Identifying Quaternary Climate Change with XRF Analysis on Loess From South-Western England
Huge changes in climate occurred at the end of the last Quaternary glaciation. The end of this glaciation corresponds with the end of Pleistocene with its repeated glacial cycles and the start of the current geological epoch, the Holocene interglacial. The climate at this time was characterized by i...
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| Format: | Others |
| Language: | English |
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Uppsala universitet, Institutionen för geovetenskaper
2020
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| Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-412179 |