Testing the reliability of detrital cave sediments as recorders of paleomagnetic secular variations, Seso Cave System (Central Pyrenees, Spain)
A paleomagnetic study has been carried out on a waterlaid detrital sedimentary sequence of ~240cm thick within the Seso Cave System (West-Central Pyrenees). In these sediments, seven charcoal samples were dated using 14C AMS ranging from 2080 to 650calyrBP (130BC–1300AD). Two levels of human occupat...
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Veröffentlicht in: | Catena (Giessen) 2014-08, Vol.119 (119), p.36-51 |
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