University of Michigan, Department of Geological Sciences

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    I[University of Michigan, Department of Geological Sciences]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (143)"]
    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 [?]

A11083

Abbreviation [?]

Dep Geo Sci

Parent Institutions [?]

• University of Michigan

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• A Modified SVAT Model That Links the Geothermal Climate Signal to Land-Surface Processes
• Elasticity of (Mg<SUB>1-x</SUB>,Fe<SUB>x</SUB>)SiO<SUB>3</SUB>- Perovskite at High Pressures
• GeoWall: Stereo Projection Systems Designed for Earth Science Classrooms
• Isotopic Studies of Gypsum in the Macquarie Island Ophiolite: Tracing Hydrothermal Reactions
• Neogene Biogenic Sedimentation Records from the South China Sea
• Oceanic Versus Continental Strike-Slip Earthquakes: a Case for the "W" Model
• Permian Paleomagnetism of Eastern Kazakhstan: Implications Concerning the Amalgamation of Eurasia
• Ridge-Flank Hydrothermal Circulation is not a Cure for the Imbalance in Oceanic Sr-Isotope Budgets
• Water in Planets: Dissociation of H<SUB>2</SUB>O at High Pressures and Temperatures to a New Form of Oxygen
• Characterization of Martian Rock Shape for MER Airbag Drop Tests
• Correlation and Astronomical Calibration of Pacific Sediments From ODP Leg 199
• Incorporation of hydrogen in stishovite: a first principles investigation
• Lithospheric Mantle Evolution Beneath the Bering Sea Volcanic Province: An Isotopic and Trace Element Study of Peridotite Xenoliths and Their Host Lavas
• Provenance of Atlantic Surface Sediment Based on Sr and Nd Radiogenic Isotopes
• The Paleogene Intertropical Convergence Zone
• A review of palaeoproductivity records from the N Pacific: The end of the iron hypothesis?
• Carbon and Nitrogen Stable Isotope Systematics in Three Mid-Pleistocene Sapropels from ODP Site 974 in the Tyrrhenian Basin
• Conductive Transport of Annual Temperature Signals in Variable Subsurface Media and Regional Analyses of Seasonal Decoupling Between Air and Ground Surface Temperatures
• Downcore Contrasts in the Provenance of Cenozoic Pelagic and Hemipelagic Sediment, Central North Pacific: Deep Ocean vs. Near-Continental Margin Sites
• How Deformed are Weakly Deformed Rocks? Insights From Magnetic Anisotropy
• Hydrothermal Alteration of the Lower Oceanic Crust: Sr Isotopic Constraints from the CCSP CY-4 Drill Hole, Troodos Ophiolite, Cyprus
• Iceland, the Scotian Basin, and the Farallon Slab: Dynamic Topography of the North Atlantic
• Implications From a new Continuous Astronomically Calibrated Geological Time Scale Back to ∼ 42 Myrs
• Quantitative Prograde P-T Paths From Inclusion Assemblages in Eclogitic Garnets
• Strontium and Oxygen Isotopic Profiles Through a Complete Sequence of Oceanic Crust Exposed on Macquarie Island
• A Mechanism For Amplifying Obliquity Forcing In Low-Latitude Oceans During The Pleistocene
• Dense layer entrainment and structure of mantle plumes
• Long-Term Glacial Erosion Rates and Pre-Glacial Topography in Southwest British Columbia
• Mercury Isotope Variations in Hydrothermal Ore Deposits
• New Constraints on the Erosion History of the Andean Plateau Inferred From Detrital Thermochronology Across the Northern Bolivian Thrust Belt
• Numerical modeling of noble gas recycling into the mantle
• Paleomagnetism Indicates Mid-Miocene Clockwise Rotation of the NE Tibetan Plateau
• Rapid, Coherent Apparent Polar Wander in the Terminal Neoproterozoic - Early Cambrian?
• Solubility of hydrogen and aluminum in CaSiO<SUB>3</SUB>-perovskite and the partitioning of water among silicates in the lower mantle
• Sr, Nd, Pb and Hf Isotopic Compositions of Late Cenozoic Alkali Basalts in South Korea: Evidence for Mixing Between the Two Dominant Asthenospheric Mantle Domains beneath East Asia
