Durham University, Department of Earth Sciences

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    I[Durham University, Department of Earth Sciences]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (555)"]
    CA["Linked Collaborating Authors (3)"]
    I== skos:broader ==>PI
    CI== skos:broader ==>I
    AW== affil ==>I
    AW== author ==>CA
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    click CI "#child-institutions"
    click AW "#affiliated-works"
    click CA "#collaborating-authors"

ADS ID [?]

A00499

Abbreviation [?]

Dep Ear Sci

Parent Institutions [?]

• Durham University, UK

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• A Geophysical Investigation and Geological Interpretation of a Super-Slow Spreading Segment at the South West Indian Ridge (SWIR).
• BIFROST project: 3-D site motion inferred from 2500 days of continuous GPS in Fennoscandia and implications for regional changes of sea level
• Contribution of Pyroxenite-Derived Melts to Baikal Rift-Related Magmatism
• Fault Characteristics and Strain Accommodation at the Ultra Slow Spreading South West Indian Ridge (SWIR).
• A Western Pacific Hotspot?
• Crustal Profiling in Iceland Using Earthquake Source-Arrays
• Proof of plumes, or richness of plate tectonics?
• RAMESSES II - Mapping an Axial Melt System Beneath a Slow-Spreading Ridge
• Techniques for Obtaining Crustal Structure from Inversion of Receiver Functions by Using Additional Data Constraints
• Application of the Rhenium-Osmium Isotopes to the Geochronology of Diamonds
• Comparison of U-series ages with (U-Th)/He apatite ages at Damavand Volcano, Iran
• Mid-Atlantic Ridge 29<SUP>o</SUP>N: New Insights on Ridge-Axis Faulting From High-Resolution, Deep-Towed Swath Bathymetry
• The Textural Analysis of Evolved Magmatic Systems; a Case Study on the Fish Canyon Tuff.
• Fluid Overpressure and Earthquakes Triggering in the Natural Laboratory of the Northern Apennines: Integration of Field and Laboratory Data
• Formation of the Rio Grande Rift and Upper Mantle Seismic Wave Velocity Anomaly
• From source to surface: An Os isotope study of the transfer of mantle source signatures in subduction-related melts
• Glacial Sea Level Variations and Their Effects on Resonance of the Ocean Tide in the Labrador Sea: Possible Implications for Ice Sheet Dynamics and Millennial Scale Climate Variation
• Seismic Imaging of the Antarctic Circumpolar Current near Drake Passage
• Seismic Reflection Signatures of Internal Waves and Thermohaline Intrusions in the Norwegian Sea
• Seismic Structure of the Continental Margin Offshore French Guiana and North-Eastern Brazil
• Seismic imaging of thermohaline circulation: observations from the Antarctic Circumpolar Current
• Strain Partitioning During Oblique Divergence: a Key Concept in Matching Geodetic, Seismological and Geological Datasets.
• U-Series Disequilibria From the East Pacific Rise (9N, 10N and 11N): evidence for off-axis magmatism along fast spreading ridges?
• UK Ocean Bottom Instrumentation Consortium: a New Pool of Seafloor Geophysical Equipment
• 3D crystal packing variation through a rythmic layer in the Dais Intrusion, Dry Valleys Antarctica: Initial insights through 3D micro CT analysis.
• A Mantle Domain With a Helium Isotope Ratio of 11Ra at the Margins of the North Atlantic Igneous Province
• Controls on Strain Localization in Continental Rifts: Importance of Reworking Interval and Basement Reactivation
• Crustal Structure of the Continental Margin Offshore French Guiana, Central Atlantic
• Crustal Structure, Gravity Anomalies and Flexure of the Continental Margin Offshore North-Eastern Brazil
• Distinguishing Phenocrysts From Xenocrysts; Dating the Onset of Volcanic Activity on the Isle of Rum, Scotland.
• Does Sea-Level Lowstand Always Lead to Cross-Shelf Valley Formation and Source-to-Sink Sediment Flux?
• Evolution from Oceanic Subduction to Continental Collision: A Case Study of the Northern Qaidam UHP belt
• Far-Field Post-Glacial Sea-Level Geometries as a Probe of Antarctic Ice History
• Guided Seismic Waves: Possible Diagnostics for Hot Plumes in the Mantle
• Holocene sea levels and palaeoenvironments, Southeast Sulawesi, Indonesia: Application of mangrove palynology and the transfer function approach.
• Kinematic Modeling and Complete Moment Tensor Analysis of the Anomalous, Vertical CLVD Bardarbunga, Iceland, Event
• Modelling Near-Field Antarctic Sea-Level Data to Explore the Possibility of a Dominant Antarctic Contribution to Meltwater Pulse IA.
• Physical Properties of Samples Cored From Atlantis Oceanic Core Complex, Mid-Atlantic Ridge 30 N
• Putting the geology back into Earth models
• Segmentation and Volcanic Cycles: Their Relationship and Evolution at the Southern Reykjanes Ridge, MAR
• Slurry flow and structures formation in a magma mush: the Basement Sill, McMurdo Dry Valleys, Antarctica
• Switches in the Stress Field Induced by Fluid Overpressures Below a Low-Permeability Fault Zone
• Textural and micro-Sr isotopic investigations of feldspar phenocrysts from the Teide-Pico Viejo stratovolcanic complex, Tenerife (Canary Islands)
• The Application of Terrestrial Laser Scanning Techniques to the Investigation of Mechanisms of Mass Movement
• The Geology of Weak Fault Zones: Long Term and Short Term Processes
• The Puzzle of the Petrology of Oceanic Plateaux
• The tide gauge record from the eastern US as a potential indicator of Greenland ice sheet mass balance
• Three-Dimensional Brittle Shear Fracturing by Tensile Crack Interaction
• Time-Dependent Tomography and Microearthquake Moment Tensors in the Coso Geothermal Area
• Using micro-isotopic approaches to evaluate the origin and emplacement mechanism of the Basement Sill, Dry Valleys, Antarctica
• What's in a Whole Rock Analysis? Integrating Crystal Size Distributions and Micro-Scale Isotopic Variations at Stromboli Volcano
• Xenocrystic Material in Arc Volcanics: Example from Recent Merapi Lavas
• Angular Variation of the Magnetic Properties and Reversal Mode of Aligned Single-Domain Iron Nanoparticles
• Arabia-Eurasia Collision: Multiple Causes of Oligocene Global Climate Cooling?
• Basement structural control on Cretaceous pull-apart basins of the central Eastern Egypt Desert
• Chlorite Stability in the Mantle Wedge and its Role in Subduction Zone Melting Processes
• Controls on Magma Differentiation at Arcs; Crystal Redistribution and a Role for Amphibole
• Curvature of Fault Planes and Heterogeneity of Slip Patches
• Episodic Crustal Growth Recorded in the Depletion History of the Mantle
• Exploring the Potential for Long-term Storage of Depleted Peridotite in the Mantle
• Footwall Extension During Low-Angle Normal Faulting
• Glacial Isostatic Adjustment as a Control on Arctic Coastal Processes
• How are `Super' eruptions preserved in the past? Volcanological features of Large Volume Silicic Eruptions of the Paraná-Etendeka
• Isotopic Constraints on the Generation of Voluminous Felsic Magmas During the Early Evolution of the Palaeocene Rum Igneous Centre, Scotland.
