines: Implications for shallow mine geothermal energy
Collapse processes in abandoned pillar and stall coal mines: Implications for shallow mine geothermal energy Open
Flooded mine workings represent potential aquifers for shallow geothermal development projects. However, determining the collapse state of such workings in advance of drilling, and predicting their hydrogeological properties can be challen…
View article: INTERACTIONS OF DEEP-WATER GRAVITY FLOWS AND ACTIVE SALT TECTONICS
INTERACTIONS OF DEEP-WATER GRAVITY FLOWS AND ACTIVE SALT TECTONICS Open
Sediment gravity flow behaviour is influenced by seafloor topography associated with salt structures, which controls the depositional architecture of deep-water sedimentary systems. Typically, salt-influenced deep-water successions are poo…
View article: A sedimentological approach for classifying sub-surface mine wastes: implications for shallow mine geothermal energy
A sedimentological approach for classifying sub-surface mine wastes: implications for shallow mine geothermal energy Open
Following sub-surface coal extraction, workings become flooded and represent a potential aquifer for shallow geothermal development projects. We investigate the internal structure of collapsed mine workings in surface exposures of pillar a…
View article: Halokinetic modulation of sedimentary systems: an integrated approach
Halokinetic modulation of sedimentary systems: an integrated approach Open
<p>Complicated structural-stratigraphic traps at the salt-sediment interface have historically hosted large hydrocarbon discoveries. Understanding sediment-routing around active salt bodies, is now vital for carbon capture and storag…
View article: Evolution of a mixed siliciclastic-carbonate deep-marine system on an unstable margin: the Cretaceous of the Eastern Greater Caucasus, Azerbaijan
Evolution of a mixed siliciclastic-carbonate deep-marine system on an unstable margin: the Cretaceous of the Eastern Greater Caucasus, Azerbaijan Open
Mixed siliciclastic-carbonate deep-marine systems (mixed systems) are less documented in the geological record than pure siliciclastic systems. The similarities and differences between these systems are therefore poorly understood. A well-…
View article: The stratigraphic evolution of onlap in siliciclastic deep-water systems: Autogenic modulation of allogenic signals
The stratigraphic evolution of onlap in siliciclastic deep-water systems: Autogenic modulation of allogenic signals Open
Seafloor topography affects the sediment gravity flows that interact with it. Understanding this interaction is critical for accurate predictions of sediment distribution and paleogeographic or structural reconstructions of deep-water basi…