We investigated the microstructure and crystallographic preferred orientation (CPO) of quartz within veins from two different granitoid intrusions (Avio intrusion, (AV) in the Adamello-Italy, and Lake Edison intrusion (LE) in the Sierra Nevada-California). The veins localized post-magmatic crystal-plastic deformation during cooling to the host rock temperature at a depth of about 10 km. They developed during high temperature conditions as tabular fillings of joints and were later deformed by simple shear parallel of the vein wall mainly at T 500C. Synkinematic localized granitoid mylonites at the boundary of the quartz veins show recrystallization of biotite and plagioclase, and formation and recrystallization of myrmekites. The AV samples...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
Near the eastern end of the Tonale fault zone, a segment of the Periadriatic fault system in the Ita...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
We have studied quartz microstructures and the c-axis crystallographic preferred orientations (CPOs)...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
In the geologic record, the quartz c-axis patterns are widely adopted in the investigation of crysta...
Exhumed granitoid plutons are an ideal natural research target for studying the processes of nucleat...
Quartz Crystallographic Preferred Orientation (CPO) patterns are most commonly a result of deformati...
Quartz veins in the Eastern Tonale mylonite zone (Italian Alps) were deformed in strike-slip shear. ...
This study analyzes crystal preferred orientation (CPO) patterns within constrictional quartz-rich g...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
Near the eastern end of the Tonale fault zone, a segment of the Periadriatic fault system in the Ita...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
We have studied quartz microstructures and the c-axis crystallographic preferred orientations (CPOs)...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
Quartz veins within Rieserferner pluton underwent deformation during post-magmatic cooling at temper...
In the geologic record, the quartz c-axis patterns are widely adopted in the investigation of crysta...
Exhumed granitoid plutons are an ideal natural research target for studying the processes of nucleat...
Quartz Crystallographic Preferred Orientation (CPO) patterns are most commonly a result of deformati...
Quartz veins in the Eastern Tonale mylonite zone (Italian Alps) were deformed in strike-slip shear. ...
This study analyzes crystal preferred orientation (CPO) patterns within constrictional quartz-rich g...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
This study considers microstructures developed during creep deformation of metachert in the mylonite...
Near the eastern end of the Tonale fault zone, a segment of the Periadriatic fault system in the Ita...