McGill University, Department of Earth and Planetary Sciences

    flowchart
    I[McGill University, Department of Earth and Planetary Sciences]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (273)"]
    CA["Linked Collaborating Authors (2)"]
    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 [?]

A11732

Abbreviation [?]

Dep Ear Plan Sci

Parent Institutions [?]

• McGill University, Canada

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• Demagnetization of Martian Crust by Large Impacts
• Magnetic Anomalies of Mars
• The Elastic Properties of the Lithosphere Beneath Scotian Basin
• The Strength of the Lunar Interior
• A Comparison of Historic Caldera-Forming Events
• The Nature of Sulfide Weathering in the Submarine Environment: Evidence From the Southern Explorer Ridge.
• Initial Field Trials for Development of RMDI, a Miniaturized UV/Visible Spectrometer Designed for Multi-gas Remote Sensing of Volcanic Plumes
• Retrograde Evolution of the Hemlo Gold Deposit, Ontario: Fractional Crystallization of a Sulfide Melt and Remobilization of Ore-Related Metals
• The Active Period of the Core Dynamo of Mars
• Carbon Mineralization Pathways and Early Diagenesis in Lake Erie Sediments
• Oxygen Isotope Fractionation between Synthetic Aragonite and Water: Influence of Solution Chemistry
• Resolving power of satellite magnetic data for lithospheric field characterization
• The formation of the lunar and Martian mascons
• Analogue Experiments Investigating Magma Degassing Under Submarine Conditions
• Assessing the Impact of Retreating Glaciers on Dry-Season Discharge in a Tropical Andean Watershed
• DOC Cycling in Ancient Tropical Lake Matano
• Earth Hazards Consortium: a Unique Approach to Student-Centered Learning
• Experimental Study of Bubble Growth in Stromboli Basalt Melts at 1 atmosphere
• Gas Hydrate Research Coring and Downhole Logging Operational Protocol
• Magma Interactions in Rhyolite Reservoirs Caused by Injection of New Rhyolitic Liquid: Results From Analogue Modeling
• Magma mixing during caldera forming eruptions
• Magnetic Properties of Sediments from IODP Expedition 311 - Cascadia Margin Gas Hydrates: Records of Fossil Sulphate Methane Interface?
• Nature of Magma Recharge at Soufrière Hills volcano, Montserrat, West Indies
• Punctuated Sediment Input into Small Subpolar Ocean Basins During Heinrich Events and Preservation in the Stratigraphic Record
• Sand, Syrup and Supervolcanoes
• Simulations of Bubble Size Distributions and the Formation of the Giant Bubble
• The 3D Skeleton Of Basaltic Vesiculating Magmas And Implications For Degassing Pathways And Shallow Conduit Dynamics
• The REE (+Y) And Major Element Chemistry Of An Anhydrite/Caminite Dominated Black Smoker Sample, EPR 9 50'N
• The fate of Pb during dissimilatory iron reduction
• The granular sea-ice model in spherical coordinates and its application to a global climate model
• Volatile Contents of Melt Inclusions From Andesite Pumice at Soufrière Hills volcano, Montserrat, West Indies
• F and Cl Diffusion in Phonolitic Melts
• Fine scale control of microbial communities in deep marine sediments that contain hydrates and high concentrations of methane
• Fluid/Melt Partition Coefficients Of Halogens In Basaltic Melt
• Individual magma batches related to the origin of Yellowstone 516-70 ka post-caldera rhyolitic lava flows : results from glass geochemistry.
