| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9526033 | Sedimentary Geology | 2005 | 19 Pages |
Abstract
These shale-bed-partings can be interpreted in two ways: as pulses of terreginous material entering the system and overwhelming carbonate deposition, or as background sediment, accumulating during pauses in carbonate deposition. While the older Glenwood and Platteville samples can be interpreted in either way, the samples from the Galena are better interpreted as condensed background sediment.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Lauren M. Chetel, J.A. (Toni) Simo, Brad S. Singer,