The oxygen isotope composition of the surface crystalline rocks of the Canadian Shield

• Published in: Canadian Journal of Earth Sciences
• Main Authors: Shieh, Yuch-Ning, Schwarcz, Henry P.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Canadian Science Publishing 1978
• Subjects: Baffin Island; Baffin; Keewatin
• Online Access: http://dx.doi.org/10.1139/e78-185; http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-185

The average 18 O/ 16 O ratios of the major rock types of the surface crystalline rocks in different parts of the Canadian Precambrian Shield have been determined, using 47 composite samples prepared from 2221 individual rock specimens. The sampling areas include Baffin Island, northern and southwestern Quebec, Battle Harbour – Cartwright, northern District of Keewatin, Fort Enterprise, Snowbird Lake, Kasmere Lake, and Saskatchewan, covering approximately 1 400 000 km 2 . The granitic rocks from the Superior, Slave, and Churchill Provinces vary only slightly from region to region (δ 18 O = 6.9–8.4‰) and are significantly lower in 18 O than similar rock types from the younger Grenville Province (δ = 9.2–10.0‰). The sedimentary and metasedimentary rocks have δ 18 O = 9.0–11.7‰ and hence are considerably lower than their Phanerozoic equivalents, possibly reflecting the presence of a high percentage of little-altered igneous rock detritus in the original sediments. The basic rocks in most regions fall within a δ 18 O range of 6.8–7.6‰, except in northern and southwestern Quebec where the δ-values are abnormally high (8.5–8.9‰). The overall average 18 O/ 16 O ratio of the surface crystalline rocks of the Canadian Shield is estimated to be 8.0‰, which represents an enrichment with respect to probable mantle derived starting materials by about 2‰.