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Upper Mantle Heterogeneity and Weak Subduction Boundaries Control Crustal Stress in the Korean Peninsula
Most earthquakes occur at plate boundaries, but some also strike within stable continental interiors. Although dominant causes of such …
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Upper Mantle Heterogeneity and Weak Subduction Boundaries Control Crustal Stress in the Korean Peninsula
Continental rifts losing driving forces can still complete breakup
The complex evolution of continental rift systems results from the intricate interplay of external driving forces and the rift system’s …
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Continental rifts losing driving forces can still complete breakup
Viscoelastic modelling reveals correlation between GNSS-derived deformation rates after the 2011 Tohoku-Oki earthquake and lithospheric thickness in the southern Korean Peninsula
The 2011 Tohoku-Oki earthquake caused significant post-seismic (PS) deformations in a broad region in East Asia including the southern …
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Viscoelastic modelling reveals correlation between GNSS-derived deformation rates after the 2011 Tohoku-Oki earthquake and lithospheric thickness in the southern Korean Peninsula
Do Subducted Seamounts Act as Weak Asperities?
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Do Subducted Seamounts Act as Weak Asperities?
Holocene relative sea-level changes on the southern east coast of the Yellow Sea
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A Thin Elastic Plate Model for Thermally Contracting Young Oceanic Lithosphere: Insights From Comparison With Modern Seafloor Observations
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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
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Early Holocene relative sea-level changes on the central east coast of the Yellow Sea
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Tectonophysics Perspectives on Integrated, Coordinated, Open, Networked (ICON) Science
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What comes first: The fault or the ductile shear zone?
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