• Magma Vesiculation and Infrasonic Activity in Open Conduit Volcanoes
• Magma chamber rejuvenation associated with Yellowstone 516-70 ka post-caldera rhyolitic lava flows : results from crystal geochemistry
• Nd Isotope Systematics for the 3.8 Ga Nuvvuagittuq Greenstone Belt: Implications for the Degree of Depletion of Early Earth's Mantle
• Possible Eukaryotic Magnetite in the Paleocene-Eocene Boundary Clay, Ancora, New Jersey
• Seismic Reflection Blank Zones in Ulleung Basin, Offshore Korea, Associated With High Concentrations of Gas Hydrate
• Sulfur and oxygen isotope studies of sulfate reduction
• Testing the Paleocene-Eocene Thermal Maximum Magnetofossil Spike Hypothesis
• Anthropogenic Transformation of the Biomes, 1700 to 2000
• Metal Concentrations and Hydrochemical Dynamics in a Tropical-Glacier Watershed
• Pressure Effects in the Mass-Independent Fractionation Parameters of UV-Photolyte Sulfur from Broadband Irradiation of SO2
• Thermophiles as Candidate Iron-Reducing Bacteria For the Putative Biogenetic Magnetite in Banded Iron Formations
• An Appalachian Amazon? Magnetofossil evidence for the development of a tropical river-like system in the mid-Atlantic United States during the Paleocene-Eocene Thermal Maximum
• Ankaramitic Lavas and Clinopyroxene Megacrysts From the Tanganasoga Volcano, El Hierro Island (Canary Archipelago)
• Causes of supervolcano eruptions
• Compositional and thermal zoning within quartz ejected before, during and after a supervolcanic eruption at 1.256 Ma: Valles Caldera, New Mexico, USA
• Do the Columbia Hills of Gusev Crater Represent a Layered Igneous Intrusion on Mars?
• Groundwater Flow with Freeze-Thaw in Dynamic Permafrost Systems: Numerical Simulation
• Implications of the Nuvvuagittuq “faux-amphibolite” for the formation of Earth’s early crust
• Kimberlite degassing and paleoclimate
• Magma differentiation and volatile evolution at Fuego Volcano, Guatemala
• Minerals fractionate and modulate the dissolved organic carbon flux out of marine sediments
• Proglacial hydrology in the tropical Andes: lessons from the Cordillera Blanca, Peru (Invited)
• Spatial and temporal variations in subduction angle: a role for subduction erosion processes?
• Tectonics, climate and mountain building in the forearc of southern Peru recorded in the 10Be chronology of low-relief surface abandonment
• The future of volcanism at Yellowstone caldera
• The oxygen side of sulfate constrains global biospheric productivity in the mid-Phanerozoic
• Thermal History of the Bandelier Magmatic System: Evidence for Magmatic Injection and Recharge at 1.61 Ma as Revealed by Cathodoluminescence and Titanium Geothermometry
• Using global land cover data to assess regional food production potential
• An Analysis of Sulfur Content and Multiple Sulfur Isotope Fractionation of Tephra Deposits at Valles Caldera, New Mexico: Variations over the Course of Two Caldera-Forming Eruptions
• Application of the MultiGAS Sensor to Geothermal Exploration and Monitoring: Comparison of Plume and Fumarole Gas Compositions at Kawah Ijen Volcano, Indonesia
• Barium and Carbon fluxes in the Canadian Arctic Archipelago
• Crustal Thickness Variations Across Eastern Canada and Maine From Receiver Function Analysis
• Distributed Temperature Sensing of hyporheic flux patterns in varied space and time around beaver dams
• Evolution of Early Paleoproterozoic Ocean Chemistry as Recorded by Black Shales
• Interdisciplinary graduate student symposium organized by students for students
• Modeling of permafrost dynamics and hydrological processes under seasonal and long term temperature variations
• Polyphase rifting within Rodinia as seen through multiple episodes of mafic volcanism within the Canadian Cordillera
• Proglacial hydrology in the Cordillera Blanca, Peru
• Recently active contractile deformation in the forearc of southern Peru
• Steady-state behavior of the Soufrière Hills volcano, Montserrat
• Sulfur Isotopic Inferences of the Controls on Porewater Sulfate Profiles in the Northern Cascadia Margin Gas Hydrate System
• The Location and most Viable Magnetic Mineral of the Magnetic Layer of Mars Crust
• Trace element partitioning between minerals and aqueous fluid as a tool to unravel element release from the subducting slab
• A model for caldera resurgence
• Coseismic overpressure recorded in fault rocks
• Deglacial changes in the subarctic Pacific ecosystem: links to ocean circulation, deoxygenation and carbon storage
• Do faults stay cool under stress?
