Shock-related textures in feldspars have been found in impactites from the Tenoumer impact structure, Mauritania. We see a range in features, from disruption of twin planes, to inclined deformation lamellae, to true Planar Deformation Features (PDF’s) which occur at multiple orientations to one another. Most notably, these textures occur in samples that do not contain shocked quartz, suggesting feldspars record evidence of shock pressures lower than 8 GPa
The record of terrestrial meteorite impacts is fragmentary because most impact structures and ejecta...
Plagioclase and biotite phenocrysts in ignimbrites erupted from the Toba caldera, Sumatra, show micr...
The study of shock-metamorphic features of the Zagami meteorite revealed pseudotachylite-like melt v...
Shock-related textures in feldspars have been found in impactites from the Tenoumer impact structure...
Feldspars are the dominant mineral in the crust of most terrestrial planetary bodies, including Eart...
Shock metamorphism, caused by hypervelocity impact, is a poorly understood process in feldspar. This...
Impact cratering was once considered a rare geological process of no, or little, importance to the e...
Meteorite impact craters are the dominant surface feature on most terrestrial planetary bodies [1]...
Plagioclase feldspar is one of the most common rock‐forming minerals on the surfaces of the Earth an...
Shock effects in small terrestrial impact craters (diameter < 300 m) have been poorly studied becaus...
Introduction: During hypervelocity impact the crater subsurface experiences pervasive deformation. F...
Most of the craters on the Earth, produced by an impact of meteorite or other space object, have bee...
Thus far, detailed petrologic studies of shock metamorphism have been performed on samples recovered...
Shocked quartz is typically used to test if sites experienced a meteorite impact in the past, howeve...
With an age of less than ~5000 yr and diameter of 45 m, Kamil crater in Egypt [1] is one of the youn...
The record of terrestrial meteorite impacts is fragmentary because most impact structures and ejecta...
Plagioclase and biotite phenocrysts in ignimbrites erupted from the Toba caldera, Sumatra, show micr...
The study of shock-metamorphic features of the Zagami meteorite revealed pseudotachylite-like melt v...
Shock-related textures in feldspars have been found in impactites from the Tenoumer impact structure...
Feldspars are the dominant mineral in the crust of most terrestrial planetary bodies, including Eart...
Shock metamorphism, caused by hypervelocity impact, is a poorly understood process in feldspar. This...
Impact cratering was once considered a rare geological process of no, or little, importance to the e...
Meteorite impact craters are the dominant surface feature on most terrestrial planetary bodies [1]...
Plagioclase feldspar is one of the most common rock‐forming minerals on the surfaces of the Earth an...
Shock effects in small terrestrial impact craters (diameter < 300 m) have been poorly studied becaus...
Introduction: During hypervelocity impact the crater subsurface experiences pervasive deformation. F...
Most of the craters on the Earth, produced by an impact of meteorite or other space object, have bee...
Thus far, detailed petrologic studies of shock metamorphism have been performed on samples recovered...
Shocked quartz is typically used to test if sites experienced a meteorite impact in the past, howeve...
With an age of less than ~5000 yr and diameter of 45 m, Kamil crater in Egypt [1] is one of the youn...
The record of terrestrial meteorite impacts is fragmentary because most impact structures and ejecta...
Plagioclase and biotite phenocrysts in ignimbrites erupted from the Toba caldera, Sumatra, show micr...
The study of shock-metamorphic features of the Zagami meteorite revealed pseudotachylite-like melt v...