• Thallium Isotope Constraints on Hydrothermal Water Fluxes at Mid-Ocean Ridge Axes and Flanks
• A Cautionary Tale About Vertical-Axis Rotations, or How to Recognize an Orocline When You See One?
• A Multiple Proxy and Modeling Study of Cretaceous Upper Ocean Temperatures and Atmospheric Carbon Dioxide Concentrations From Tropical Atlantic Sediments
• Basement Sill of the Jurassic Ferrar Large Igneous Province, Antarctica: Constraints from its PGE Abundance Patterns on Magma Source Characteristics and Crystallization Processes
• Diffusion of Water in Silicate Melts
• Heat Budget of the World Continents Over the Past 154 Years
• Paleomagnetic Results From the Pleistocene Sediments of Lomonosov Ridge, Central Artic Ocean, IODP Leg 302
• Small-scale modal layering in the Dais section of the Basement Sill, Ferrar Province, Antarctica
• Age Uncertainties, Topography, Exhumation Pathway, and the Interpretation of Erosion Rates and Exhumation Kinematics from Thermochronometer Age-Elevation Data
• Constraints on Titanite Acitvity in the System CaTiSiO4O-CaAlSiO4F: Implications for Thermobarometry in Metamorphic Rocks
• Equation of State, Dynamics, Electronic and Atomic Structure of Diopside Liquid at High Pressure
• Hydrological changes during the Late-glacial times in northern Brazil inferred from sediments of Caço Lake.
• In Situ Alteration of Isotopic and Molecular Compositions of Organic Matter in Lake Erie Sediment Over a Two-Decade Interval
• Influence of Active Mantle Upwelling and Continental Roots for Driving Plate Motions
• Influence of groundwater flow on thermochronometer ages and exhumation rates: Insights from the Nepalese Himalaya
• Mantle-lithosphere interaction beneath the Yellowstone-Snake River province
• Paleomagnetism of the Neogene Jiuxi Basin, Hexi Corridor, China: implications for a non- rigid deformation mechanism?
• Salinity of the Early and Middle Eocene Arctic Ocean From Oxygen Isotope Analysis of Fish Bone Carbonate
• Stability of hcp phase and temperature variation of axial ratio of iron near Earth-core conditions
• Structure and Physical Properties of Mg2SiO4 Melt at Mantle Pressures and Temperatures
• Subcontinental-Scale Crustal Velocity Changes Along the Pacific-North America Transform Plate Boundary From BARGEN GPS Data
• Surface Temperature Reconstructions for the Last Five Centuries From Borehole Temperature Profiles
• Temporal and Spatial Variations in Erosion from Multiple Geochronometers: Wasatch Mountains, Utah
• The Amphibole-Bearing Chondrite Meteorite LAP04840: Metamorphism and `Tectonics' in a Hydrous Asteroid
• The role of gravitational potential energy in the Martian lithospheric stress field
• Why do Slabs Disappear in the Lower Mantle?
• A Field Test of Noble Gas Temperature Systematics from an Instrumented Monitoring Well: Implications for Gas Transport in the Capillary Fringe
• A New Stable Isotope Record From the Subantarctic Southeastern Pacific
• Determination of Volcanostratigraphy of ODP/IODP Hole 1256D: Qualitative and Quantitative Core-Log Integration
• Dufek Layered Mafic Intrusion and Basement Sill, Antarctica: Constraints on their Magma Sources Based on PGE Abundance Patterns, Nd-Sr-Pb Isotopic Ratios and Trace Element Modeling
• Influence of topographic evolution and faulting on detrital thermochronometer ages: Application to the Nepalese Himalaya
• Investigation of site-dependent GPS errors and monument stability using a short-baseline network of braced monuments
• LectureTools: An Open Source Technology to Promote Student Inquiry
• Lithium and Oxygen Isotopic Composition of the Oceanic Crust formed at a Superfast Spreading Ridge, Hole 1256D
• Mass Dependent Fractionation of Hg Isotopes in Source Rocks, Mineral Deposits and Spring Waters of the California Coast Ranges, USA
• Not all Primordial Noble Gas Signatures are Associated with OIBs and Mantle Plumes - Mantle Heterogeneity, Primordial Shallow Sources and a Solar-like He, Ne Signature in an Ancient North American Craton
