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Title: Western boundary of Mesozoic North America

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6644801

The line most often used to delineate the western edge of cratonic North America is the strontium isotope line. Strontium isotopes, however, differentiate, essentially, between continental crust and oceanic crust. They cannot usually distinguish between old autochthonous continental crust and old allochthonous continental crust. Geophysical parameters are often better suited to this purpose. In many places in the Western Cordillera, notably in SE British Columbia, the use of the strontium isotope line as a cratonic boundary line conflicts with other evidence, including other isotopic evidence, geological field relations, paleomagnetic evidence and geophysical data. Magnetic and gravity anomalies, conductivity, heat flow and seismic data suggest that the cratonic boundary there is approximately along the line of Kootenay Lake (117/sup 0/ W). This boundary, which is also a magnetic quiet zone, continues south into Idaho, where it is on strike with the western edge of the Idaho Batholith. Further south, the western boundary of Mesozoic North American probably lay west of the basement quiet zone, at the pre-extension western edge of the Basin and Range Province. The geophysical evidence in northern Canada suggests that the Rocky Mountain Trench and the Tintina fault mark the cratonic edge of Mesozoic North America in that region.

Research Organization:
Univ. of Alberta, Edmonton (Canada)
OSTI ID:
6644801
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English