Data publications found:
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Data for coupled brittle-viscous deformation of folded olivine veins in metaserpentinite: implications for slow slip and tremor
Austin Arias
2026
We documented the microstructural and geochemical characteristics of partially dehydrated and deformed metaserpentinite rocks from Erro-Tobbio, Voltri Massif, Italy. A thin section was prepared from a hand specimen taken from Erro-Tobbio. The thin section contains a folded olivine vein...
SWELliNG (Sulphates With Expansion: the roLe of New crystals’ Growth) and SWELliNG_2 (Sulphates With Expansion: voLume and phase chaNGes over long periods) - Excite projects
Chiara Caselle | Laurenz Schröer
2026
Each folder contains a stack of .tiff files achieved after reconstructing a µCT scan. The scans were performed as part of the SWELLiNG and SWELLiNG2 project (Excite Network). The main purpose of the performed experiment was to measure the changes in volume and observe the changes in the...
Data for Generative AI Modeling of Serpentinte Dehydration Veins in Subduction Zones
Austin Arias
2026
We used hand specimens of Erro-Tobbio meta-serpentinite (ET-MS) and outcrop surface images of olivine dehydration veins to train generative models to generate unique and varied dehydration vein network structures. These models coupled with thermodynamic calculations allowed us to predict...
Data for Generative AI Modeling of Serpentinte Dehydration Veins in Subduction Zones
Austin Arias
2026
We used hand specimens of Erro-Tobbio meta-serpentinite (ET-MS) and outcrop surface images of olivine dehydration veins to train generative models to generate unique and varied dehydration vein network structures. These models coupled with thermodynamic calculations allowed us to predict...
Data for Generative AI Modeling of Serpentinte Dehydration Veins in Subduction Zones
Austin Arias
2025
We used hand specimens of Erro-Tobbio meta-serpentinite (ET-MS) and outcrop surface images of olivine dehydration veins to train generative models to generate unique and varied dehydration vein network structures. These models coupled with thermodynamic calculations allowed us to predict...
Evaluating Self-Healing on Mortars by Coupling Water Permeability Assessments to X-ray Micro-Computed Tomography
Franco Grosso Giordano
2024
This dataset contains 18 reconstructed Micro-computed tomography (µCT) scans. These scans belong to nine samples (50 x 45 mm) and the reconstructed images from these scans represent a 3D volume of cracked lime mortar. Of each sample one scan was taken before (Day 0) and one scan after 28 days...
Data Supplement to Erosion by CO2 driven flows on Mars
Lonneke Roelofs
2025
The data presented and described here is a supplement to the following manuscript: Roelofs, L., Conway, S.J., van Dam, B., van Eijk, A., Merrison, J.P., Iversen, J.J., Markies, H., van Maarseveen, M., de Haas, T. - Flow dynamics and volume growth during erosion of different substrates by...
EXCITE_C1_2022_31_SOUP
Orlando Sébastien Olivieri
2025
S.O.U.P. EXCITE Project: Unconventional energy Sources production, storage and release linked to subduction serpentinization: evidence from methane and hydrogen-rich fluid inclusions from the exhumed serpentinized peridotite of Monte Maggiore, Corsica
Activation of dissolution-precipitation creep causes weakening and viscous behaviour in experimentally-deformed antigorite
André Rik Niemeijer
2024
Antigorite occurs at seismogenic depth along plate boundary shear zones, particularly in subduction and oceanic transform settings, and has been suggested to control a low strength bulk rheology. To constrain dominant deformation mechanisms, we perform hydrothermal ring-shear experiments on...
Reaction weakening and the seismogenic potential of dolomite fault gouges
Elisabeth Kozlov
2026
An understanding of the evolution of the frictional behaviour and deformation mechanisms in dolomite faults is required to better understand earthquakes in carbonate terrains. Therefore, we investigated the seismogenic potential of dolomite and the dominant deformation mechanisms using rotary...