• Self-Consistent Thermodynamic Description of Silicate Liquids
• Simulation of Modern and Cretaceous δ18O With a Global Ocean-Atmosphere General Circulation Model
• Temporal and spatial paleoproductivity patterns associated with Eastern Mediterranean sapropels: paleoceanographic significance.
• The Aeolian Volcanic Arc: New Insights From Subduction Zone Thermal Models and Mineral Solubility Scaling Relationships
• The Biogeochemical Dynamics of a Large-lake Ecosystem and Past Environmental Changes Recorded by a Sediment Core From Lake Erie, 1900-2003
• Using a New Multi-Discipline Approach to Predict Seismic Tomography from Geodynamical Models of Mantle Convection
• What Comes Around Goes Around: Mantle Convection and the Meaning of Mantle Isochrons
• A Community Benchmark for 2D Cartesian Compressible Convection
• Constraints on the Rates and Timing of Exhumation of the Greater Caucasus from Low- Temperature Thermochronology
• Effects of landsliding, faulting and topographic evolution on detrital thermochronometers
• Evidence for the Involvement of Medium- to High- Pressure Fractionation Processes in the Origin of Marie Byrd Land Pantellerites, West Antarctic Rift System.
• Extrustion vs. convergence? Two-phase late Tertiary growth of the Laji-Jishi Shan, NE Tibet
• Interseismic Deformation and the Mechanical Behavior of Megathrusts: Transient Postseismic Creep, Stress Shadows, and Megathrust Rheology
• Investigating the Causes of Variability in the Intensity of Hydrothermal Alteration of Ocean Crust Formed at Intermediate to Fast Spreading Rates
• Isolation and characterization of ancient hydrocarbon biomarkers from crystalline minerals
• Late Pliocene Changes in Abyssal Southern Ocean Ventilation: New Insights from the Subantarctic Pacific
• Peat Plant-Wax n-Alkane D/H Ratios Document Early Holocene Arrival of Indian Ocean Monsoon in Southern China
• Stable Spin and Magnetic Arrangements in Fe2O3 Post-Perovskite
• Structure and composition of the San Andreas Fault in central California: Recent results from SAFOD sample analyses
• Tracing a past thermal event by using atmospheric noble gases dissolved in deep Michigan Basin brines
• What Controls Subduction Earthquake Size and Occurrence?
• Fault Slip Distribution of the Mw 7.9 Wenchuan Earthquake Estimated from GPS and ALOS/PALSAR Measurements
• Hydrological variability for the last two millennia: palynological and organic proxies extracted from lacustrine sediments of Lake Dahu, northeastern subtropical Taiwan
• Mmax and Lithospheric Structure in Central and Eastern North America
• Post-Pliocene localization of Arabia-Eurasia shortening in the Greater Caucasus and Kura fold-thrust belt (Invited)
• Upwelling Record of the Last 3500 years in Santa Barbara Basin, California
• Arc Basalt Simulator version 3: Spreadsheet mass balance for exploring on element behavior between subducted slab, mantle wedge, and magma
• Climate controls on precipitation δ18O along the Andes
• Degassing-Induced Crystallization of Plagioclase in Hydrous Rhyolite Liquids: Evidence from Obsidian Samples from the Mexican and Cascades Volcanic Arcs
• Empirical test of an illite/muscovite 40Ar/39Ar thermochronometer
• From geodesy to geological, similar slip rates at different time scales: The Dead Sea Fault example (Invited)
• Persistence of Coseismic Rupture Asperities as Inferred from Interseismic Geodetic Observations from Northeastern Japan
• Seismic detection of post-perovskite at the core-mantle boundary
• The fabric and compaction of mudstones in the Gulf of Mexico
• The puzzling late Precambrian paleoposition of Laurentia: new insights from preliminary paleomagnetism of the Sainte-Sophie diabase dyke swarm, Quebec
• Time series and MinTS analysis of strain accumulation along the Haiyuan fault (Gansu, China) over the 2003-2010 period, from ENVISAT InSAR data