• Mediterranean undercurrent and Meddies imaging by multichannel seismic data.
• Microearthquake characterisation of an artificially stimulated hydraulic fracture at the Coso geothermal area, California
• New Estimates of Three-dimensional Crustal Motions in the British Isles from Continuous GPS, Geological Evidence and Glacial Isostatic Adjustment Models
• New Views of Seafloor Spreading Processes on the Very Slow Spreading Southwest Indian Ridge
• Polymodal Faulting by Crack or Anticrack Interaction
• Quantification of Stable Strontium Isotope Variability in Nature Using MC- ICPMS
• Quantifying Fold and Fracture Attributes Using Real Time Kinematic (RTK) GPS and Laser- Scanning
• Rheological Control of Interbedded Siliciclastic Strata on Damage Zone Evolution During Fault Growth
• Slip on 'Weak' Faults by the Rotation of Regional Stress in the Fracture Damage Zone
• The British-Irish Palaeocene Igneous Province Revisited: Influence of Crustal Composition on Differentiation Processes Across Four Major Crustal Terranes
• The Flux of Dissolved Organic Carbon From UK Rivers
• The Northern Apennines: a Key Area to Investigate the Feasibility of Detachment Accommodated Extension
• The Structure and Emplacement of the Western Granite, Isle of Rum, NW Scotland
• Towards a complete DOC budget for peat-covered catchments - accounting for upscaling and in-stream processes
• Trace Element Systematics in Bulk-Rock Abyssal Peridotites and Constituent Minerals: Evidence for Porous Melt Migration Beneath Ocean Ridges
• Understanding Crystal Populations: The Role of Textural Analysis in Determining Magmatic Timescales
• Variable Styles of Magma-Crust Interaction Recorded in Cone-Sheets at the Carlingford Igneous Centre, Republic of Ireland
• A Numerical Model for the Development of Magma Permeability During Eruption
• A multi-axial growth analysis of stable isotopes in the modern shell of Saxidomus gigantea: implications for sclerochronology studies
• An integrated geospatial model to investigate tectonics of the Caspian Sea region
• Capturing Detailed Outcrop Geology Using Terrestrial Laser Scanning (Lidar) and Other Digital Technologies: Current Status and Future Directions
• Constraining differentiation processes and timescales from mineral-scale isotopic data
• Constraints on the Rates of Replenishment, Magma Mixing, and Crystal Recycling at Santorini Volcano, Greece
• Continental Collision Zones are Primary Sites of net Continental Crustal Growth: Evidence From the Linzizong Volcanic Succession in Southern Tibet
• Coronae on Venus: Relationship of Geology to Gravity
• Could managed burning of peatlands lead to carbon storage?
• Deep-Towed Sidescan Sonar Studies of Amagmatic Spreading Centres: the Mid-Atlantic Ridge at 13N
• Did an Earthquake Trigger the Eruption of the Sidoarjo (Lusi) Mud Volcano?
• Earth's deep H cycle: H isotope evidence from the Manus Basin for complementary recycled reservoirs
• Elucidating the Holocene Relative Sea-Level History of the US Atlantic Coast
• Fault Zone Architecture and Deformation Processes Within Exhumed Evaporitic Rocks in The Upper Crust
• Fluid Overpressure and Earthquakes Triggering in the Natural Laboratory of the Northern Apennines: Integration of Field and Laboratory Data
• Formation of the Rio Grande Rift and Upper Mantle Seismic Wave Velocity Anomaly
• Localized Versus Distributed Deformation as a Control on the Evolution of Permeability in Anhydrite Rocks
• Major Rifts on Venus: Lithospheric Properties and Formation of Parga and Hecate Chasmata
• Mixing the mantle marble-cake: timescale constraints from Os isotopes
• Numerical Models of Lithosphere-Mantle Interaction at Continental Rift Zones
• Orogenic Plateaux Produce Sigmoidal River Profiles
• Postglacial slip rate increase on the Teton normal fault, northern Basin and Range Province, caused by melting of the Yellowstone ice cap and deglaciation of the Teton Range?
• Reanalysis of Geophysical Data With IODP Constraints at Atlantis Massif
• Response of the Intertropical Convergence Zone to Southern Hemisphere cooling during Ordovician glaciation
• Searching for Eustasy in Deglacial Sea Level Histories
• Stable isotopes in pedogenic calcite: Can the positive linear covariant trends be used to quantify paleo-evaporation rates?
• The Petrogenesis of the Unit 7/8 and 11/12 Chrome-spinel Seams of the Rum Eastern Layered Intrusion (NW Scotland) Re-evaluated
• The potential for carbon storage in UK peatlands
• The prognosis for carbon storage in northern peatlands - evidence from peatlands in the UK
• U-Series Disequilibria From the East Pacific Rise (9N, 10N and 11N): evidence for off-axis magmatism along fast spreading ridges?
• Vertical land displacements in Hokkaido, northern Japan
• A Three Dimensional Analysis of the Geometry and Kinematics of a Transfer Zone
• A calving law for ice sheet models; Investigating the role of surface melt on dynamics of Greenland outlet glaciers
• Active gas Venting at the Landward Limit of Hydrate Stability Offshore Svalbard
• Calibrating a Glaciological Model of the Greenland Ice Sheet From the Last Glacial Maximum to Present-day Using Field Observations of Relative sea Level and ice Extent
• Complex Isotope Mixing Arrays Arising From Upper Mantle Dynamics and Melting of a Veined Mantle Plume
• Constraining Greenland Ice Sheet Mass Balance in the Last Millennia Using High Resolution Sea-Level Data
• Crustal Anatexis by Upwelling Mantle Melts in the N.Atlantic Igneous Province: the Isle of Rum, NW Scotland.
• Crustal structure of Montserrat and Surrounding Area From Integrated Onshore, Ocean Bottom and Multichannel Reflection Seismic Data
• Detailed distribution and rapid degradation of small seamounts on the MAR axial volcanic ridge, 45°30'N
• Evidence for Footwall Rotation in an Oceanic Core Complex From IODP Core Samples Reoriented Using Borehole Wall Imagery
• Evidence for a heterogeneous astenosphere from intra-transform and seamount lavas
• Fluid Overpressure and Earthquake Triggering in Faulted Evaporitic Sequences
• Glacial Chronology over the Past 450 kyr Around the Margins of the Southern North Sea (UK and Netherlands) From Quartz Luminescence Dating
• Global Correlations of MORB Chemistry With Ocean Ridge Axial Depth: Fertile Mantle Compositional Control
• How Long is the Trigger? Olivine Diffusion Profiles Constraining Pre-Eruptive Triggering Times, Nea Kameni, Santorini, Greece.
• Improved Sub-Basalt Seismic Imagery. Can Outcrops in East Greenland Suggest a Solution?
