Eunseo Choi

Latest

Do Subducted Seamounts Act as Weak Asperities?
Holocene relative sea-level changes on the southern east coast of the Yellow Sea
A Thin Elastic Plate Model for Thermally Contracting Young Oceanic Lithosphere: Insights From Comparison With Modern Seafloor Observations
Crustal and Uppermost Mantle Structures Imaged by Teleseismic P-wave Travel-time Tomography Beneath the Southeastern Korean Peninsula: Implications for a Hydrothermal System Controlled by the Thermally Modified Lithosphere
Early Holocene relative sea-level changes on the central east coast of the Yellow Sea
Tectonophysics Perspectives on Integrated, Coordinated, Open, Networked (ICON) Science
What comes first: The fault or the ductile shear zone?
Contributions from lithospheric and upper-mantle heterogeneities to upper crustal seismicity in the Korean Peninsula
Seismicity in the central and southeastern United States due to upper mantle heterogeneities
Persistent fine-scale fault structure and rupture development: A new twist in the Parkfield, California, story
Effects of Preexisting Structures on the Seismicity of the Charlevoix Seismic Zone
Whitepaper Reporting Outcomes from NSF-Sponsored Workshop: CTSP: Coupling of Tectonic and Surface Processes, April 25–27, 2018; Boulder CO
Effects of axially variable diking rates on faulting at slow spreading mid-ocean ridges
Semi-brittle rheology and ice dynamics in DynEarthSol3D
Prediction of ground motion and dynamic stress change in Baekdusan (Changbaishan) volcano caused by a North Korean nuclear explosion
Making Coulomb angle-oriented shear bands in numerical tectonic models
Accelerating DynEarthSol3D on tightly coupled CPU–GPU heterogeneous processors
Modes of continental extension in a crustal wedge
Spatial arrangement of décollements as a control on the development of thrust faults
Using core complex geometry to constrain fault strength
A novel method for predicting fracture in floating ice
Constraints on the strength of faults from the geometry of rider blocks in continental and oceanic core complexes
One-sided transform basins and "inverted curtains": Implications for releasing bends along strike-slip faults