• Toward the Cenozoic Megasplice - high-resolution XRF core scanning data and improved composite records from IODP Expedition 320: implications for fine scale paleoceanography (Invited)
• Tropical cyclone activity and western North Atlantic stratification over the last millennia and potential connections (Invited)
• Utilizing Thermal &amp; Thermo-Chemical Mantle Circulation Models to Constrain the Origin of Earth's Lower Mantle Seismic Signature
• Variability in P-T paths in subducting mantle and crust, and its control on the locations of intraslab earthquakes (Invited)
• Wedge deformation and erosional exhumation in the Spanish Pyrenees: erosion rates track deformation
• What do Westerly Wind Reconstructions from Fiordland, New Zealand, say about Southern Hemisphere Paleoclimatic Mechanisms?
• A Bayesian Analysis of the Post-seismic Deformation of the Great 11 March 2011 Tohoku-Oki (Mw 9.0) Earthquake: Implications for Future Earthquake Occurrence
• A geodetic view of the 2011 Mw 9.0 Tohoku-Oki, Japan earthquake
• Carbon Content of the Core through New Windows on the Earth's Interior
• Chemical modifications of subducted crust and sediments beneath convergent plate margins and the fate of extracted liquids and residual solids: examinations using ABS ver.4 numerical model
• Direct Measurement of Recoil Effects on Ar-Ar Standards
• Does post-perovskite exist in the lowermost mantle? A statistical interpretation of seismic observations
• Earthquakes with anomalously steep dip in the source region of the 2011 Tohoku-Oki earthquake - Possible indicators for enhanced plate coupling
• Ediacaran paleomagnetic results from feeder dikes of the Catoctin Formation
• Hg Isotopes as Indicators of Paleoceanographic Change in the Arctic Ocean (55 Ma to Present)
• Isotopically Light Organic Carbon in Phanerozoic Black Shales: Diagenetic, Source, or Environmental Signal?
• Limits to Reconstructing Paleotopography From Thermochronometer Data
• Metamorphic devolatilization in subduction zones: thermal, dynamic and thermodynamic modeling
• Neogene rotations in the Jiuquan Basin, Hexi Corridor, China
• No evidence for a deglacial intermediate water Δ<SUP>14</SUP>C anomaly in the SW Atlantic
• Organic Carbon Accumulation during the Holocene in the Southeastern Brazilian Shelf: its Paleoceanographic Significance
• Organic Geochemical Characterization of Mid-Cretaceous Black Shales from ODP Site 1276 in the Newfoundland Basin
• Paleozoic ice sheet inception; a study of paleogeographic sensitivity
• Rapid terrestrial core formation from in situ X-ray computed microtomography
• Reconciling Dynamic and Seismic Mantle Models: The Role of Chemical Heterogeneity
• Rheological control in subduction zones: slab dynamics, fluid flow and seismic anisotropy
• Temperature Dependent Mössbauer Spectra of Aluminous Perovskite and Implications for the Earth's Lower Mantle
• Testing The Noble Gas Paleothermometer With A Year-long Study Of Groundwater Noble Gases In An Instrumented Monitoring Well
• The Role of Slab Return Flow Associated with Flat Slab Subduction in Driving the Laramide Orogeny
• Can lower mantle plumes be located using seismic tomography and transition zone topography?
• Increased storminess during MIS3 altered the late Quaternary basin-scale weathering, erosion, and deposition in Nahal Yael, hyperarid Negev, Israel
• Influence of carbon on physics and chemistry of iron and experimental constraints on carbon content of Earth's core
• Linking foraminiferal proxy records to the instrumental temperature record over the last 200 years in Santa Barbara Basin, California
• Metamorphic dehydration reactions control the location of intermediate-depth seismicity
• "Invar"-like behavior in compressed Fe<SUB>7</SUB>C<SUB>3</SUB> with implication for deep carbon cycle
• The Origins of Seismic Heterogeneities in the Lower Mantle: Insights from Mineral Physics

Linked Collaborating Authors [?]

• M. Arnaboldi
• P. Elósegui