• Interpreting Century-To-Decadal Scale Sea-Level Records From Greenland
• Life Cycle of Oceanic Core Complexes
• Lithological and Mechanical Control on the Base of the Crustal Seismogenic Zone: a Case-Study from the Northern Apennines of Italy
• Lithosphere Erosion and Crustal Growth in Subduction Zones: Insights from Initiation of the Nascent East Philippine Arc
• Lithosphere Thickness Control on the Extent and Pressure of Mantle Melting Beneath Intraplate Ocean Islands
• Magma source evolution beneath the Caribbean oceanic plateau: New insights from elemental and Sr-Nd-Pb-Hf isotopic studies of ODP Leg 165, Site 1001 basalts
• Marine Geophysical Investigations of Arctic and Antarctic margins: implications for paleoglaciology
• Marine geophysical evidence for former expansion and flow of the Greenland Ice Sheet across the northeast Greenland continental shelf
• Mid-Miocene Carbon Isotope Maximum: Marine Versus Terrestrial Carbon Burial
• Modelling sea-level data from China and Malay-Thai Peninsula to infer Holocene eustatic sea-level change
• Modelling the Glacial Isostatic Adjustment of Greenland on Millennial to Decadal Timescales
• Recent Inflexions in Proxy Records of Sea-Level Change and Their Possible Fingerprint
• Repeated ridge jumps associated with plume-ridge interaction and melt migration
• Seismic Constraints on the Structure of the Cape Verde Swell
• Seismic Faulting of Dolomite Rocks: Textures and Possible Slip Weakening Mechanisms
• Seismic Imaging Of The South Atlantic Ocean
• Seismic Velocity Structure of the Island of Montserrat From Reflection/Refraction Tomography
• Stream Nitrate Concentrations in a Small Catchment in South West England over a Period of 35 Years (1970-2005)
• Structural Precursors to Continental Break-Up; the Faroe Islands, NE Atlantic Margin
• Talc Formation Along Continental Low-Angle Normal Faults: Growth, Deformation, and Mechanical Consequences
• The Fluvial Flux of Nitrogen from Great Britain 1974 - 2005 in the context of the terrestrial nitrogen budget of Great Britain.
• The ICSD Method: Integrating Crystal Size Distributions (CSD) With Isotopic Microanalysis
• The Multi-annual carbon budget of a peat-covered catchment
• The Nature and Evolution of Fluid-Related Weakening Mechanisms Along a Continental Low-Angle Normal Fault: the Zuccale Fault, Elba Island, Italy
• The effectiveness of nitrate vulnerable zones for limiting surface water nitrate concentrations - the failure of nutrient input management.
• The potential for carbon storage in UK peatlands
• The production of black carbon during managed burning of UK peatlands: could managed burning of peatlands lead to enhanced carbon storage?
• Thermal Pressurization Induced by Coseismic Shear Heating Within Thermally Unstable Rocks
• Volcanic facies from 1D to 3D: Using Wireline Logs and Terrestrial Laser Scanninng to Characterise the Internal Architecture of Flood Basalt Provinces
• Volcano-Tectonic History of the Island of Montserrat, West Indies, From Seismic Reflection Profiles
• A Seismological Portrait of the Anomalous 1996 Bardarbunga Volcano, Iceland, Earthquake (Invited)
• Anatomy of an Axial Volcanic Ridge: The Mid-Atlantic Ridge at 45°N
• Basement inheritance controls on continental margin architecture: steep basement fabrics and segmented margins
• Carbon fluxes from restored peatlands - the carbon benefit of revegetation
• Changes in Sea Levels around the British Isles Revisited (Invited)
• Crustal structure and melt supply variability in the presence of oceanic core complex formation: The Mid-Atlantic Ridge at 13°N
• Evidence of long-term change in fluvial DOC composition - why is fluvial DOC increasing and is it having more impact on the atmosphere?
• Fault Lubrication and Earthquake Propagation in Thermally Unstable Rocks
• Faults, fault rocks and fractures in basalts: a macro- to micro-analysis of fault rock evolution on the NE Atlantic Margin
• Fracture network heterogeneity in continental lithosphere: An example from the Lewisian Gneiss Complex, NW Scotland
• Gas transport through magma near the percolation threshold (Invited)
• Ice sheet extent and early deglacial history of the southwestern sector of the Greenland Ice Sheet
• Interrogating coccolith calcite: paleoceanographic proxy data from nannofractions, foraminifera and single coccolith specimens
• Microearthquake Analysis Techniques For Geothermal Applications (Invited)
• Non-Plume Models For Intraplate Volcanism
• Post-seismic slip on the 6th April 2009 L'Aquila earthquake surface rupture, measured using a terrestrial laser scanner (tripod-mounted lidar)
• Reconstructing flood basalt lava flows using terrestrial laser scanning and GSI3D software
• Resolving Seismic Moment Tensors with Body-Wave Amplitude Ratios
• Seawater Os heterogeneity during the OAE 2 and across the Cenomanian-Turonian Boundary: Implications for global ocean paleocirculation
• Seismic Reflection Along the Path of the Mediterranean Undercurrent
• Seismic constraints on the flexural response of the lithosphere to loading at the Cape Verde Swell
• Slug pressurization in Strombolian eruptions: analytical and experimental investigation of the transition from passive to explosive degassing
• Small-scale sublithospheric convection reconciles geochemistry and geochronology of 'Superplume' volcanism in the western and south Pacific (Invited)
• The microstructural character and evolution of fault rocks from the SAFOD core and potential weakening mechanisms along the San Andreas Fault (Invited)
• The terrestrial nitrogen budget of the United Kingdom
• Towards 3D joint inversion of full tensor gravity, magnetotelluric and seismic refraction data
• Using in situ isotopic analyses of crystals to investigate the origins of layered intrusions
• What is the prognosis of nitrogen losses from UK soils?
• A 125 year long record of DOC flux from a major temperate catchment: land-use vs. climate control?