• Landscape modification in a glaciated tropical mountain range: Basin-averaged 10Be erosion rates from the Cordillera Blanca, Peru
• Late Cenozoic Exhumation in the Northern Peruvian Andes
• Mesozoic fault reactivation along the St. Lawrence Rift System as constrained by (U-Th/He) thermochronology
• Origins of apparent conglomerates of the Nuvvuagittuq Greenstone Belt (Nunavik, Québec): Sulfur and oxygen isotope evidence and chronological implications
• Past peak water in Peru's Cordillera Blanca: diagnosing the demise of glacier influence on stream discharge
• Rupture process of oceanic transform faults linked to material variability: local observations and models of the Gofar Fault, EPR
• Southern Ocean overturning, export production and climate variability over the past 1 Myr
• Synoptic global view of nitrogen isotopes in the modern and glacial oceans
• Textural evidence for jamming and dewatering of a sub-surface, fluid-saturated granular flow
• The Behaviour of Base Metals in Arc-Type Magmatic-Hydrothermal Systems - Insights from Merapi Volcano, Indonesia
• The Role of Sulfur on Major Fluctuations in the Carbon Cycle During the Neoproterozoic Interglacial Interval
• The Rusty Sink: Iron Promotes the Preservation of Organic Matter in Sediments
• The importance of groundwater flow in thawing permafrost systems
• The regolith hypothesis for the Tonian-Cryogenian transition
• Thresholds of glacier hydrologic change and emergent vulnerabilities in a tropical Andean waterscape
• Using multiple natural and injected tracers to evaluate spatial and temporal patterns of hyporheic flux and biogeochemistry
• Volcanology and Geochemistry of the Taney Seamounts northeast Pacific Ocean
• What's Cooking? Evaluating frictional stress using extractable organic material in fault zones
• δ13C Degassing Dynamics of a Young Volcanic Center, Cerro Negro, Nicaragua
• "Gray Areas": Silica gels, amorphous silica and cryptocrystalline silica on fault surfaces
• A continuous transect through the lower seismogenic zone of a transform boundary: The Pofadder Shear Zone, Namibia and South Africa
• An old question revisited: the mechanics of shallow creep events on strike-slip faults and their triggering by nearby earthquakes
• Changing Hydrology in Glacier-fed High Altitude Andean Peatbogs
• Connecting multi-scale fault geometry with field observations: insights into fluid-fault rock relations
• Did the Moon have a dipolar field?
• Do volcanic gases represent equilibrium volatile concentrations? Some insights from a model of diffusive fractionation during rapid bubble growth
• Exhumation of the Western Cordillera of the Peruvian Andes (5-12°S)
• Groundwater-surface water interactions in a glacierized catchment and their influence on proglacial water supply
• Holocene denudation and landscape deformation in the Cordillera Blanca, Peru
• Organic geochemical evidence for frictional heating of the NE Japan décollement in drillcores from Expedition 343: JFAST
• Processes governing transient responses of the deep ocean buoyancy budget to a doubling of CO<SUB>2</SUB>
• The Finlayson Lake Greenstone Belt, Superior Province, Canada: A Structural Perspective
• The Importance of Sulfur on Enriched Carbon Isotopes and Extreme Carbon Cycle Perturbations of the Cryogenian
• The NICOPP synthesis of the marine sedimentary nitrogen isotope record 0-30,000 years BP: Documenting deglacial changes in the marine N cycle
• The role of pegmatites and acid fluids for REE/HFSE mobilization in the Strange Lake peralkaline granitic pluton, Canada
• Towards inferring geodetic signatures of megathrust coseismic slip, afterslip and slow slip events in an earthquake cycle under the influence of dilatancy
• Applying time-reverse-imaging techniques to locate individual low-frequency earthquakes on the San Andreas fault near Cholame, California
• Characterizing changing stream water quality in a glacierized tropical watershed
• Detecting the frictional temperature rise during the 2011 Tohoku Earthquake using the thermal maturity of biomarkers
• Effects of Drake Passage widening during the Eocene-Oligocene Transition on Southern Ocean bulk sediment trace element geochemistry
• Groundwater, springs, and stream flow generation in an alpine meadow of a tropical glacierized catchment
• Hillslope runoff temperatures and their influence on winter stream temperature for a coastal forested catchment
• Hydrothermal REE and Zr mobilization in the Strange Lake peralkaline granitic system: a reaction path model linked to petrological and geochemical observations
• Internal structure of the shallow Japan Trench décollement: insights into the long-term evolution of the margin and coseismic slip processes
• Mechanism of spontaneous and triggered shallow creep events - Implications for shallow fault zone properties
• Numerical modeling on the source parameter scaling relations and synthetic surface deformation of episodic slow slip events in subduction zones
• Oceanic transform fault earthquake nucleation process and source scaling relations - A numerical modeling study with rate-state friction (Invited)
• Paleomagnetic records of core samples of the plate-boundary thrust drilled during the IODP Japan Trench Fast Drilling Project (JFAST)
• Permafrost response to climate change: Linking field observation with numerical simulation
• Shrinking Arctic Lakes are Forming New Local Permafrost, but for How Long?
