LE
Lisa Eberhard
University of Bremen, Utrecht University, University of Bayreuth, University of Bern
Research areas: Earth and Planetary Sciences · Geophysics · High-pressure geophysics and materials · Geological and Geochemical Analysis · earthquake and tectonic studies
0000-0002-3655-6364
Employment
- 2025 - Present
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Utrecht University Postdoctoral researcher2021 - 2025
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Universität Bayreuth Postdoctoral researcher2021 - 2021
Education
- 2017 - 2020
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Universität Bern MSc in Earth Sciences2015 - 2017
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Universität Bern BSc in Earth Sciences2012 - 2015
Projects & Funding
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Brucite vein network dehydration allows focused fluid flow Horizon 2020 research and innovation programme
Publications (21)
- Seismogenic Consequences of COH‐Fluid Rock Interactions in Ultramafic Fault Zones Insights From Carbonation‐Decarbonation Friction Experiments Save
- Coupling antigorite deformation and dehydration in high-pressure experiments Save
- Quantifying Vein Network Permeability in Dehydrated Serpentinites Using Thermodynamics and Generative AI Save
- Controls of focused fluid release in subduction zones: insights from experimental dehydration of brucite vein networks in serpentinite Save
- Faults inside out: 4DμCT on direct shear dehydrating gypsum experiments Save
- Imaging the textural evolution of gypsum through a metamorphic cycle Save
- Fault weakening due to CO2-fluid-rock interaction – evidence from deformation experiments of carbonated serpentinites Save
- Heterogeneous fluid release in subduction zones – evidence from experimental dehydration of brucite vein networks in serpentinite Save
- Hydro-mechanical-chemical modelling of dehydration during serpentinite deformation: Comparing laboratory and numerical experiments Save
- Experimental Evidence for Reaction‐Induced Weakening of (Carbonated) Serpentinite Fault Gouges Save
- Elastic stresses can form metamorphic fabrics Save
- Experimental constraints on the ferric Fe content and oxygen fugacity in subducted serpentinites Save
- Deuterium Content and Site Occupancy in Iron Sulfide at High Pressure and Temperature Determined Using In Situ Neutron Diffraction Measurements Save
- Experimental observation of antigorite dehydration triggered by shear stress at subduction zone pressure and temperature conditions Save
- Micro to Macroscale: the three-dimensional network characteristics of serpentinite dehydration veins Save
- Transdisciplinary connections help understand natural mechanisms behind major seismic ruptures Save
- Early release of H2O during subduction of carbonated ultramafic lithologies Save
- A New Method for Determining Fluid Flux at High Pressures Applied to the Dehydration of Serpentinites Save
- Experimental constraints on low temperature dehydration induced by mineral reactions in calcite-bearing ophicarbonates Save
- Multidimensional Analysis of Serpentinite Dehydration Networks and Implications for Volatile Flux in Subduction Zones Save