University of Calgary, Department of Geoscience

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    I[University of Calgary, Department of Geoscience]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (242)"]
    CA["Linked Collaborating Authors (0)"]
    I== skos:broader ==>PI
    CI== skos:broader ==>I
    AW== affil ==>I
    AW== author ==>CA
    click PI "#parent-institutions"
    click CI "#child-institutions"
    click AW "#affiliated-works"
    click CA "#collaborating-authors"

ADS ID [?]

A00315

Abbreviation [?]

Dep Geos

Parent Institutions [?]

• University of Calgary, Canada

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• Thickened Ocean Crust or Basal Island Arc Origin for the Pitka Mafic-Ultramafic Complex, Northern Alaska
• Comparison of Three Geophysical Methods for Characterizing a Gravel Aquifer
• Contributions of surface measurements and GRACE data to the study of the secular geoid change in North America
• Effects of Lateral Heterogeneity and Power Law Rheology on Glacially Induced Surface Motion and Gravity Rate of Change
• Exhumation of the Magallanes foreland basin, Patagonian Andes, Chile (51 °S): Preliminary results from apatite (U-Th)/He dating
• GRACE Observed Glacial Isostatic Adjustment in Laurentia
• Improvement and Test of the Simplex Optimum Method for Seismic Location
• Optimization of Discrete Spherical Harmonic Transforms and Applications
• Pc3 Excitation of the Ionosphere: a Preliminary Analysis
• Shallow Low-Viscosity Zones in Flat-3D Finite-Element Models of Glacial-Isostatic Adjustment
• Spontaneous Growth and Mobilization of a Gas Phase in the Presence of Dense Non- Aqueous Phase Liquid (DNAPL)
• Identification of groundwater contamination sources of nitrate and sulfate in shallow alluvial aquifers using a dual-isotope approach in an agricultural area
• Laurentia Glacial Isostatic Adjustment Observed From GRACE and Satellite Altimetry
• New stratigraphic constraints on Holocene glacier advances at Mt. Baker, Washington
• Time-Lapse Electrical Resistivity Monitoring of the Remediation of a Saline Groundwater Plume
• Discontinuity Structure Beneath the North American Craton and the Signature of Continental Roots
• Field Mapping of Geologic Structures Bounding Little Lake Valley Correlate With Multiple Seismogenic Clusters Within the Maacama Fault Zone, Northern California
• Glacial Isostatic Adjustment in Laurentia and Fennoscandia Observed by TOPEX/POSEIDON Radar Altimetry Over Land
• HuBLE-UK, the Hudson Bay Lithospheric Experiment: Insights into the formation of the Canadian Shield
• Insights into the Deep Biosphere from Petroleum Geology
• Isotopic Approaches to Evaluate the Fate of Injected CO2 in Two Geological Storage Projects in Mature Oilfields in Canada
• Monitoring the Remediation of Salt-Affected Soils and Groundwater
• Rational Experimental Design for Electrical Resistivity Imaging
• Seismic Wave Velocity in Earth's Shallow Core
• Shallow-Earth Thermomechanical Models of NW-Europe From GIA Constrained by GOCE Gravity Data
• Structure of the Crust and Uppermost Mantle Beneath Hudson Bay Based on Ambient- Noise Tomography
• Suboxic conditions at the Permian-Triassic boundary in the NE Panthalassic Ocean suggest a different extinction mechanism compared to Paleotethys anoxia
• Temperature dependence of electrical resistivity measurements: A useful infiltration tracer?
