Optical measurements of microstructural features in experimentally deformed Carrara marble help define their dependence on stress. These features include dynamically recrystallized grain size (Dr), subgrain size (Sg), minimum bulge size (Lρ), and the maximum scale length for surface-energy driven grain-boundary migration (Lγ). Taken together with previously published data Dr defines a paleopiezometer over the range 15–291 MPa and temperature over the range 500–1000 °C, with a stress exponent of −1.09 (CI −1.27 to −0.95), showing no detectable dependence on temperature. Sg and Dr measured in the same samples are closely similar in size, suggesting that the new grains did not grow significantly after nucleation. Lρ and Lγ measured on each sam...
AbstractWe study the role of grain size in the rheological behavior of calcite aggregates in the sem...
Different types of deformation experiments were conducted on specimens of Carrara marble at a temper...
This study investigates the microstructure and texture variations across a mm-scale shear zone in Ca...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Geodynamic processes such as subduction and rifting are mainly controlled by high temperature plasti...
Thesis (S.B.)--Massachusetts Institute of Technology, Dept. of Materials Science and Engineering; an...
Geodynamic processes such as subduction and rifting are mainly controlled by high temperature plasti...
A flanking structure developed along a secondary shear zone in calcite marbles, on Syros (Cyclades, ...
Calcite twinning is a dominant deformation mechanism at low temperatures. It is often used to recons...
This study investigates the microstructure and texture variations across a mm-scale shear zone in Ca...
AbstractWe study the role of grain size in the rheological behavior of calcite aggregates in the sem...
Different types of deformation experiments were conducted on specimens of Carrara marble at a temper...
This study investigates the microstructure and texture variations across a mm-scale shear zone in Ca...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Optical measurements of microstructural features in experimentally deformed Carrara marble help defi...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Recrystallized grains are potentially useful as indicators of palaeostress in naturally deformed roc...
Geodynamic processes such as subduction and rifting are mainly controlled by high temperature plasti...
Thesis (S.B.)--Massachusetts Institute of Technology, Dept. of Materials Science and Engineering; an...
Geodynamic processes such as subduction and rifting are mainly controlled by high temperature plasti...
A flanking structure developed along a secondary shear zone in calcite marbles, on Syros (Cyclades, ...
Calcite twinning is a dominant deformation mechanism at low temperatures. It is often used to recons...
This study investigates the microstructure and texture variations across a mm-scale shear zone in Ca...
AbstractWe study the role of grain size in the rheological behavior of calcite aggregates in the sem...
Different types of deformation experiments were conducted on specimens of Carrara marble at a temper...
This study investigates the microstructure and texture variations across a mm-scale shear zone in Ca...