RB
Member Since 2006
Rebecca E. Bell
Research Associate, Imperial College London
AGU Research
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Using 4D time shift analysis to unlock the interpretation of CO2 plume dynamics in consolidated heterogenous onshore reservoirs
AGU 2024
seismology | 13 december 2024
Idris Bukar, Rebecca E. Bell, Ann H. Muggeridge, S...
Time-lapse seismic methods are the main geophysical techniques used to monitor sequestered CO2 plumes. Time-lapse seismic analysis is often performed ...
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Local Earthquake Analysis at the Northern Hikurangi Margin in a Region of Repeating Slow Slip Events
AGU 2024
seismology | 11 december 2024
Amy Woodward, Ian D. Bastow, Rebecca E. Bell, Laur...
The northern Hikurangi margin experiences slow slip events every 6-24 months, and is an ideal natural laboratory in which to observe this phenomenon d...
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An Integrated Study of Age and Formation of the Aru Trough, Eastern Banda Arc, Indonesia: Implications for Seismic Hazards
TECTONICS
21 september 2024
Zhiwen Zhang, Rebecca E. Bell, Jian Lin, Walter D....
The Banda Arc in eastern Indonesia has a complex tectonic history involving oceanic and continental subduction, arc‐continent collision and s...
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...
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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...
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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...
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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...
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