Paleopedology of soils in thick Holocene loess, Nebraska, USA
Bignell Loess is a Holocene loess unit that has accumulated in the central Great Plains since9,000 14C yr BP. The Brady Soil separates Bignell Loess from last glacial Peoria Loess and thick sections,which can reach 6 m thickness, may contain four buried soils beneath the modern surface soil. TheBrad...
Shranjeno v:
| izdano v: | Revista Mexicana de Ciencias Geológicas |
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| Principais autores: | , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Universidad Nacional Autónoma de México
2004
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| Teme: | |
| Online dostop: | https://www.redalyc.org/articulo.oa?id=57221107 |
| Oznake: |
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