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Original Article
Tectono-sedimentary Evolution of Early Pennsylvanian Alluvial Systems at the Onset of the Alleghanian Orogeny, Pocahontas Basin, Virginia
Article first published online: 20 MAR 2013
DOI: 10.1111/bre.12008
© 2013 The Authors. Basin Research © 2013 Blackwell Publishing Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists
Additional Information
How to Cite
Grimm, R.P., Eriksson, K. and Carbaugh, J. (2013), Tectono-sedimentary Evolution of Early Pennsylvanian Alluvial Systems at the Onset of the Alleghanian Orogeny, Pocahontas Basin, Virginia. Basin Research. doi: 10.1111/bre.12008
Publication History
- Article first published online: 20 MAR 2013
- Accepted manuscript online: 20 NOV 2012 09:34AM EST
- Manuscript Accepted: 10 OCT 2012
- Manuscript Revised: 22 JUL 2012
- Manuscript Received: 22 DEC 2011
- Abstract
- Article
- References
- Supporting Information
- Cited By
| Filename | Format | Size | Description |
|---|---|---|---|
| bre12008-sup-0001-FigS1.tif | image/tif | 8583K | S1. Transverse Fluvial Facies Association. (a) Siderite conglomerate lag. Pen for scale, Pocahontas, West Virginia. (b) Mudstone-clast conglomerate lag. EQT #1 Sandy Ridge Core, 1927 ft. Scale bar is 1 cm. (c) Thick gleyed and rooted mudstone below tabular coal horizon, Pocahontas Formation along I-77 near Flat Top, West Virginia. |
| bre12008-sup-0002-FigS2.tif | image/tif | 3606K | S2. Example vertical successions of lithologies, sedimentary structures, facies associations and subsurface gamma-ray characteristics of the Warren Point and Pocahontas Formations from the Equitable Sandy Ridge Core (a) and (b) US Dept. of Energy CO2–ECBM monitoring well #2. |
| bre12008-sup-0003-FigS3.tif | image/tif | 8575K | S3. Isopach map of the total combined thickness of Pocahontas, Bottom Creek and Alvy Creek composite sequences. |
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