S. Han

    flowchart
    A[S. Han]
    AC["Associated Concepts (18)"]
    AW["Authored Works (12)"]
    CA["Linked Co-Authors (20)"]
    CI["Linked Collaborating Institutions (18)"]
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    AW== affil ==>CI
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    click AW "#authored-works"
    click CA "#co-authors"
    click CI "#collaborating-institutions"

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    NO["add outgoing edge"]
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ORCiD

https://orcid.org/0000-0002-2904-3659

OpenAlex ID

https://openalex.org/A5077926083 (API record)

Associated Concepts [?]

• Biology
• Geology
• Paleontology
• Seismology
• Physics
• Tectonics
• Geography
• Subduction
• Engineering
• Oceanography
• Geophysics
• Geochemistry
• Materials science
• Chemistry
• Composite material
• Petrology
• Organic chemistry
• Medicine

Authored Works

sorted by decreasing year, and then by display-name

• Sediment Subduction along the Cascadia Subduction Zone Constrained by New Active Source Seismic Imaging from the CASIE21 Experiment
• Northern Cascadia Subduction Termination and Plate Boundary Amplitude Variations from Marine Seismic Data
• New Observations of Plate Interface Depth and Geometry at the Offshore Cascadia Subduction Zone from the CAscadia Seismic Imaging Experiment 2021 (CASIE21) and Comparisons with Existing Plate Depth Models.
• Massive Submarine Landslides Imaged Offshore Southern Oregon
• Low Permeability Faults Inhibit Fluid Expulsion from the Northern Hikurangi Subduction Margin
• Investigation of a bottom-simulating reflector at the Hikurangi subduction margin by means of 3D full-waveform inversion
• Initial Active-Source Vp Tomography Results for CASIE21 Experiment Line PD12 Offshore Northwestern Oregon, and a Comparison with Nearby Land-Based Receiver Functions
• Fluid flow within the shallow forearc of the Cascadia Subduction Zone: Seismic imaging, high-resolution ROV mapping, and gas/fluid geochemistry
• CASIE21-OBS: Acquisition of a Controlled-Source Marine Wide-Angle Seismic Refraction/Reflection Dataset Across the Cascadia Margin
• A new plate boundary born as another dies: The influence of the Nootka Fault Zone segmenting subduction processes along the northern Cascadia margin
• Incoming sediment properties at the Cascadia subduction zone constrained by active source seismic data
• Deformation of a trench slope basin above the location of shallow slow earthquakes at the Hikurangi subduction margin

Linked Co-Authors

• A. Bécel
• A. F. Arnulf
• Anne M. Tréhu
• B. Boston
• D. Lizarralde
• Dan Barker
• Gregory F. Moore
• Hanchao Jian
• J. P. Canales
• M. R. Nedimović
• Michael Everett Mann
• Michelle K. Lee
• N. L. Bangs
• Nathaniel C. Miller
• Nathaniel J. Buck
• Ryuta Arai
• S. G. Merle
• Shuichi Kodaira
• Tamara Baumberger
• Tanner Acquisto

Linked Collaborating Institutions

• Brown University, Rhode Island
• Columbia University, New York
• Dalhousie University, Canada
• Geological and Nuclear Science Ltd, New Zealand
• Imperial College, London
• Japan Marine Science and Technology Center
• Lamont-Doherty Earth Observatory
• NOAA Pacific Marine Environmental Laboratory
• National Institute of Water and Atmospheric Research, New Zealand
• Oregon State University, Corvallis
• Peking University, China
• U.S. Geological Survey, Woods Hole
• University of Hawaii, Manoa
• University of Texas, Austin
• University of Texas, Austin, Department of Geological Sciences
• University of Washington, Seattle
• Woods Hole Oceanographic Institute, Massachusetts
• Yokohama National University, Japan

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