• Silica Lubrication in Faults (Invited)
• The Downstream Fate of Glacial Runoff and Groundwater in the Cordillera Blanca, Peru
• The behavior of sulfur, volatile species and metals in subduction zone, magmatic-hydrothermal systems: Insights from Merapi volcano, Indonesia (Invited)
• Using an Earthquake Simulator to Model Tremor Along a Strike Slip Fault
• Development of Mylonites and Pseudotachylites in Granitic Bodies: Brittle Deformation by Reactivation of Pre-existing Ductile Fabrics Defined by Mica
• Evolution of the Proterozoic Earth System: Insights from the Δ<SUP>17</SUP>O Record of Sedimentary Sulfate Minerals
• Modeling the Failure of Magmatic Foams and Application to Infrasonic Signals at Stromboli Volcano, Italy
• The Implications of the Moon-Forming Impact for Terrestrial Oxidation State and Surface Water Stability
• The Vanda Dike Swarm, Dry Valleys, Antarctica II: Geochemistry and Geochronology
• Cold seep carbonates along the Norwegian margin, insights into U-Th geochronology and S geochemistry
• Coseismic brecciation at fault stepovers and transient fluid pathways in a mid-crustal San Andreas analogue: The Pofadder Shear Zone, Namibia and South Africa
• Earthquake lubrication and healing explained by amorphous nanosilica
• Evolution of the fluid in the REE-rich pegmatites of the Strange Lake pluton
• Investigating sulfur partitioning between nominally volatile-free minerals and silicate melts
• Linking Deformation and Diffusion to Develop a Strain Speedometer in Plagioclase
• Multi-surface Earthquake Rupture Recorded in Pseudotachylyte Vein Geometries, Norumbega Shear Zone, southern Maine
• Rapid ductile afterslip from coseismic heating
• Refining the chemical composition of the inner core with multicomponent alloys: from first-principles to thermodynamics and seismology
• Relationship between amorphous silica and precious metal in quartz veins
• Sedimentary environments and preservation biases limit sulfur isotope fractionation observed in pyrite, despite large microbial fractionations
• Using Multiple Sulfur Isotope Signatures to Delineate Terrane Boundaries and Investigate Crustal Formation Mechanisms during the Paleoproterozoic
• Why Are Andesitic Eruptions Often More Violent Than Basaltic Ones? -- Insights from 4D X-ray Tomographic Microscopy
• A Comparison Between Modeling and Field Observations of Off-Fault Strain around Pseudotachylyte Fault Veins, Norumbega Shear Zone, southern Maine
• Assessing the impacts of 1.5°C of global warming - The Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) approach
• Computing phase relations involving ordered solid solutions ab initio: Three thermodynamic approaches to the Fe-Si binary
• Dipping Upper Mantle Boundary Beneath Southeastern Superior Province - a Trace of Archean Subduction?
• Fluid Flow, Reactions and Exhumation of Mantle Peridotite Along a Serpentinite Fault Zone.