• Why heavy oilfields exist? The dynamic interplay of oil charge, basin dynamics, caprock leakage and gas generating biodegradation that produces heavy oilfields
• (Accelerated) mass changes in the Siberian permafrost regions from GRACE
• An example of complex fault geometries in a young, rapidly deforming transform fault system: The Maacama Fault in northern California
• Biot Theory Frequency Dependent Seismic Attributes
• Canadian Advanced Nanospace eXperiment 2 Orbit Operations: Over a Year of Pushing the Nanosatellite Performance Envelope
• Crustal Anisotropy of Hudson Bay from Ambient-Noise Tomography
• Education and Public Outreach at The Pavilion Lake Research Project: Fusion of Science and Education using Web 2.0
• Effect of hydrocarbon contamination on laboratory measurements of the streaming potential coupling coefficient
• Geophysical Imaging of Discontinuous Permafrost: Effects of Sub-grid Landcover Variability and Linear Disturbance
• Gravimetric Investigations in the Tien Shan and in the seismically active region of Almaty (Kazakhstan)
• High-resolution 3-D seismic reflection imaging of late Quaternary deformation in the shallow Alpine Fault Zone, New Zealand
• HuBLE-UK, the Hudson Bay Lithospheric Experiment: Insights into the Formation of the Canadian Shield From Seismic Tomography and Shear-Wave Splitting
• Initial results from continuous GPS stations at Hudson Bay
• Integration of Geologic and Geophysical Data to Model Hydrostratigraphy Under a Recharge Pond for Aquifer Storage and Recovery
• Lithospheric architecture of the Hudson Bay region (Invited)
• Monitoring groundwater storage in an alpine watershed in the Canadian Rockies using microgravity measurements
• Numerical Modeling of Unconsolidated Sediments to Explore Relationships Between Electrical Conductivity and Hydrogeologic Parameters at the Pore-Scale
• Optimal locations of GPS measurements in Laurentide and Fennoscandia for constraining 3D GIA models
• Precambrian Crustal Evolution of the Hudson Bay Region: Insights from Receiver Function Analysis (Invited)
• Skeleton-migration: Applications in deep crustal reflection seismic profiling
• Source identification of nitrate in groundwater using stable isotopes and Cl/Br ratios in an agricultural area
• The LITHOPROBE trans-continental lithospheric cross-sections: Imaging the internal structure of the North American continent
• The viscosity structure of Northern Europe inferred from GRACE data
• Variations in Lithospheric Structure Across Northern Hudson Bay From Rayleigh Wave Array Tomography
• A Distribution-Based Parameterization for Difference Tomographic Imaging of Solute Plumes
• A Geoelectrically-Monitored Tracer Test At The Macrodispersion Experiment (MADE) Site In Columbus, Mississippi
• Accretion, modification and erosion of Archean lithosphere: evidence from the Superior Province and adjacent regions (Invited)
• Degassing of groundwater with elevated dissolved methane from monitoring wells in Alberta, Canada
• Did the November 17, 2009 Queen Charlotte Island (QCI) earthquake fill a predicted seismic gap?
• Effects of water-energy feedback processes on thawing of peat-covered, discontinuous permafrost
• Electrical Resistivity Imaging for Studying Dynamics of Vadose Zone Processes
• Estimation of the Anelastic Parameters of Subsurface Structures From Their Seismic AVF and AVA Signatures
• GIA simulation with plastic and visco-plastic ice models on a laterally heterogeneous 3D Earth model for Scandinavia
• Isopycnicity, Thermal State and Secular Evolution of Cratonic Mantle Keels
• Long-Term Monitoring of Infiltration at a Managed Aquifer Recharge Site Using Electrical Resistivity Probes
• Mantle transition zone structure beneath the Canadian Shield
• Mapping degrading organic contaminant plumes with spontaneous potential: Why does it not always work?
• Mastering the Concepts of Geologic Time: Novice Students' Understanding of the Principles of Relative Age
• Modes of continental decretion in western Canada
• Multitracer Study of Flow to Tile Drains in Irrigated Macroporous Soil
• Precambrian Plate Tectonics and the Formation of the Canadian Shield: Seismic Evidence from Hudson Bay
• Shear Wave Velocity Structure and Azimuthal Anisotropy of Hudson Bay
• Storage and transmission of groundwater in alpine moraine and talus deposits (Invited)
• The Utility of Proximal-Accretion Stratigraphy in Lateral Moraines
• A tale of two solutes: Dual-domain flow and the role of the mass transfer coefficient
• Aerial LiDAR Based Analysis of a Degraded Fault Scarp in Stewart Valley, Nevada
• CO<SUB>2</SUB> Emissions Generated by a Fall AGU Meeting
• Comparison of shallow aquifer and soil gas monitoring approaches for detecting CO2 leakage at a natural analogue site in France
• Deformation, deposition, and surface uplift in the hinterland of the Central Andes, Bolivia
• Detrital thermochronology and sedimentology of the Sabine Bay and Assistance formations, Ellesmere Island: insights into the source of the Melvilian Disturbance event
• Development of the aftershock process of the 2010 Val-des-Bois (Quebec) Mw 5.0 Earthquake
• Enigmatic Post-Glacial Degradation and Aggradation of Rivers on the Alberta Plains
• Evaluation of the GOCE-Based Global Gravity Field Models in Iran
• IONOTOMO: A new approach for ionospheric tomography using OTH radar
• Latest Pleistocene and Holocene Glacier Fluctuations in southernmost Patagonia
• On the Extraction of Seismic AVF Information and the Inversion of Anelastic Reflectivity
• Post-glacial induced stress changes in central Europe - large enough to trigger earthquakes?
