Neodymium isotopic evidence for early Proterozoic units in the Watersmeet gneiss dome, northern Michigan. Temperature-pressure estimates of dynamically recrystallized rocks in the early Proterozoic Mountain shear zone, northeastern Wisconsin
Links
- Document: Report (pdf)
- Larger Work: This publication is Chapter G,H of Contributions to Precambrian geology of Lake Superior region
- NGMDB Index Page: National Geologic Map Database Index Page
- Download citation as: RIS | Dublin Core
Abstract
No abstract available.
Suggested Citation
Barovich, K.M., Patchett, P.J., Peterman, Z., Sims, P., Day, W.C., 1991, Neodymium isotopic evidence for early Proterozoic units in the Watersmeet gneiss dome, northern Michigan. Temperature-pressure estimates of dynamically recrystallized rocks in the early Proterozoic Mountain shear zone, northeastern Wisconsin: U.S. Geological Survey Bulletin 1904, 36 p., https://doi.org/10.3133/b1904GH.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Neodymium isotopic evidence for early Proterozoic units in the Watersmeet gneiss dome, northern Michigan. Temperature-pressure estimates of dynamically recrystallized rocks in the early Proterozoic Mountain shear zone, northeastern Wisconsin |
| Series title | Bulletin |
| Series number | 1904 |
| Chapter | G,H |
| DOI | 10.3133/b1904GH |
| Year Published | 1991 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Description | 36 p. |
| Country | United States |
| State | Michigan, Wisconsin |