MULTIMETHOD RADIOMETRIC AGE FOR A BENTONITE NEAR THE TOP OF THE BACULITES-REESIDEI ZONE OF SOUTHWESTERN SASKATCHEWAN (CAMPANIAN MAASTRICHTIAN STAGE BOUNDARY)
H. Baadsgaard et al., MULTIMETHOD RADIOMETRIC AGE FOR A BENTONITE NEAR THE TOP OF THE BACULITES-REESIDEI ZONE OF SOUTHWESTERN SASKATCHEWAN (CAMPANIAN MAASTRICHTIAN STAGE BOUNDARY), Canadian journal of earth sciences, 30(4), 1993, pp. 769-775
A 15 cm thick bentonite at the top of the Baculites reesidei Zone in C
ruikshank Coulee north of Herbert in southwestern Saskatchewan yielded
biotite, sanidine, plagioclase, and zircon. Rb-Sr analyses give a min
eral isochron with an age of 72.5 +/- 0.2 Ma (+/- 2a). U-Pb analyses o
f zircon produced concordant Pb-206/U-238 and Pb-207/U-235 ages of 72.
4 +/- 0.4 Ma (+/- 2sigma) and 72.6 +/- 0.4 Ma (+/- 2sigma), respective
ly. Laser Ar-40/Ar-39 dating of sanidine and biotite revealed ages of
72.5 +/- 0.2 Ma (+/- SE) and 72.6 +/- 0.2 Ma (+/- SE), respectively. I
f the Campanian - Maastrichtian stage boundary is near the top of the
Baculites reesidei Zone, then the overall average age of 72.5 +/- 0.4
Ma dates the stage boundary.