• A Cretaceous terrestrial isotope record: implications for correlation and determining the link between terrestrial and marine biotic events (Invited)
• A Mechanism for Shear-Thinning Rheology of Suspensions of Solid Particles
• A framework for 3D joint inversion of MT, gravity and seismic refraction data (Invited)
• Are ``Hot Spots'' Hot? - An Overview
• Cenozoic magmatism in Gangdese, southern Tibet: Records of collision and subduction between India and Asia
• Continental Crust Growth as a Result of Continental Collision: Ocean Crust Melting and Melt Preservation
• Crystal Transfer at Chaos Crags during Magma Mingling
• Deriving Fault Slip Histories From Cosmogenic Exposure Ages Along Bedrock Fault Scarps Using Synthetic And Natural Data
• Differentiation and source processes at Mt Pelée and The Quill; active volcanoes in the Lesser Antilles Arc
• Distinguishing mantle and crustal contributions in a continental arc volcano: Tatara-San Pedro, Chilean Andes
• Dynamics of retreating subduction: insights from numerical models
• Evidence for the thickening of the lithosphere beneath accretionary continental crust from the subsidence of intercontinental basins
• Hf-Nd isotope and trace element constraints on subduction inputs at island arcs: limitations of Hf anomalies as sediment input indicators
• High-resolution terrestrial GDGT data from the mid-Cretaceous: significant shifts in continental paleotemperatures (Invited)
• Interphase Misorientation - A Technique for Identifying Mimetic Lattice Preferred Orientation
• Investigating crustal contamination: a case study from the Bolivian Altiplano, Central Andes
• Lithological Controls on 3D Fold Geometry in Mechanically Layered Rocks
• Load support at the Cape Verde swell: seismic constraints on the flexural response of the lithosphere
• Marine osmium isotopic record of cherts across the Triassic-Jurassic boundary: implications for environmental change
• Metamorphic Controls on Relative Strength of Mafic and Felsic Rocks
• Modelling lithospheric ageing during subduction: Implications for the Izu-Bonin-Mariana trench migration
• New Insights into Diking Processes from High Resolution Bathymetry of Pillow Ridges on the Juan de Fuca and Gorda Ridges
• Non-stationarity in long hydrological time series: a new theoretical technique for detecting multiple changes in mean and variance
• Os-Hf isotopes of the ultrapotassic rocks in southern Tibet: Significant crustal input into the mantle source region
• Perspectives on Crystal Populations Versus Individual Crystals: Linking CSD, Diffusion Times, and Geochemistry to Determine Magma Histories
• Portrait of an Axial Volcanic Ridge: sidescan sonar and bathymetry at three resolutions
• Quantitative petrological constraints on the depth of the Lithosphere-Asthenosphere boundary and the implications for changes in cratonic lithosphere thickness through time
• Reconstructing the Growth History of Bubbles in Magma from Preserved Volatile Concentrations in Glass
• Rhenium - osmium heterogeneity of enriched mantle basalts explained by composition and behaviour of mantle-derived sulfides
• Seismology and Enhanced Geothermal Systems
• Small-scale convection induces temporal and spatial variability in Hawaiian plume volcanism (Invited)
• Sr isotopic microsampling of magmatic rocks; a review (Invited)
• Surface roughness of ancient seismic faults exhumed from 10 km depths (Gole Larghe Fault, Italian Alps) characterized over five orders of magnitude
• Teaching the Mantle Plumes Debate
• The 190Pt-186Os Decay System Applied to Dating Platinum-Group Element Mineralization in Layered Intrusions, Ophiolites and Detrital Deposits
• The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth
• The distribution of the Linzizong sequences along the Indo-Asian collision belt
• The influence of particle shape and volume fraction on the rheology of crystal-bearing magma
• The largest volcanic eruptions on Earth
• The microstructural character and evolution of fault rocks from SAFOD and potential weakening mechanisms along the San Andreas Fault
• The terrestrial nitrogen budget of the United Kingdom
• The use of very long term water quality records from the UK: gaining perspective on problems of nitrate and DOC (Invited)
• Understanding Crystal Populations; Looking Towards 3D Quantitative Analysis
• Widespread evidence for a late veneer on the terrestrial planets and planetisimals
• A reconsideration of marine strontium budgets using both stable (δ<SUP>88</SUP>Sr) and radiogenic (<SUP>87</SUP>Sr/<SUP>86</SUP>Sr) systems
• Are All Hyaloclastite Deposits Hyaloclastite Deposits? Field Characterisation in Different Subaqueous Environmental Settings
• Bubble, Burp, Bang! Self-organizing Cyclicity in Slug-driven Eruptions
• Characterising fracture systems within fractured crystalline reservoirs: the Lewisian Gneiss Complex, Scotland as an onshore analogue for the Clair Field basement
• Crossint - an interactive tool for the analysis of normal fault slip rates, using cross sectional data derived from terrestrial laser scan datasets
• Crustal structure and seismicity associated with seamount subduction: Preliminary results from the Tonga-Kermadec Trench - Louisville Ridge collision zone
• Crystal Recycling in the Steady-State System of the Active Stromboli Volcano: a 2.5 ka Story Inferred from In-Situ Sr-ISOTOPE and Trace-Element Data
• DOC fluxes from the UK - up to 194 monitoring sites over 125 years and from 0.1 km2 to 10000 km2
• Detailed study of an axial volcanic ridge using TOBI sidescan sonar and phase bathymetry
• Dy/Dy*; a tool for resolving petrogenetic processes from REE data
• Fault Zone Architecture and Permeability-Structure Evolution in Basalts: the Generation of Fluid-Flow Pathways in low Permeability Rocks
• Fire and Ice Revisited
• Hidden tectonics at slow-spreading ridges: distinguishing magmatic from tectonic spreading
• High Mg basalts and basaltic andesites from pyroxenite melts(?) in a continental arc: Tatara-San Pedro, Chilean Andes
• Induced Earthquakes: The Seismological State of the Art
• Lateral variations in the structure of the overriding and down-going plates in response to subduction of the Louisville Ridge seamount chain at the Tonga-Kermadec Trench
• Molybdenum Isotopes and Soil Processes
• Nitrate concentrations and fluxes in the River Thames, London UK 1868 to 2008: catchment-scale modelling of diffuse agricultural sources and groundwater response using the world's longest water quality time series
• Oceanic mantle rocks reveal evidence for an ancient, 1.2-1.3 Ga global melting event
• Os and HSE of the hot upper mantle beneath southern Tibet: Indian mantle affinity?
• Precise Timing and Elevation of the Mid-Holocene Highstand at Belitung Island, Indonesia, on the Sunda Shelf, from Coral Microatolls
• Quantitative monitoring of subsurface CO2 emplacement and leakage using muon tomography
• Slip zone structure and processes in seismogenic carbonate faults
• The Frictional Proprierties of Dolomite Gouges at Subseismic Slip Rates
• The Role of Reactivation and Fluid Pressure Cycling in The Development of Late Zeolite-bearing Faults and Fractures From The Adamello Batholith, Italy
• The Timing of Oceanic Mantle Depletion
• The terrestrial nitrogen budget of the Thames catchment, UK
• The total nitrogen budget of the UK- amounts, controls and prognosis
• Two Phases of Sulphide Saturation in Reunion Magmas: Evidence from Cumulates
• Unearthing the basement of the Central Andes: insights from crustal xenoliths
• Vesiculation and enclave formation at Chaos Crags
• Volatile Content of the Mid-ocean Ridge Mantle Inferred from Off-axis Seamounts and Intra-transform Lavas
• Wide-angle seismic reflections as direct indictors of partial melt beneath an andesite arc
• 3D joint inversion of complex geological structures: Example of a salt dome
• A New Approach To Characterizing The Holocene Slip History Of Active Normal Faults: An Integrated Study Using Terrestrial Laser Scanning, Ground Penetrating Radar, 36Cl Cosmogenic Exposure Dating And Field Analysis
• Along-arc geochemical and isotopic variations in Javanese volcanic rocks: 'crustal' versus 'source' contamination at the Sunda arc, Indonesia
• Are Axial Volcanic Ridges where all the (volcanic) action is?
