We investigated the microstructures of periclase-to-brucite hydration domains within marble from the Adamello contact aureole (Italy). The microstructure preserve high differential stresses within the calcite surrounding the hydration domains of up to 1.5 GPa. Samples were investigated using optical, scanning and transmission electron microscopy as well as high-angular resolution electron backscatter diffraction (HREBSD). Stress measurements obtained via HREBSD are compared to analytical solutions. The data is organised in 10 folders termed (Supplementary) Figure X, where X is the figure number in the primary publication and supplementary information. An additional folder contains Matlab scripts for the analytical solutions to the stress me...
The paper examines the cracks initiation, propagation and coalescence until failure in a crystalline...
Stone physical weathering, deterioration and damage (e.g. bowing, cracking, microfracturing) represe...
International audienceFor the first time, nanometer resolution techniques both in situ and ex situ w...
Hydration reactions are a fundamental metamorphic process and play a critical role in Earth’s tecton...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Calcite twinning is a dominant deformation mechanism at low temperatures. It is often used to recons...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Hydration reactions influence rock density and rheology. For example, volume increases produced in h...
Understanding conditions in the Earth's interior requires data derived from laboratory experiments. ...
The volume-increase associated with hydration reactions in rocks may lead to reaction-induced fractu...
International audienceArgillaceous rocks are chosen as possible host rocks for underground radioacti...
One of the properties that makes marble such an excellent construction and ornamental material is it...
The paper examines the cracks initiation, propagation and coalescence until failure in a crystalline...
Stone physical weathering, deterioration and damage (e.g. bowing, cracking, microfracturing) represe...
International audienceFor the first time, nanometer resolution techniques both in situ and ex situ w...
Hydration reactions are a fundamental metamorphic process and play a critical role in Earth’s tecton...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Calcite twinning is a dominant deformation mechanism at low temperatures. It is often used to recons...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Hydration reactions influence rock density and rheology. For example, volume increases produced in h...
Understanding conditions in the Earth's interior requires data derived from laboratory experiments. ...
The volume-increase associated with hydration reactions in rocks may lead to reaction-induced fractu...
International audienceArgillaceous rocks are chosen as possible host rocks for underground radioacti...
One of the properties that makes marble such an excellent construction and ornamental material is it...
The paper examines the cracks initiation, propagation and coalescence until failure in a crystalline...
Stone physical weathering, deterioration and damage (e.g. bowing, cracking, microfracturing) represe...
International audienceFor the first time, nanometer resolution techniques both in situ and ex situ w...