| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6442117 | Precambrian Research | 2016 | 27 Pages |
Abstract
Regular 0.5Â m-scale sedimentary rhythms, reflecting subtle variations in sediment texture or composition occur throughout E3 and are interpreted as allocyclic. They are thought to be mainly primary in origin, locally modified slightly during early diagenetic cementation. Rhythms are proposed to represent ca. 18Â kyr precession cycles, implying 6-8Â Myr deposition between glaciations.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Ian J. Fairchild, Pierre Bonnand, Tesni Davies, Edward J. Fleming, Nathalie Grassineau, Galen P. Halverson, Michael J. Hambrey, Emily M. McMillan, Elizabeth McKay, Ian J. Parkinson, Carl T.E. Stevenson,