• Changes in nitrate concentrations and loads in United Kingdom watersheds since 1868: Evidence for land use change as a dominant driver and ineffective mitigation
• Constraints on Fault Dynamic Weakening Mechanisms From Natural Slip Surfaces in Carbonate Faults
• Continental collision and slab break-off: modelling results and implications for topography, trench migration and magmatism
• Digital mapping of accommodating structures and deformation associated with the emplacement of high level magmatic intrusions, Henry Mountains, Utah
• Exploration of the Lesser Antilles arc signature in St Lucia using a multiscale analytical approach
• Exploring separated gas-magma flows in basaltic volcanoes using analogue experiments at a range of scales
• Field evidence for contrasting origins of ash pellets, coated ash pellets, and accretionary lapilli: implications for the vertical structure of density currents and atmospheric ash plumes
• Flexural characteristics of pre- and post-subduction lithosphere - the influence of large-scale plate loads
• From Muons to the Moon; the Role of Particle Physics and Lunar Tides in Monitoring Geostorage of Carbon Dioxide
• Joint inversion of 3-D seismic, gravimetric and magnetotelluric data for sub-basalt imaging in the Faroe-Shetland Basin
• Magnesium isotope variations in cratonic eclogites: origins and implications
• Modeled Differential Muon Flux Measurements for Monitoring Geological Storage of Carbon Dioxide
• Mt. Kinabalu, Borneo: Source and evolution of a multi-phased post-collisional I-Type granite
• Multiple seafloor spreading modes in the Mid-Cayman Spreading Centre
• Non-stationarity in long hydrological time series: cumulative sums, autocorrelation and temporal scale-shifting
• Petrogenesis of Syn-collision Plio-Quaternary Lavas in Northwest Armenia: Magma Generation in the Turkish-Armenian-Iranian Plateau
• Reconciling geophysical and geochemical observations to understand craton lithosphere architecture
• Slip distributions on active normal faults measured from Terrestrial Laser Scan (TLS) data and field mapping of geomorphic offsets: An example from L'Aquila, Italy, and implications for modeling seismic moment release
• Slow-Spreading Oceanic Crust Formed By Steady-State Axial Volcanic Ridges
• The Northern Kolbeinsey Ridge, North Atlantic: Excess volcanism and ridge relocations close to Jan Mayen
• The evolution of continental subduction: from slab detachment to delamination
• The geological manifestation of earthquake swarms: Evidence from the Adamello Batholith in the Southern Italian Alps
• The loss of DOC in transit through river catchments - impact on the atmosphere and understanding trends
• The relationships between topography, rates of extension, subduction and mantle dynamics in the actively-extending Italian Apennines
• The rheology of two-phase magmas
• The use of very long term water quality records from the UK: new insights and new methods
• Trench-parallel variations in Pacific and Indo-Australian crustal velocity structure due to Louisville Ridge seamount subduction
• Using Distant Sources in Local Seismic Tomography
• Volcanic ash aggregation: a new classification scheme
• A Global Study of Swath Bathymetry and the Changing Depth of the Seafloor with Time
• A Potential Field and Geomorphological Study of Monowai Volcano: Interplay Between Volcanism and Tectonics on the Tonga-Kermadec arc
• CO<SUB>2</SUB> Sequestration within Spent Oil Shale
• Complex frictional behaviour of clay-bearing carbonate faults revealed by integrated field and experimental investigation
• Craton stability and continental lithosphere dynamics during plume-plate interaction
• Crustal structure and seismicity associated with seamount subduction: A synthesis of results from the Tonga-Kermadec Trench - Louisville Ridge collision zone
• Detecting change in long hydrological time series: moving on from double-mass curves
• Discovery of an active shallow submarine silicic volcano in the northern Izu-Bonin Arc: volcanic structure and potential hazards of Oomurodashi Volcano (Invited)
• Dissolved water distribution in vesicular magmatic glass records both decompressive bubble growth and quench resorption
• Diverse styles of volcanism at slow-spreading ridges (Invited)
• Early Earth melt production in a subduction zone, a petrological model
• Evolution of Stiffness and Permeability in Fractures Subject to - and Mechanically-Activated Dissolution
• Fluid pressure and fault strength: insights from load-controlled experiments on carbonate-bearing rocks
• Four Flavours of Orogenic Plateau Magmatism: What's Melting Beneath the Turkish-Iranian Plateau?
• Friction at seismic slip rates: testing thermal weakening models experimentally
• Lower crustal assimilation in oceanic arcs: insights from an osmium isotopic study of the Lesser Antilles
• Magma chamber evolution: implication for the generation of continental crust: A case study in Kekeli batholith, North Qilian Orogenic Belt
• Mantle flow, volatiles, slab-surface temperatures and melting dynamics in the north Tonga Arc - Lau Backarc Basin
• Proto-Pacific OAE2 osmium isotope records revealed: global correlation and basin dynamics
• Structure and deformation of the Tonga-Kermadec subduction system in the Louisville Ridge pre-collision zone
• Sub-lithospheric small scale convection - a process for continental collision magmatism
• Subduction of Louisville Ridge seamounts: Effects on Tonga-Kermadec Trench and forearc morphology and seismic structure
• Understanding the fluvial loss of carbon from UK watersheds - implications for terrestrial carbon; greenhouse gases and water quality
• Using Distant Sources in Local Seismic Tomography
• Variability in Central American rainfall amount and seasonality over the past four centuries: evidence from a monthly resolved Belizean stalagmite
• West-to-east Moisture Transport Dynamics in the East Asian Monsoon
• Where is the Total Nitrogen accumulating in the Thames catchment (UK)?
• Conduit speed limit promotes formation of explosive `super slugs'
• Fractionation of Highly Siderophile Elements in Refertilized Mantle: Implications for the Os Isotope Composition of Basalts
• Hotspots in Hindsight
• How to Snowboard on Mars
• Maruyamaite, a new K-dominant tourmaline coexisting with diamond -an important accessory mineral in UHP rocks
• Origin of the 'Gabbro' Signature in Ocean Island Basalts: Constraints from Osmium Isotopic Ratios of Galapagos Basalts
• Testing the Consistency of Diffusion Modelling in Multiple Crystal Phases: A Case Study from the Bishop Tuff, California
• The Rheology of Three-Phase Basaltic Magma
• The Yellowstone 'hot spot' track results from migrating Basin Range extension
• Trace Element Geochemistry of Basaltic Tephra in Maar Cores; Implications for Centre Correlation, Field Evolution, and Mantle Source Characteristics of the Auckland Volcanic Field, New Zealand
• Volatile element content of the heterogeneous upper mantle
• When Do Complex Eruption Dynamics Matter? The Roles of Column Instability and Magma-water Interaction on Dispersal of Volcanic Ash
• When Is a Diffusion Profile Not a Diffusion Profile? the Importance of Initial State Assumptions in Diffusion Modelling
• Apatite: A New Tool For Understanding The Temporal Variability Of Magmatic Volatile Contents
• Beyond Brittle Deformation: Insights into Seismogenic Slip Processes from Natural and Experimental Faults
• Enhanced oxidative weathering in glaciated mountain catchments: A stabilising feedback on atmospheric carbon dioxide?
