| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6446760 | Quaternary Science Reviews | 2012 | 15 Pages |
Abstract
⺠Low clay/silt ratios indicate periglacial chemical weathering. ⺠Secondary mineral assemblages consistent with generally minor chemical weathering. ⺠Temperature and parent lithology exert primary control on clay and silt abundances. ⺠Secondary minerals controlled by climate, regolith residence time, and hydrology. ⺠Quaternary blockfield formation, rather than Neogene initiation, is indicated.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
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Authors
Bradley W. Goodfellow,