Absolute age of early Precambrian rocks in the Bighorn Basin of Wyoming and Montana, and southeastern Manitoba
- 1 April 1958
- journal article
- Published by American Geophysical Union (AGU) in EOS, Transactions American Geophysical Union
- Vol. 39 (2) , 322-334
- https://doi.org/10.1029/tr039i002p00322
Abstract
Age determinations on nine samples from the southeastern part of the Beartooth Range, Montana, indicate that the absolute age of the pegmatites and granitic gneisses of this area is 2750 ± 150 m y. A single determination from the northern Bighorn Mountains, Wyoming, suggests a similar age for this portion of the Precambrian basement. Several samples from the Winnipeg River ‐ Johnston Lake area of Manitoba indicate an absolute age of 2650 ± 150 m y for both the pegmatites and gneisses. A similar age was found for a muscovite from the northwestern angle region of Minnesota. Rubidium‐strontium ages were found to be more consistent than potassium‐argon ages. Argon loss from micas was commonly as great as 15 pct.Keywords
This publication has 25 references indexed in Scilit:
- Radioactivity of Potassium and Geologic TimeScience, 1957
- URANIUM-LEAD METHOD OF AGE DETERMINATIONGSA Bulletin, 1957
- Decay Constants ofas Determined by the Radiogenic Argon Content of Potassium MineralsPhysical Review B, 1956
- Half-Life ofPhysical Review B, 1956
- Petrology of Pre-Cambrian Granites in the Northern Bighorn Mountains, WyomingThe Journal of Geology, 1955
- Redetermination of the Disintegration Constant ofPhysical Review B, 1955
- The Specific Alpha-Activities and Half-Lives of , , andPhysical Review B, 1952
- A Redetermination of the Relative Abundances of the Isotopes of Neon, Krypton, Rubidium, Xenon, and MercuryPhysical Review B, 1950
- The Isotopic Constitution of Lead and the Measurement of Geological Time. IIIPhysical Review B, 1941
- Diastrophic Behavior around the Bighorn BasinThe Journal of Geology, 1940