• Formation and Maintenance of a Viscous Plug in a Strombolian Volcanic Conduit
• Monitoring our Hazardous Planet with Sentinel-1 InSAR: Results and Prospects
• Mount Etna: 3-D and 4-D structure using seismic tomography
• New Insights into Trace Element Partitioning in Amphibole from Multiple Regression Analysis, with Application to the Magma Plumbing System of Mt. Lamington (Papua New Guinea)
• Satellite Measurements of Lava Extrusion Rate at Volcán Reventador, Ecuador
• Slugs and Plugs: the Role of Conduit Boundary Conditions in Shaping Strombolian Explosive Activity
• Tomography &amp; Geochemistry: Precision, Repeatability, Accuracy and Joint Interpretations
• Unravelling the magmatic processes behind zoned fall units on Ascension Island, South Atlantic
• 3D Micro-tomography on Aggregates from the 2014- 2015 Eruption of Hunga Tonga-Hunga Ha'apai Volcano
• 3D crustal structure beneath the Costa Rica Rift from seismic tomography: insight into magmatic activity
• An experimental investigation of earthquake rupture in granite at hydrothermal temperatures (20-160<SUP>o</SUP>C)
• Detailed Surface Rupture Geometry from the 2016 Amatrice Earthquake
• Effects of geothermal activity and primary production on molybdenum isotopes: Lake Mývatn, Iceland
• Frictional instability of rough faults in granite
• Geological carbon budget of the Mackenzie River Basin: New insight from the oxidation of rock-derived organic carbon
• Global Review of Induced and Triggered Earthquakes
• Global perspectives on oxidative weathering of organic carbon in sedimentary rocks
• Global warming and ocean acidification through halted weathering feedback during the Middle Eocene Climatic Optimum
• High resolution fault slip rate determination reveals temporal and spatial strain partitioning in Abruzzo, Italy
• Hot and Steamy Fractures in the Philippines: The Geological Characterization and Permeability Evaluation of Fractures in the Southern Negros Geothermal Field, Philippines
• InSAR observations of focused interseismic strain along the entire North Anatolian Fault: implications for seismic hazard assessment and the rheology of the lower crust
• Insight on fault segmentation, linkage and hazard from the 2016 M<SUB>w</SUB>6.2 Amatrice earthquake (central Italy)
• Investigation of post-seismic deformation resulting from the 24<SUP>th</SUP> August 2016 Central Italy Earthquake (M 6.2)
• LiCSAR: Tools for automated generation of Sentinel-1 frame interferograms
• Magmas on the Move: in situ 4D Experimental Investigation into the Rheology and Mobility of Three-Phase Magmas Using Ultra Fast X-ray Tomography
• Numerical Modelling of Trace Elements Behaviour in Deep Magmatic Processes
• Orogenic inheritance and continental breakup: Wilson Cycle-control on rift and passive margin evolution
• Osmium Stable Isotope Composition of Chondrites and Iron Meteorites: Implications for Planetary Core Formation
• Plate-scale measurement of interseismic strain from Sentinel-1
• Plutonic Xenoliths from Martinique and Statia: A Record of Differentiation Within the Plumbing Systems of the Lesser Antilles Volcanic Arc.
• Post-glacial mantle evolution in Southern Chile and the development of the Carrán-Los Venados volcanic field (40'20<SUP>o</SUP>S)
• Relocation and Seismicity of the aseismic central Iranian plateau
• Seasonal freeze-thaw cycles and iron mobilization from peat soils: role of organo-metallic complexes
• Strontium stable isotope behaviour accompanying basalt weathering
• Sulfide in the core and the Nd isotopic composition of the silicate Earth
• Systematic assessment of atmospheric uncertainties for InSAR data at volcanic arcs using large-scale atmospheric models: Application to the Cascade volcanoes, United States
• The Behaviour of Fe Stable Isotopes Accompanying Fluid Migration in Subducted Serpentinite from the Zermatt-Saas Ophiolite of the Swiss Alps
• The Deep Crust Magmatic Refinery, Part 1: A Coupled Thermodynamic and Two-phase Flow Model
• The Deep Crust Magmatic Refinery, Part 2 : The Magmatic Output of Numerical Models.
• The Flavour of Slab Fluids
• The dynamics of continental convergence in Iran
• The formation of Gullies by Dry Ice
• Time-dependent changes in magmatic and hydrothermal activity at the Costa Rica Rift recorded by variations in oceanic crustal structure
• Time-dependent seismic tomography: Application to the Coso geothermal system, California
• Titanium Isotopes Link the High 3He/4He Reservoir to Continent Formation
• Tracing Anthropogenic Osmium around Japan using the Osmium Isotopic Composition of Macroalgae
• Tracing oxidative weathering from the Andes to the lowland Amazon Basin using dissoved rhenium
• Understanding Fracturing and Alteration at ODP Borehole 504B: 3D Seismic Structure and Anisotropy of 5.9 Ma Oceanic Crust
• Velocity structure of the crust at 13°N on the Mid-Atlantic Ridge: implications for crustal accretion and oceanic core complex formation
• Volcanoes Distribution in Linear Segmentation of Mariana Arc
• Weakness of serpentine minerals revealed by friction experiments under low and high temperature conditions.
• Weathering Feedbacks and Atmospheric CO<SUB>2</SUB> during a Silurian Icehouse World: Insights from Os and Li Isotopes
• A New Paradigm for New Oceans
• A generalised model of secondary circulation for a wide range of geophysical flows from direct observations of natural turbidity currents
• An experimental overview of the seismic cycle
• Anatomy of a turbidity current: Concentration and grain size structure of a deep-sea flow revealed by multiple-frequency acoustic profilers
• Andean surface uplift constrained by radiogenic isotopes of arc lavas
• Axial crustal structure of the Costa Rica Rift: Implications for along-axis hydrothermal circulation
• Benthic Foraminifers identify the source of displaced sediment from a sediment density flow at 1840 m near the Seafloor Instrument Node of the Monterey Coordinated Canyon Experiment
• Breaking barriers and halting rupture: the 2016 Amatrice-Visso-Castelluccio earthquake sequence, central Italy
• COMET-LICSAR: Systematic Deformation Monitoring of Fault Zones and Volcanoes with the Sentinel-1 Constellation
• Commercial helium reserves, continental rifting and volcanism
• Determining the Extent of Hydrothermal Interaction on the Southern Costa Rica Rift Ridge Flank During the Past 8 Ma from Joint Inversion of Geophysical Data
• Direct Measurements of the Evolution and Impact of Sediment Density Flows as they Pass Through Monterey Submarine Canyon, Offshore California
• Distribution of magmatism in numerical models of delamination during continental collision
• Earthquake Nucleation Size: Evidence of Loading Rate Dependence in Laboratory Faults
• Earthquake rupture dynamics in poorly lithified sediments
• Evolution of Heat Flow with Age on the Southern Flank of the Costa Rica Rift
• First direct observations linking confined supercritical turbidity currents to their depositional architecture and facies characteristics
• Frictional behaviour and evolution of rough faults in limestone
• Full-Waveform Modelling of Seismic Wave Propagation and Scattering within Extrusive Basalt Sequences
• Geothermal heating in the Panama Basin and its impact on water mass transformation
• Go big or die out: Bifurcation and bimodality in submarine sediment flow behaviour
• Gradual or abrupt earthquake rupture initiation controlled by fault structure
• High resolution shallow co-seismic and post-seismic slip from the 2016 central Italy earthquake sequence captured using terrestrial laser scanning, structure from motion and low-cost near-field GNSS
• High-resolution surface velocity and strain rate mapping across the Alpine-Himalayan belt using InSAR and GNSS data
• How well do basic models describe the turbidity currents coming down Monterey and Congo Canyon?
