Published March 30, 2022
| Version v1
Figure
Open
Fig. 8 in Priabonian, late Eocene chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana, USA
Authors/Creators
Description
Fig. 8. Correlation of Pipestone Springs and Flagstaff Rim upper Eocene lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. → A. Location of Flagstaff Rim (Wyoming) and Pipestone Springs (Montana). B. Pipestone Springs reference section and Flagstaff Rim section showing its lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. Sections are correlated based upon Pipestone Spring's 40Ar/39Ar age of 36.00±0.20 Ma tuff and Flagstaff Rim's Ash B, and on middle Chadronian vertebrate assemblages in the PSMP and between Flagstaff Rim's Ash B to Ash G. 40Ar/39Ar age controls for Pipestone Springs strata are from this study; Flagstaff Rim tuff ages are from Swisher and Prothero (1990), Obradovich et al. (1995), and Sahy et al. (2015) Abbreviations: An, anorthoclase; Bi, biotite; S, sanidine (denote minerals used for single crystal 40Ar/39Ar age analyses of tuffs).
Notes
Published as part of Hanneman, Debra L., Lofgren, Donald, Hasiotis, Stephen T. & Mcintosh, William C., 2022, Priabonian, late Eocene chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana, USA, pp. 5-20 in Acta Palaeontologica Polonica 67 (1) on page 14, DOI: 10.4202/app.00901.2021, http://zenodo.org/record/10626764
Files
figure.png
Files
(348.1 kB)
| Name | Size | Download all |
|---|---|---|
|
md5:b608f7b5fe02a3065f8635a859d921d7
|
348.1 kB | Preview Download |
Linked records
Additional details
Related works
- Is part of
- Journal article: 10.4202/app.00901.2021 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFD4D320FFE33034FFBEFFE2335BFFF7 (LSID)
- Journal article: https://zenodo.org/record/10626764 (URL)