• Geological Development of the Izu-Bonin Forearc Since the Eocene Based on Biostratigraphic, Rock Magnetic, and Sediment Provenance Observations from IODP Expedition 352 Drill Cores
• Heterogeneous bubble nucleation on pyroxene and plagioclase in andesite magmas
• Insights into Magmatic Degassing at Merapi Volcano, Indonesia from Uranium-Series Disequilibria in Recently Erupted Volcanic Rocks
• Insights into earthquake rupture and recovery from paleoseismic faults
• New Frontiers for Deep Fluids and Geobiology Research in the World's Oldest Rocks
• On the transport of physical and biogeochemical tracers into the North Pacific and North Atlantic subtropical gyre
• Opal-replaced "Phenocrysts" in Fresh Pumice from 1817 Phreatomagmatic Deposits from Kawah Ijen, East Java, Indonesia: Implications for Eruptive Timescales?
• Sliding history and energy budget recorded in a frozen mantle earthquake
• The Role of Microbial Iron Reduction in the Formation of Proterozoic Molar Tooth Structures
• Tracing Magmatic Degassing Timescales at Soufrière Hills Volcano using Short-Lived Uranium Series Isotopes
• Understanding Earthquake Slip Surface Distribution in a Lithologically Heterogeneous Shear Zone
• A Sulfur Trigger for the 2017 Phreatomagmatic Eruption of Poás Volcano, Costa Rica? Insights from MultiGAS and Drone-based Gas Monitoring
• Climate reconstruction from borehole temperatures influenced by groundwater flow
• Crustal Structure and Seismic Anisotropy in the St-Lawrence/Charlevoix Region, Eastern Canada
• Earthquake source parameter and focal mechanism estimates for the Western Quebec Seismic Zone in eastern Canada
• Groundwater controls on post-fire permafrost thaw
• How Might Draining Lake Campotosto Affect Stress and Seismicity on the Monte Gorzano Normal Fault, Central Italy?
• Interactions of ice sheet evolution, sea level and GIA in a region of complex Earth structure
• Isotopic composition of reduced and oxidized sulfur in the Canary Islands: implications for the mantle S cycle
• Mafic Spatter-Rich and Lava-Like Welded Ignimbrites Linked With Collapse of a Basaltic Caldera: The Halarauður Eruption, Krafla, Iceland
• Numerical simulation of dynamic triggering of aseismic slip events in Northern Chile and New Zealand
• Observation of ground deformation associated with hydraulic fracturing and seismicity in the Western Canadian Sedimentary Basin
• Processes of 21st Century Ice Sheet Melt and their Global Consequences
• Proglacial Hydrogeology of the Cordillera Blanca (Peru): Integrating Field Observations with Hydrogeophysical Inversions to Inform Groundwater Flow Simulations and Conceptual Models
• Smoothing of Fault Slip Surfaces by Scale Invariant Wear
• Stress Rotation Across the Cascadia Megathrust Requires a Weak Subduction Plate Boundary at Seismogenic Depths
• Subsurface flow recently triggered the development of taliks under a sub-Arctic road embankment: a prelude to the collapse of the Alaska Highway?
• Sulfur partitioning applied to LIP magmatism - A new approach for quantifying sulfur concentration in basaltic melts
• The influence of fluorine on phase relations and REE enrichment in alkaline magmas
• The permeability of fault zones in the upper continental crust: statistical analysis from 460 datasets, updated depth-trends, and permeability contrasts between fault damage zones and protoliths.
• Tourmaline's record of Alpine metamorphism and segregation formation in the Pfitsch Formation, Western Tauern Window
• Volcanic activity at Etna volcano, Sicily, Italy between June 2011 and March 2017 studied with TanDEM-X SAR interferometry
• Water and CO<SUB>2</SUB> content of melt inclusions from the high-silica rhyolite Bandelier Tuff super-eruptions, New Mexico, USA
• A simple box model of nutrient fluxes in the St. Lawrence Estuary
• Advances in submicron Raman spectroscopy mapping of serpentinite fault rocks
• Assessing Variability of Intraplate Crustal Stress Orientation and Seismic Hazard in the Charlevoix Seismic Zone, Eastern Canada
• Biogeochemical signatures in coralloid speleothems in basaltic lava tubes
• Characterizing the Microbial Community of Lava Tube Ice for Determining its Habitability on Mars
• Constraining Geological Structures and Temporal Variations in Fluid Accumulation near Hydraulic Fracturing Injection Sites in the Western Canada Sedimentary Basin
• Constraining fault-valve behavior at Val d'Or, Quebec.