• Hydro-fracture in the laboratory: matching diagnostic seismic signals to fracture networks
• Hypothesis Testing in Seismic Tomography
• Inferring the thermal structure of the Panama Basin by seismic attenuation
• Insights from field observations into controls on flow front speed in submarine sediment flows
• Linking turbidity current triggers to flow power, frequency and runout distances
• Lithospheric Controls on the Distribution of Volcanoes in Mariana Arc
• Localization, Weakening and Fluid-rock Coupling Mechanisms in Gypsum: Development and Initial Data From a New, Combined, Rotary Shear and Acoustic Emission Apparatus.
• Masuda's Sandstone Core Hydrate Dissociation Experiment Revisited
• Modelling the possible interaction between edge-driven convection and the Canary Islands mantle plume
• Multi-scale Fracture Patterns Associated with a Complex Anticline Structure: Insights from Field Outcrop Analogues of the Jebel Hafit Pericline, Al Ain-UAE
• New technological developments provide deep-sea sediment density flow insights: the Monterey Coordinated Canyon Experiment
• Not Just Rough Around the Edges: Fractal Properties of Exhumed Fault Surfaces in the Italian Apennines
• Novel Quantification of Sediment Concentration in Turbidity Currents Through in-situ Measurements of Conductivity and Temperature
• Organic Carbon Mobilisation Mechanisms: Evidence from Globally Distributed Stalagmite Records
• Percolation of isotopically heterogeneous interstitial melts in the crystal mush of the Rum layered intrusion, NW Scotland
• Porosity, Fracturing and Alteration of Young Oceanic Crust: New Seismic Analyses at Borehole 504B
• Quantifying the Journey of a Turbidity Current: How Water and Sediment Discharges Vary with Distance in Monterey Canyon
• Quivering on the brink: Common observations of turbidity current frequency and triggering in disparate settings
• Reconciling experimental and static-dynamic numerical estimations of seismic anisotropy in Alpine Fault mylonites
• Repeat Mapping in Upper Monterey Canyon Captures the Effect of Sediment Transport Events of Known Magnitude and Duration on the Seafloor Morphology
• Repeat Mapping in the Lower Monterey Submarine Canyon Sheds Light on Morphological Change During Discrete Sediment Density Flow Events
• Seabed Motion During Sediment Density Flows as Recorded by Displaced Man-Made Motion-Recording Boulders and a Heavy Instrument Platform
• The Stratigraphic Incompleteness of Submarine Channels
• The down canyon evolution of submarine sediment density flows
• The fate of carbonates along a subducting slab
• The record of mantle heterogeneity preserved in Earth's oceanic crust
• The transition from brittle cataclasis to viscous flow during the weakening of carbonate gouges sheared at seismic velocities recorded through the activity of acoustic emissions.
• There and back again: The life and death of magma permeability in volcanic conduits
• Triggering of frequent turbidity currents in Monterey Canyon and the role of antecedent conditioning
• Unravelling the Natural and Anthropogenic Drivers of North Atlantic Tropical Cyclone Track Position since the Little Ice Age
• VoiLA: A multidisciplinary study of Volatile recycling in the Lesser Antilles Arc
• Water in geodynamical models of mantle convection and plate tectonics
• Weak Serpentine-bearing Fault Zones: laboratory evidence and implications for the activity of of oceanic detachments
• A Fractal Future for Earthquake Slip Inversions
• A new module designed to study seismic attenuation in large displacement experimental faults
• Anatomy of dynamic slip in laboratory earthquakes at crustal conditions
• Characterising magmatic domains from a synthesis of global satellite radar measurements
• Coseismic Throw Variation Across Along-Strike Bends on Active Normal Faults: Implications for Displacement/Length Scaling of Earthquake Ruptures.
• Distributed Faulting in the Early Stages of Continental Rifting: New Evidence from the Zomba Graben in Southern Malawi
• Dry Ice and Granular Flows on Mars
• Dual control of fault intersections on stop-start rupture in the 2016 Central Italy seismic sequence
• Dyke intrusion between neighbouring arc-volcanoes responsible for 2017 unrest at Agung, Bali: insights from Sentinel-1 InSAR and 3D stress modelling
• Evolution of Heat Flow, Hydrothermal Circulation and Permeability with Age on the Southern Flank of the Costa Rica Rift
• Experiments on the interaction between sublimating carbon dioxide ice and granular substrate under Martian conditions and implications for araneiform formation
• Formative Controls on Dune-Scale Upstream-Migrating Bedforms in Submarine Channels
• Frictional Behaviour and Comminution of Sintered Glass Samples as an Analogue of Volcanic Rocks
• How surface topography of convergent margins depends on the deep slab geometry and kinematics: insights from numerical modelling.
• InSAR Observations of Long-term Extension in the Build-up to the January 2017 Eruption of Erta 'Ale Volcano, Afar, Ethiopia.
• Inter Tropical Convergence Zone Dynamics of the Neotropics During the Common Era
• Interactions between roughness, wear, normal stress and fault friction during simulated faulting in limestone
• Investigation of the Potential Respiratory Hazard of Combined Exposure to Volcanic Ash and Urban Pollutants in a Multicellular Human Lung Model
• Knickpoint Migration and Long-term Submarine Channel System Evolution within Bute Inlet, British Columbia, Canada
• Magmatic Intrusion and Its Interaction with a Volcano Centre in Main Ethiopian Rift
• Mixing and entrainment at the interface of lock-release gravity currents
• Morphodynamics of Knickpoints Active Turbidity Current Channels
• New Insight on the Rotation and Deep Crustal Structure of Java and the Lesser Sunda Islands Based on Arc Volcano Distribution
• Off-fault deformation and shallow slip deficit in the 2016 Norcia, Italy earthquake captured by differential terrestrial laser scanning and structure-from-motion
• Organic carbon sorting by turbidity currents: a Bouma Sequence for geochemists
• Rise and Burst of Overpressured Bubbles in a Particle-Rich Suspension: Consequences for Interpretation of Normal Activity at Stromboli Volcano, Italy.
• Satellite observations of volcanoes in the Asia-Pacific region and their potential for use in parametric insurance
• Shallow Mantle Counterflow Rather Than Deep-mantle Plumes Produces Linear Island Chains
• The Impact of Tasman Gateway Opening on Early Paleogene Climate and Oceans: New Results from IODP Expedition 369, Site U1514
• The architecture of seismic faults in poorly lithified sediments: implications for the energy budget of earthquake surface-rupture.