• Probabilistic Seismic Hazard Analysis: Adaptation for CO2 Sequestration Sites
• Runoff from wetland-dominated terrains with thawing permafrost
• SimLAB: Evaluating Geophysical Proxies for the Lithosphere-Asthenosphere Boundary
• Stress directions from Earthquakes in Northeast Canada Compared to Stress from Postglacial Rebound Models
• Structural Complexities Influencing Biostratigraphic Interpretations of the Permian Nansen Formation type-section, Ellesmere Island, Canada
• The Arctic Eurekan Orogen : A plate tectonic conundrum
• The Influence of Non-linear 3-D Mantle Rheology on Predictions of Glacial Isostatic Adjustment Models
• The Place of Rock and Mineral Identification in Geoscience Programs
• The Thermo-Tectonic Evolution of Hoodoo Dome, Ellef Ringnes Island: Implications for Petroleum Exploration in the Sverdrup Basin
• Time-Lapse Monitoring Through Direct, Scattering-Based Inversion of Seismic Difference Data
• U-Pb and <SUP>40</SUP>Ar/<SUP>39</SUP>Ar isotopic evidence for coeval Neogene pluton emplacement and fault-induced exhumation in the Cordillera Blanca, Peru
• Validation of numerical viscous seismic modeling
• Very nearly UHP metamorphism-lawsonite and epidote eclogites from western Canada
• A graph theoretic approach to global earthquake sequencing: A Markov chain model
• Application of Spatial Continuous Wavelet Transforms to Identify Noise in Regional Airborne Electromagnetic Data
• Are Late-Pleistocene Climate Reconstructions from Cirque and Valley Moraines Possible in Regions of Decaying Ice Sheets?
• Assessment of Bathymetry and Sediment Accumulation of Walker Lake, PA with Multiple Frequency GPR Antennas
• Detection and Evaluation of Episodic Tremor and Slip on Vancouver Island with a Superconducting Gravimeter
• Determining Carbon and Oxygen Stable Isotope Systematics in Brines at Elevated p/T Conditions to Enhance Monitoring of CO2 Induced Processes in Carbon Storage Reservoirs
• Equilibrium and kinetics in metamorphism
• GIA Modeling with 3D Rheology and Recent Ice Thickness Changes in Polar Regions
• Geophysics for improved groundwater management - a demonstration of the value added.
• Geothermobarometry of Spinel Peridotites from Southern British Columbia: Implications for the Thermal Conditions in the Upper Mantle
• Impact of Siberian Trap eruptions on Latest Permian Oceans
• Parameter coupling in seismic reflection amplitudes and the importance of the number V<SUB>P</SUB>/V<SUB>S</SUB>=2
• Patagonian Glacier Advances in Concert with those in Western North America
• Stable carbon isotope ratios as proxies for CO2 migration: An experimental approach with analogue fluids
• Stratification of Seismic Anisotropy Beneath Hudson Bay
• Stratigraphy and Geochemistry of the Lower Permian Esayoo Volcanics, Northwest Ellesmere Island: Insights into Sverdrup Basin Paleogeography
• Structure and Deformation on NW Ellesmere Island, Arctic Canada, and Implications for Regional Tectonics
• The Satah Mountain and Baldface Mountain Volcanic Fields, Chilcotin Highland, West-Central British Columbia
• A combined experimental and numerical study of pore water pressure variations in sub-permafrost groundwater
• Approximating snow surface temperature from standard temperature and humidity data: new possibilities for snow model and remote sensing validation (Invited)
• Distribution of Total Dissolved Solids in McMurray Formation Water in the Athabasca Oil Sands Region, Alberta, Canada: Implications for Oil Sands Mining and In Situ Resource Development
• Fault activation due to glacially induced stresses
• Impacts of Siberian Trap Eruption on NW Pangea during the Latest Permian Extinction (Invited)
• Importance of Stratabound Fracture Networks for Seismic Hazard Assessment of Hydraulic Fracturing
• Insight into earthquake sequencing: Analysis and interpretation of time-series constructed from the directed graph of the Markov chain model