• Controls on the dissolution rates of natural and synthetic calcites under seafloor-like conditions
• Cryohydrogeology - Is Groundwater a Catalyst for Arctic Change?
• Cyclic Compositionally Zoned Explosive Eruptions at an Arc Volcano (Cosigüina, Nicaragua): Implications for Magma Reservoir Processes
• Development of in situ analysis of δ<SUP>7</SUP>Li in garnets to decipher metamorphic processes
• Dynamic rupture simulation along the southern San Andreas Fault through the San Gorgonio Pass - Effects of fault geometry and 3D velocity model
• Evaluation of Climate Impacts on Andean Hydrology Using an Integrated Groundwater, Surface Water and Glacier Model.
• Geologic observations of fault healing
• Geometric complexity of earthquake rupture surfaces preserved in pseudotachylyte networks
• Heat Transfer Triggered by Mobile Subsurface Water Degrades Permafrost and Impacts Overlying Highways
• How permafrost thaw will affect the groundwater contribution to streams and lakes?
• Improving the Accuracy of Stream Temperatures Acquired through Ground-Based Time-Lapse Thermal Infrared Imagery
• Influence of Water-Rock Interaction on Cave Biogeochemistry
• Methane Radiocarbon and Clumped Isotope Measurements in Lakes from Permafrost Landscapes Link Methanogenesis Kinetics with the Age of Carbon Substrates
• Modeling Short-term Ice sheet - Sea level - Solid Earth Interactions within a Glacial-cycle Timescale Simulation
• Monitoring Gases via Drone during the 2017 Eruption Crisis at Poás Volcano, Costa Rica
• Near real-time isotopic measurements of CO<SUB>2</SUB> sampled by drone at Stromboli, Italy
• New Evidence of an Ancient Martian Ocean from the Global Distribution of Valley Networks
• Numerical modeling of dynamically triggered shallow slow slip events in New Zealand by the 2016 M w 7.8 Kaikoura earthquake
• Quantifying the uncertainty in GNSS-R sea level measurements
• Rupture to the trench? Frictional properties of incoming sediments at the Cascadia subduction zone
• Searching for a Seismic Signature in the Landscape of the Western Quebec Seismic Zone, Canada
• Seismicity from a dense hydraulic fracturing stimulation monitoring array favors a fluid diffusion mechanism in a low-permeability shale formation in the Montney Basin, British Columbia
• Spatter-Rich and Lava-Like Ignimbrites of the Halarauður Eruption, Krafla (Iceland): An Unusually Violent Eruption From a Basalt-Dominated Caldera
• Sulfur Systematics Record the Volatile-Rich, Oxidized, and Recycled Nature of the Canary Island Mantle Source
• The influence of Northern Hemisphere ice sheets on Antarctic ice dynamics during the Last Deglaciation
• Transecting the Cordillera Blanca of northern Peru: a glacial geochronology determined from <SUP>10</SUP>Be exposure ages of moraine crest boulders
• Tree rings as a volcanic gas proxy: carbon and sulfur isotopes in proximal trees linked to volcanic degassing fluctuations through time
• Triple sulfur isotope fractionation associated with sulfate reduction in modern marine sediments
• What Do GPS-derived 1-D Viscosity Models Represent Given Antarctica's Complex 3-D Structure?
• What does a tremorgenic rock look like?
• Conduit controls on the release of material at the onset of two caldera-forming eruptions: case study from the Bandelier Tuff
• Does Sporadic Permafrost Influence Catchment-scale Groundwater Processes?
• Earthquake lubrication and healing caused by amorphous silica powder - experimental wear products compared to natural fault rocks
• Earthquake triggering in the crystalline basement from hydraulic fracturing: two examples from the Montney Basin, BC, Canada.
