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• W1989535012 abstract "The Manicouagan Structure, of impact origin, is located in eastern Quebec, about 300 km north of the St. Lawrence River. The complex is of Triassic age. The shock deformation of the more important rock-forming minerals of the autochthonous, or at least parautochthonous, rocks within the structure is described. Four zones of shock metamorphism are delineated, based on the deformation features of plagioclase: (1) plagioclase without planar features, (2) plagioclase with planar features, (3) first occurrence of plagioclase with partial isotropization and (4) first occurrence of plagioclase with total isotropization. These four zones are more or less concentric and indicate a general increase in the grade of shock metamorphism towards the centre of the structure. However, several small areas, probably underlain by allochthonous rocks, appear not to fit this general picture. Biotite and garnet show evidence of a shock orientation of their deformation features. An impact origin for the structure is favoured, the impact possibly triggering volcanism." @default.
• W1989535012 created "2016-06-24" @default.
• W1989535012 creator A5063804902 @default.
• W1989535012 date "1990-01-01" @default.
• W1989535012 modified "2023-10-12" @default.
• W1989535012 title "Shock metamorphic features and their zoning and orientation in the Precambrian rocks of the Manicouagan Structure, Quebec, Canada" @default.
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• W1989535012 doi "https://doi.org/10.1016/0040-1951(90)90101-d" @default.
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