Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6442385 | Precambrian Research | 2012 | 12 Pages |
Abstract
⺠Paleosols occur in the Aravalli craton along the Archean-Proterozoic interface. ⺠The weathering interval is defined as between â¼2.5 Ga and â¼2.15 Ga. ⺠Lateritic weathering formed a lower iron-depleted and upper iron-enriched zone. ⺠An evolutionary model shows the structural control of paleosol sections. ⺠Complete sections are preserved only along the eastern flank of the synclinorium.
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Authors
Helga de Wall, Manoj K. Pandit, Narendra K. Chauhan,