• Instantaneous Frequency Attribute Comparison
• Late Quaternary climatic influences on river geomorphology on the Alberta Plains, Canada
• Lithospheric structure at the leading edge of the North American craton: Imaging the Shield-Cordillera transition in western Canada by teleseismic Rayleigh-wave analysis
• Permafrost response to climate change: Linking field observation with numerical simulation
• Regional-scale Hydrostratigraphic Analysis of the Paskapoo Aquifer Using Normalized Gamma-ray Logs
• Thermal evolution of cratonic mantle keels: implications for buoyancy and rheology of continental lithosphere (Invited)
• Clumped isotope paleothermometry of eggshells as an indicator of vertebrate endothermy
• Imaging the Lithosphere-Asthenosphere Boundary Using Iterative Method of Receiver Function Analysis: A Synthetic Seismogram Approach
• Multi-phase submarine channel-fill history recorded by stratigraphic architectures in outcropping slope-channel deposits, Tres Pasos Formation, southern Chile
• Oligo-Miocene Alpine Sediment Routing from Integrated Analysis of Seismic-Reflection Data and Detrital Zircon U-Pb Geochronology
• Seismic characteristics of tensile fracture growth induced by hydraulic fracturing
• The Stratigraphic Expression of Formative Processes in Channels
• Facies Analysis and b-Value for Operationally Induced Microseismicity
• High-Resolution Chronostratigraphic Correlation and Sedimentation Rate Calculations With Maximum Depositional Ages Derived From Large-n Detrital Zircon Datasets
• Hydrologic Storage Functions of an Alpine Talus: Linking Field Observations with Numerical Simulations
• Influence of Diffuse and Discrete Groundwater Discharge on River Thermal Regimes in Present and Future Climates
• On the Importance of the Earthquake-Earthquake Triggering in Microseismicity Induced by Hydraulic Fracturing
• Quantifying Similarity in Seismic Polarizations
• Statistical Analysis of Seismicity Associated with Hydraulic Fracturing in Western Canada
• The Implications of Detrital Zircon Maximum Depositional Age (MDA) from Large Sample Datasets (&lt;em&gt;n&lt;/em&gt;&gt;500)
• The Relationship Between Seismicity and the Oil and Gas Industry in Western Alberta and Eastern B.C.
• Traffic Light Protocol for Induced Seismicity: What is the Best Strategy?
• "The Bridge" from Earthscope to EarthsCAN to Maintain North American Geoscience Momentum
• At the craton edge: Geodynamic evolution of the southern Canadian Cordillera
• Conditioning geostatistical simulations of a heterogeneous paleo-fluvial bedrock aquifer using lithologs and pumping tests
• Controlled source electromagnetic data analysis with seismic constraints and rigorous uncertainty estimation in the Black Sea
• High Resolution Stratigraphic Mapping in Complex Terrain: A Comparison of Traditional Remote Sensing Techniques with Unmanned Aerial Vehicle - Structure from Motion Photogrammetry
• Investigating the Subsurface Stress Field based on Hybrid Earthquake Focal Mechanisms: Examples from the Fort Worth Basin, Texas
• Non-trivial Clustering and Inter-Event Triggering in Microseismicity Induced by Hydraulic Fracturing
• The linkage between fluvial meander-belt morphodynamics and the depositional record improves paleoenvironmental interpretations, Western Interior Basin, Alberta, Canada
• Uncertainty quantification of seabed parameters for large data volumes along survey tracks with a tempered particle filter
• Using spectral attributes to characterize the source mechanisms of microseismic events
• Using stable isotopes to determine sources and pathways of groundwater recharge in the Canadian Prairies
• Advancing Knowledge on Fugitive Natural Gas from Energy Resource Development at a Controlled Release Field Observatory
• Conceptual models of microseismicity induced by fluid injection