• Evaluation of inter-annual to decadal changes in tropical Andean stream chemistry below debris-covered glaciers
• Examining possibilities for speleothem biosignatures in Mars lava tubes based on Californian lava tubes
• Fracture energy of Cascadia input sediments integrated into a global compilation
• Global patterns in the hydrogen isotope composition of methane from freshwater ecosystems with implications for source apportionment and methanogenesis pathways
• Investigating the Bias in GPS-derived 1-D Viscosity Models due to Antarctica's Complex 3-D Mantle Structure
• Late Permian cold subduction in the Yukon-Tanana Terrane, Yukon Territory, Canada: Progressive elcogitization in the lawsonite stability field recorded by lawsonite and garnet inclusions in garnet
• Mineralogical clues to the origin of the serpentinite mélange on Ring Mountain
• Modeling Northern Hemispheric ice sheet dynamics, sea level change and solid Earth deformation through the last glacial cycle.
• On-Ramps to More Effective Teaching: Quick-Start Guides to Strategies for Actively Engaging Students in The Classroom to Improve Learning
• Precise Ground-Based GNSS-Reflectometry Sea Level Measurements Using Low-Cost Antennas
• Quantifying Surface Roughness Development of Experimentally Sheared Fault Surfaces
• Quantitative Relationship Between Injection Operations and Induced Seismicity in the Southern Montney Play, British Columbia, Canada
• Radiocarbon Data from Permafrost Peatland Lakes Indicate Dissolved Methane is Dominantly Modern while Particulate Matter and Ebullition Methane Contain Older Carbon
• Revitalizing the classic "Streetcar to Subduction" Field Guide to the San Francisco Bay Area via Google Earth
• Role of hydrous minerals in the structure and rheology of the subduction plate interface
• Searching for Extant Life on Mars: What's Next?
• A bio-physically-based model of the human-Earth System applicable to long timescales
• A three-dimensional groundwater flow simulation of Granger Basin, Yukon, Canada
• Carbon Isotope Systematics of Poás Volcano, Costa Rica, from 2017 to 2019
• Chasing the Franciscan megathrust and its implications for Deep Subduction Zone Dynamics: Insights from Angel Island, Franciscan Complex.
• Deformation mechanisms of phyllosilicates and amphibole and the interdependence of deformation in polymineralic rocks
• Exhumation-related deformation in a developing thin-skinned nappe complex: Naukluft, Namibia
• Geological constraints on the mechanisms of slow earthquakes
• Groundwater in high mountains: Climate change impacts on a hidden water resource
• How waters feeding the eastern American continental slope affect oxygen concentrations in the St. Lawrence Estuary
• Linking Fault-Related Injection Veins to Paleoearthquake Cycles: Observation from the Muddy Mountain Thrust, NV, USA
• Metamorphic thermobarometry captures a rheology-controlled subduction depth limit in exhumed high-pressure/low-temperature rocks exposed on Syros, Greece
• Near-surface structure and mechanical properties of shallow seismogenic faults: Implications for ground-motion simulations
• Ocean Acidification: Insights from the Paleocene-Eocene Thermal Maximum (PETM)
• Potential Uncertainties in Measuring Soil Moisture with Active Fiber Optic Distributed Temperature Sensing
• Reactive gossans in permafrost as indicators of ancient hydrothermal activity on Mars
• Structural petrology and petrochronology record subduction, underplating, and return flow in the Cycladic Blueschist Unit exposed on Syros Island, Greece
• Temperature rise, slip localization, and fault weakening as observed from the rock record
• The economic potential of granitic pegmatites in Sri Lanka: preliminary findings
• The potential for spatial resolution of freshwater methane emissions using hydrogen isotope measurements
• Trees as sensors of pre-eruptive change
• Tropical CO<SUB>2</SUB> Fertilization using Volcanic CO<SUB>2</SUB>: Results from a Recent CO<SUB>2</SUB> Mapping Field Campaign at Volcán Rincón de la Vieja in Costa Rica
• Walking the seismogenic zone: A field geology perspective on earthquakes
• Greenhouse Gas Emissions From Permafrost Peat Altered by Gradual Drying but Depends on Landscape Position and Peat Biogeochemistry
• How Does Climate Warming Affect the Mass Transport of a Nonreactive Solute in a Thawing Permafrost Environment?

Linked Collaborating Authors [?]

• Jeffrey M. McKenzie
• Thomas M. Mitchell