RB
Member Since 2006
Rebecca E. Bell
Research Associate, Imperial College London
AGU Research
Search
Filters
Clear All
New Insights into CO2 Migration Behaviour from Time-Lapse Seismic Time Shifts at the Illinois Basin – Decatur Project
ACHIEVING NET ZERO EMISSIONS WITH GEOLOGIC CARBON STORAGE AND GEOTHERMAL ENERGY II ORAL
global environmental change | 15 december 2023
Idris Bukar, Rebecca E. Bell, Ann H. Muggeridge, S...
Geophysical monitoring of CO2 at storage sites is key to understanding its flow behaviour and improving predictive modelling of CO2 sequestration at f...
View Abstract
A New Seismicity Catalogue for the Northern Hikurangi Margin from a High-Density Seismic Network
SUBDUCTION TOP TO BOTTOM (ST2B): THE NATURE OF THE SUBDUCTION INTERFACE, EARTHQUAKES, AND THE ROLES OF FLUIDS I POSTER
tectonophysics | 14 december 2023
Amy Woodward, Ian D. Bastow, Rebecca E. Bell, Bill...
The Hikurangi subduction zone, where the Pacific Plate subducts beneath the Australian Plate, hosts a wide spectrum of slip modes, including earthquak...
View Abstract
Determining the Controls on Subduction Zone Seismic Behaviour with Machine Learning
INTEGRATING WIDE-OPEN DATASETS INTO MODELS OF THE SUBDUCTION ZONE EARTHQUAKE CYCLE TO IMPROVE SOCIETAL RESILIENCE I POSTER
tectonophysics | 13 december 2023
Valerie Locher, Rebecca E. Bell, Cedric M. John
Plate convergence at subduction plate boundaries is accommodated by a range of fault slip modes, including aseismic creep, slow slip events (SSE), and...
View Abstract
How Do Rift‐Related Fault Network Distributions Evolve? Quantitative Comparisons Between Natural Fault Observations and 3D Numerical Models of Continental Extension
TECTONICS
29 september 2023
Sophie Pan, John Naliboff, Rebecca E. Bell, Christ...
Continental extension is primarily accommodated by the evolution of normal fault networks. Rifts are shaped by complex tectonic processes and it ha...
Low Permeability Faults Inhibit Fluid Expulsion from the Northern Hikurangi Subduction Margin
MULTISCALE CRUSTAL DEFORMATION IN SUBDUCTION ZONES AND THE MEGATHRUST EARTHQUAKE CYCLE: PROGRESS FROM OBSERVATIONS AND MODELS III ORAL
tectonophysics | 16 december 2022
Shuoshuo Han, Nathan L. Bangs, Andrew Gase, Rebecc...
At subduction zones, sediment compaction and hydrous mineral dehydration generate a large amount of water that flows out of the accretionary wedge. Fa...
View Abstract
Fluids at slow slip megathrust zone supplied by consolidation of clay-rich, volcaniclastic subducting upper crust
MULTISCALE CRUSTAL DEFORMATION IN SUBDUCTION ZONES AND THE MEGATHRUST EARTHQUAKE CYCLE: PROGRESS FROM OBSERVATIONS AND MODELS II POSTER
tectonophysics | 14 december 2022
Andrew Gase, Nathan L. Bangs, Shuoshuo Han, Demian...
Hydrological and mechanical processes within subduction zones that ultimately control the nature of shallow (<15 km depth) megathrust slip are ofte...
View Abstract
Island Dolomitization in the Cretaceous Calcitic Ocean: A New Insight on the Role of Volcanism
CARBONATE SEDIMENTS THROUGH TIME: PROXIES FOR PROCESS AND PLANETS IV POSTER
paleoceanography and paleoclimatology | 13 december 2022
Mahmoud ElYamani, Cedric M. John, Rebecca E. Bell
Seawater dolomitization is a key process in ancient and modern settings. It requires permeable rocks, a fluid flow mechanism, and a sufficiently high ...
View Abstract
Broadband seismological analyses in the Eastern Mediterranean: implications for late-stage subduction, plateau uplift and the development of the North Anatolian Fault
CONTINENTAL COLLISIONS: STRUCTURE AND EVOLUTION II POSTER
tectonophysics | 13 december 2022
Ian D. Bastow, Christopher Steven Ogden, Thomas A....
The eastern Mediterranean hosts extensional, strike-slip, and collision tectonics above a set of fragmenting subducting slabs. Widespread Miocene-Rece...
View Abstract