• Crustal layering and gravity highs in the Midcontinent of North America - implications for the formation of the Illinois Basin
• Development of Virtual Field Experiences for undergraduate geoscience using 3D models from aerial drone imagery and other data
• First direct observations linking confined supercritical turbidity currents to their depositional architecture and facies characteristics
• Hydraulic Fracturing Completion Volume is Associated with Induced Earthquake Productivity in the Duvernay Play
• Microseismic data records fault activation before and after a M<SUB>w</SUB> 4.1 induced earthquake
• New insights on regional tectonics and crustal composition of the eastern Sierras Pampeanas in the Andean back arc region, Argentina (31-32ºS)
• Quantifying Water-Rock Interactions during Hydraulic Fracturing from the Analysis of Flowback Water
• Simulation of variation of apparent resistivity in resistivity surveys using finite difference modelling with Monte Carlo analysis
• The Stratigraphic Incompleteness of Submarine Channels
• Uncertainty Quantification in Earthquake Source Characterization with Probabilistic Centroid Moment Tensor Inversion
• A Reconnaissance Petrographic Study of Opaque Mineral Assemblages in Peridotites and Mafic Dykes from the Oman Drilling Project Holes BA1B, BA3A and BA4A
• A parsimonious Bayesian cut-and-paste algorithm for centroid moment tensor inversion
• A physics-based probabilistic approach to estimate pressure necessary to trigger seismicity from saltwater disposal
• Annual streamflow in a Rocky Mountain eastern slopes river is much younger than previously thought
• Characterizing baseline soil gas conditions at the Containment and Monitoring Institute (CaMI) CO<SUB>2</SUB> Injection Site in Alberta, Canada
• Community Engagement through Citizen Science Projects for Canadian Cordillera Array and EON-ROSE
• Computational Geophysical Approach to the Stochastic Inversion Modelling of Intracellular Copper Transport Kinetics and Steady-State Isotopic Fractionation within Saccharomyces Cerevisiae
• Contrasting nearshore and offshore responses to the tributary inputs of carbon and sulfur into Lake Erie
• Detection and location of earthquakes in the Canadian Rocky Mountain Trench by kurtosis and Bayesian sampling in the presence of strong cultural noise
• Experimental Examination of the Coupled Dissolution-Precipitation Kinetics of Ca-Feldspar and Calcite at 80<SUP>o</SUP>C
• Extreme carbon sequestration during incipient rifting of western Gondwana
• Geochemical change of groundwater by artificial CO<SUB>2</SUB> leakage through shallow silicate aquifer: emphasis on pH buffering
• Geophysical and Geochemical constraints on a regional hydrogeological model of Banff Hot Springs.
• Geophysics as an Aid to Reducing Fluoride Concentrations in Drinking Water in the Kakuma Refugee Camp, Kenya, and the Identification of Skeletal Fluorosis in a Resettled Refugee
• Ground-motion analysis of an induced-seismicity sequence associated with a hydraulic-fracturing stimulation in a Duvernay shale play, western Canada
• Hydrogeophysical Characterization of the Unique Groundwater Discharge Features Termed "Soap Holes" on the Great Plains
• Induced seismicity due to hydraulic fracturing: how far from faults?
• Investigating gas leakage from oil and gas wells in NE BC, Canada through statistical analysis of occurrence, regional hydrogeological field investigations and controlled subsurface natural gas release experiments
• Lithospheric Structure Controls the Location of Intracontinental Seismicity in Australia
• Petrographic and numerical evaluation of the glauconite carbonation reaction as a CO<SUB>2</SUB> trapping mechanism
• Seismicity-Scanning based on Navigated Automatic Phase-picking (S-SNAP)
• Silica Replacing Pyrite and Quartz Sulfidation Within the TAG Sulfide Mound as the Hallmark of the Stockwork Mineralization.
