ML
Mingqi Liu
École Normale Supérieure - PSL, Texas A&M University, ETH Zurich, Chinese Academy of Geological Sciences, University of Southern California
Research areas: Earth and Planetary Sciences · Geophysics · Geological and Geophysical Studies · High-pressure geophysics and materials · Geological and Geochemical Analysis
0000-0003-4488-4824
Employment
- 2026 - Present
- 2025 - 2026
- 2023 - 2025
Education
- 2018 - 2022
- 2015 - 2018
Projects & Funding
-
Numerical models of seismic swarms at oceanic transform faults Swiss National Science Foundation2023 - 2025
Publications (16)
- OBS Data Mining Reveals Seismic Structure and Dynamics of the Oceanic Blanco Transform Fault, Northeast Pacific Save
- Dynamic segmentation of the Sagaing fault Save
- Deciphering grain size reduction as a driver of Mid-lithosphere discontinuity formation Save
- Large megathrust earthquakes in cold mantle wedge corners under lawsonite blueschist facies Save
- Role of hydrothermal alteration and thermally activated healing on earthquake dynamics along oceanic transform faults Save
- The Effect of Brittle‐Ductile Weakening on the Formation of Faulting Patterns at Mid‐Ocean Ridges Save
- Vertical tearing of subducting plates controlled by geometry and rheology of oceanic plates Save
- Reply to: Increase of P-wave velocity due to melt in the mantle at the Gakkel Ridge Save
- Forced Subduction Initiation Near Spreading Centers: Effects of Brittle‐Ductile Damage Save
- The effect of brittle-ductile weakening on the formation of tectonic patterns at mid-ocean ridges Save
- Low-degree mantle melting controls the deep seismicity and explosive volcanism of the Gakkel Ridge Save
- Self-organization of magma supply controls crustal thickness variation and tectonic pattern along melt-poor mid-ocean ridges Save
- Dynamics of thinning and destruction of the continental cratonic lithosphere: Numerical modeling Save
- Subduction Mode Selection During Slab and Mantle Transition Zone Interaction: Numerical Modeling Save
- Diapir versus along-channel ascent of crustal material during plate convergence: Constrained by the thermal structure of subduction zones Save
- Material transportation and fluid-melt activity in the subduction channel: Numerical modeling Save