Rock-magnetic study of Late Pleistocene-Holocene sediments from the Babícora lacustrine basin, Chihuahua, northern Mexico
Rock-magnetic and sedimentological studies of the Quaternary sequence of lakeBabícora (29.4°N, 107.7°W; 2,100 m a.s.l.) from Late Wisconsin to Holocene arereported. Two vertical profiles have been studied. Magnetic susceptibilities andnatural remanence (NRM) and isothermal remanence (IRM) intensitie...
Furkejuvvon:
| Publikašuvnnas: | Geofísica Internacional |
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| Váldodahkkit: | , , |
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Universidad Nacional Autónoma de México
1997
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| Fáttát: | |
| Liŋkkat: | https://www.redalyc.org/articulo.oa?id=56836202 |
| Fáddágilkorat: |
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