Val Sorda: An upper Pleistocene loess-paleosol sequence in northeastern Italy
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| Formato: | Artículo científico |
| Lenguaje: | en |
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Universidad Nacional Autónoma de México
2004
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| _version_ | 1876451805073768448 |
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| author | Francesca Ferraro |
| author_facet | Francesca Ferraro |
| contents | Val Sorda: An upper Pleistocene loess-paleosol sequence in northeastern Italy Francesca Ferraro Birgit Terhorst Franz Ottner Mauro Cremaschi Ciencias de la Tierra loess Italy paleosol Chernozem Val Sorda The upper Pleistocene loess-paleosol sequence of Val Sorda (northeastern Italy) is investigatedwith paleopedological, micromorphological, and mineralogical methods. Special emphasis is placed onmagnetic parameters and analysis of clay minerals. The base of the sequence is an Eemian paleosol,which consists of a rubefied Bt-horizon formed in till. This Bt-horizon is covered by loess, three interstadialpaleosols and colluvial deposits. The three interstadial paleosols have a Chernozem morphology andcharacteristics, reflecting a dry and continental paleoclimate. The top of the sequence is covered by tilldeposited during the Solferino Stage glacial advance. 2004 artículo científico 1026-8774 https://www.redalyc.org/articulo.oa?id=57221105 en http://www.redalyc.org/revista.oa?id=572 Revista Mexicana de Ciencias Geológicas application/pdf Universidad Nacional Autónoma de México Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.21 |
| format | Artículo científico |
| id | redalyc_57221105 |
| institution | Redalyc |
| language | en |
| publishDate | 2004 |
| publisher | Universidad Nacional Autónoma de México |
| spellingShingle | Val Sorda: An upper Pleistocene loess-paleosol sequence in northeastern Italy Francesca Ferraro Ciencias de la Tierra loess Italy paleosol Chernozem Val Sorda Val Sorda: An upper Pleistocene loess-paleosol sequence in northeastern Italy Francesca Ferraro Birgit Terhorst Franz Ottner Mauro Cremaschi Ciencias de la Tierra loess Italy paleosol Chernozem Val Sorda The upper Pleistocene loess-paleosol sequence of Val Sorda (northeastern Italy) is investigatedwith paleopedological, micromorphological, and mineralogical methods. Special emphasis is placed onmagnetic parameters and analysis of clay minerals. The base of the sequence is an Eemian paleosol,which consists of a rubefied Bt-horizon formed in till. This Bt-horizon is covered by loess, three interstadialpaleosols and colluvial deposits. The three interstadial paleosols have a Chernozem morphology andcharacteristics, reflecting a dry and continental paleoclimate. The top of the sequence is covered by tilldeposited during the Solferino Stage glacial advance. 2004 artículo científico 1026-8774 https://www.redalyc.org/articulo.oa?id=57221105 en http://www.redalyc.org/revista.oa?id=572 Revista Mexicana de Ciencias Geológicas application/pdf Universidad Nacional Autónoma de México Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.21 |
| title | Val Sorda: An upper Pleistocene loess-paleosol sequence in northeastern Italy |
| topic | Ciencias de la Tierra loess Italy paleosol Chernozem Val Sorda |
| url | https://www.redalyc.org/articulo.oa?id=57221105 |