• Source Analysis of Induced Earthquakes in the Duvernay Play Near Fox Creek, Alberta, Using Empirical Green's Functions
• Tochilinite Occurrence in Serpentinized Peridotite from the Samail Ophiolite
• Trans-dimensional Inversion and Uncertainty Quantification in Seabed Geoacoustics
• A Toolbox for the Accurate Detection of the Sources of Fugitive Methane Associated with Development of Unconventional Hydrocarbon Resources
• A distributed acoustic sensing and geophone array to study the Mt. Meager Volcano
• A novel nodal seismic investigation into the Mt. Meager geothermal system
• A receiver function investigation into the crustal structure of the Rocky Mountain Trench near Valemount, British Columbia
• Autogenic translation and concave bank deposition in meandering rivers
• Crustal and upper-mantle structure of the northern Canadian Cordillera using Bayesian joint inversion of receiver-functions and surface-wave dispersion curves
• Effects of Intrabasinal Recycling on the Preservation of Tectonic and Climate Signals Determined from Provenance Analysis
• Efficient Bayesian model selection strategy for tsunami source inversion
• Evidence for Projectile Tunneling at Small Craters on Asteroid (101955) Bennu
• Evolution of Grain Shapes by Dissolution: A Comparison of Pore-Scale Simulations and Microfluidic Experiments
• Exploring ambient noise correlation technique for monitoring CO<SUB>2</SUB> injection at the CaMI Field Research Station
• Fugitive gas migration and effluxes at oil and gas sites
• Glacial Isostatic Adjustment with 3D Earth models in North America
• Hisingerite-forming serpentinization in the Duluth Complex (USA): A rare terrestrial analogue for serpentinization on Mars
• How Is Sediment Transported through Submarine Channels and onto Lobes? New Insights from Turbidity Current Monitoring and Repeat Seafloor Mapping
• Hydraulic-Fracturing Induced Seismicity Driven by Aseismic Creep
• Induced seismicity and the phenomenon of runaway rupture earthquakes
• Interactive 3D Visualization and Dissemination of UAV-SfM Models for Virtual Outcrop Geology
• Location uncertainty for induced events: A comparison of fully nonlinear Bayesian estimates to double-pair double difference relocations for large datasets
• Meander kinematics and their depositional products in modern and ancient rivers
• Migrating knickpoints are primary morphodynamic agents in submarine channels that control deep-water stratigraphy
• New Visions for Oil Spill Preparedness from the Perspective of the Deepwater Horizon Blowout, the Sediment Slumping at Taylor Energy, and Continued Ultra-Deep Oil Exploration and Production in Frontier Region
• Novel Thermal Maturity Parameters Derived from Alkylbiphenyls
• Observations of long-lived hydraulic-fracturing induced earthquake swarms support driving role of aseismic creep
• Passive seismic monitoring at the CaMI Field Research Station, Alberta, Canada
• Recent doubling of mid- and low-latitude glacial lakes
• Response of the soil water budget in a grassland of the Canadian Prairies to climate change
• Seismic Hazard due to Fluid Injections
• Signatures of focused fluid flow and methane venting along the Queen Charlotte Fault off southeastern Alaska and western British Columbia
• The need for comprehensive benthic baselines and monitoring programs prior to marine petroleum extraction: Lessons learned form the Deepwater Horizon Oil Spill
• Transient Nanoporosity at the Reaction Front in Serpentinized Peridotite
• Turbidity current evolution in Bute Inlet, British Colombia, Canada
• Uncovering relationships between ground shaking and coseismic landsliding during the April 25, 2015 Gorkha Earthquake through full wavefield simulations using SPECFEM3D
• Variability in the Temperature of Groundwater Discharge to a First-order Alpine Stream as a Function of Flow Path
• Alkalinity Constraints on Basalt Carbonation for Permanent CO<SUB>2</SUB> Storage
• Combined experimental interpretation and numerical investigation of the impact of fluid alkalinity on basalt carbonation during CO<SUB>2</SUB> storage
• Crustal fault regime and stress field in northern Chile: Insights on partition from the subduction interface
• Distributed Acoustic Sensing for the Exploration of the Mount Meager Volcanic Complex, British Columbia, Canada.
• Fluvial response to climate change-induced stream capture, Yukon, Canada
• Gas migration in the shallow subsurface: Insights from a natural gas release into a deep vadose zone
• Gatekeeper function of alpine aquifers for the resilience of headwater streams
• Linking Slab Structure to Mantle Dynamics in the South American Subduction Zone
• Microseismic monitoring at a shallow CO<SUB>2</SUB> injection site, the CaMI Field Research Station in Alberta, Canada
• Reconstruction of Tweedsmuir Glacier's surge cycle with historical images
• Spontaneous Imbibition Dynamics of Liquids in Homogeneous Nanoporous Media: Experiment and Theory
• Thermal history modelling in extensional settings: the Rwenzori Mountains of the East African Rift
• Timing of Bedrock Exhumation Across the Columbia River Fault near Revelstoke, BC
• The Stress-dependence of Poroelasticity in Low-permeability Rocks
• Use of a New Core Analysis Method ('RTAPK') to Evaluate Permeability to Multiple Gases Using a Low-Permeability Coal Sample: Implications for CO2 Sequestration

Linked Collaborating Authors [?]