• The dominant control on submarine channel evolution revealed by new high-resolution time-lapse bathymetry
• Towards large-scale, InSAR-derived surface velocities and strain rates for the global tectonic belts
• Triggering dynamic slip instability on heterogeneous faults: model and experiment
• Understanding the Impact of In-Plume Ash-Gas Interactions Upon the Respiratory Hazard of Volcanic Ash
• Use of Social Media to Deliver Volcano-Hazards Information and Build Trust During the 2018 Kīlauea Crisis
• Viscous flow of nano-granular materials lubricates faults during earthquake propagation.
• Wave Ripple Development on Mixed Clay-sand Substrates: Effects of Clay Winnowing and Armouring
• A validated numerical model for the growth and resorption of bubbles in magma
• Ageing and Evolution of Oceanic Crust Formed by Magma-Rich and Magma-Poor Spreading
• Assessing Along-Axis Continuity of Oceanic Detachment Faults using microearthquakes near 13°N, Mid-Atlantic Ridge
• Automated methods for detecting volcanic deformation using Sentinel-1 InSAR time series
• Better, faster landslide detection from optical and radar satellite data
• Confidence Limits in Double-Epoch Time-Dependent Seismic Tomography
• Controlling factors on the shallow co-seismic slip at the Sumatra subduction zone megathrust
• Crustal fragmentation, magmatism, and the diachronous opening of the Norwegian-Greenland Sea
• Ductile deformation explains the physics of rock friction
• Exploring eruption dynamics in 3D; textural and geochemical analysis of archetypal Ocean Island eruptive deposits, Ascension Island, South Atlantic
• Fault Healing Controls the Spectrum of Slip Modes
• From laboratory to crustal scale seismic velocities on carbonates: insights from Apennines limestones
• High-TiO2 Basalts at Iceland and the North Atlantic Igneous Province
• How Is Sediment Transported through Submarine Channels and onto Lobes? New Insights from Turbidity Current Monitoring and Repeat Seafloor Mapping
• Insights Into Sediment Gravity Flows from Man-Made Motion-Recording Boulders.
• Investigating along- and across-arc crust and upper mantle anisotropy using OBS teleseismic and local shear-wave splitting with the VoiLA experiment
• Is Turbidity Current Activity Predictable?
• Knickpoints and Their Interactions with Crescentic Bedforms: the Building Blocks of Submarine Channel Systems
• Long fault, narrow damage: the Bilila-Mtakataka fault, Malawi
• Machine Learning Techniques for Detecting Slow, Sustained Deformation in InSAR Time Series.
• New combined nonparametric/parametric statistical analysis of fracture networks to unravel the evolution of fault zones: a study of the exhumed seismogenic Gole Larghe Fault Zone (Italian Southern Alps)
• Numerical Insights into the Formation and Stability of Cratons
• Origin of a public health concern: Cristobalite in ash from the May 18, 1980 Mt St Helens eruption
• P- and S-Wave Velocity Structure of Oceanic Core Complexes of the 13°N Segment of the Mid-Atlantic Ridge
• Pangaea dispersal and Large Igneous Provinces: Cause or effect?
• Processing out sideswipe - a case study from the slow spreading Mid-Atlantic Ridge at 13° N
• Rapid Detection of Earthquake-triggered Landslides with Satellite Radar Coherence
• Roughness, Off-fault Damage and Frictional Melt Distribution in an Exhumed Seismogenic Fault
• Structural inheritance and strain in the amagmatic southern Malawi rift
• Subduction sustaining subduction-transform-edge-propagator (STEP)-fault activity controls back-arc ridge jumps
• The Challenge of Providing Safe Water to All in a World of Climate Change
• The Greenland-Iceland Ridge is Continental
• The birth of bubbles by spinodal decomposition: Solving the tiny bubble paradox
• The decisive role of irregular continental margins on ophiolite creation and peridotite exhumation
• The performance of Harmony's two-dimensional sea-ice-drift observations
• They Don't Make 'Em Like That Anymore
• Towards InSAR- and GNSS-Derived Seismic Hazard Models for Anatolia and the Alpine-Himalaya Belt
• Tracing oxidative weathering of rock organic carbon in the Mackenzie River using rhenium isotopes
• Tracing the Release of Oxidizing Fluids during Subduction: Insights from Zoned Fe Isotope Measurements within Garnet
• Turbidity current evolution in Bute Inlet, British Colombia, Canada
• Upstream-migrating bedforms in the southern overbank area of the lower Taiwan Canyon, northeastern continental slope of the South China Sea
• Using temperature to constrain water entrainment of full-scale turbidity currents
• Velocity and Strain in the Afar Rift from Sentinel-1 InSAR
• Viscous Earthquakes
• Volcanica: a diamond open-access success story for volcano-based research
• Volcanically Initiated Shoaling of the Marine Calcite Compensation Depth during Oceanic Anoxic Event 2 ( 94 Ma)
• Watershed-scale Effects of Longleaf Pine Restoration on Water Yield and Carbon: A Paired Watershed and Modeling Approach
• What controls turbidity currents flow modes? New insights from direct measurements worldwide
• What is the contribution (if any) of off-fault damage to the earthquake energy budget?
• What's the damage? Multiscale analyses of attributes in fault damage zones - fracture length distributions, orientation scale transitions and network connectivity
• A bigger splat: The catastrophic geology of a 1.2 billion year old terrestrial megaclast, NW Scotland
• Changing rift physiography across blocks of laterally variable crustal strength - Insights from 3D numerical modelling
• Control of pore fluid pressure on rupture propagation: implications for induced seismicity
• Converging Research in the Earth, Health and Social Sciences with Humanitarian Practice for Community Protection in Volcanic Eruptions
• Detecting Ground Deformation in the Built Environment using Sparse Satellite InSAR data with a Convolutional Neural Network
• Diffuse vs Localized Deformation in Scaly Clays: insights from experimental reactivation of natural fabrics
• Earthquake clustering controlled by shear zone interaction: insights from cosmogenic dating and stress interactions for normal faults in central Italy
• Exploring Variability in a Global Compilation of Aseismic Afterslip Estimates
• Fault heterogeneities control self-arrested vs. run-away induced ruptures: implications for deep enhanced geothermal systems
• Incorporating geologic and geodetic data into probabilistic seismic hazard assessment of infrequent large magnitude earthquakes: insights from southern Malawi
• Insights into incipient rifting in thick lithosphere from a GNSS survey of the southern Malawi Rift
• Magma Mixing and the Contrasting Chemistries of Basalt at Most Spreading Ridges and the North Atlantic Igneous Province
• Reconciling observations of volcanic deformation and degassing from basaltic volcanoes
• Structural and frictional heterogeneities along natural faults and implications for fault slip behaviour
• The bioanalytical screening of deleterious organic compounds on volcanic ash: a pilot study using the AhR-CALUX assay
• The relationships between large tectonic earthquakes and explosive volcanic eruptions
• Using TanDEM-X Satellite Interferometry for Measuring Pyroclastic Flow Processes: Bulking and Run-out During the 2018 Eruption of Fuego Volcano, Guatemala
• Weakening mechanisms efficiency during seismic slip.

Linked Collaborating Authors [?]

• J. N. McElwaine
• Matthew Sylvest
• Thomas M. Mitchell