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- W2135774536 abstract "Recent work in a previously little-known part of the Central Gneiss Belt of the southwestern Grenville Province has outlined a regional structural pattern made by a number of geologically distinctive domains that are separated by broad ductile shear zones. Characteristics rock assemblages, metamorphism, geophysical signatures and structural trends are modified or truncated at domain margins. Bounding high strain zones contain mylonite and other forms of tectonically modified gneiss, formed under at least middle amphibolite facies conditions, within which kinematic indicators imply a northwesterly sense of overriding or lateral sliding between adjacent crustal masses. Similar kinematics also apply at the margin of the Central Metasedimentary Belt to the southeast and along the Grenville Front to the northwest. A scenario involving northwesterly stacking of large crustal blocks and slices at relatively deep level can account for the observed relationships and implies a period of crustal thickening that may represent the culmination of the Grenvillian Orogeny in this region." @default.
- W2135774536 created "2016-06-24" @default.
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- W2135774536 date "1984-12-01" @default.
- W2135774536 modified "2023-10-14" @default.
- W2135774536 title "Tectonic boundaries within the Grenville province of the Canadian shield" @default.
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- W2135774536 doi "https://doi.org/10.1016/0264-3707(84)90018-8" @default.
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