作者: A.G. Wintle , S.C. Packman
DOI: 10.1016/0277-3791(88)90021-2
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摘要: Abstract Samples were collected from sections at Mende, Paks and Tapiosuly. Ages for the loess above MF1 soil Mende in agreement with radiocarbon dates on charcoal fragments soil. Tapiosuly also ages younger soils. However, TL age estimates or below MF2 each of three sites suggested that this had an around 76 ka. It has not been confirmed whether these are underestimated, however, they older than previously thought basis other studies. They imply underlying MB is much last interglacial.