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A new mid-Holocene tephra in central Sweden

机译:瑞典中部的全新中全新世特非拉

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A mid-Holocene tephra, LBA-2 has been found in a peat bog in central Sweden. Geochemical analyses suggest an origin in an evolved volcanic centre, most likely the Snafellsnes volcanic centre in western Iceland. The geochemistry of the LBA-2 tephra is similar to the youngest of three silicic tephra layers from Snafellsjokull, Sn-1 dated to 1780 cal yr BP. However, wiggle-match dating indicates an age of 3550–3650 cal yr BP, close in age to the Hekla-S/Kebister tephra (3720 cal yr BP), previously found in several sites in Scandinavia. Detailed geochemical analyses and dating is lacking for the mid-Holocene Sn-2 tephra in Iceland but it is likely that the geochemical composition is similar as the Sn-1 tephra. The LBA-2 tephra is tentatively correlated with the Sn-2 tephra and we also suggest that the ‘x’ tephra layer (ca 3500 BP) found in the Dyngjufjoll area, central Iceland (Sigvaldason et al. 1992) can be correlated with the Sn-2 tephra.
机译:在瑞典中部的一个泥炭沼泽中发现了一种全新世中生的特弗拉LBA-2。地球化学分析表明它起源于一个演化的火山中心,很可能是冰岛西部的Snafellsnes火山中心。 LBA-2特菲拉的地球化学特征类似于Snafellsjokull的三个硅质特菲拉层中最年轻的一个,Sn-1年代可追溯至1780 cal BP。但是,摆动匹配约会表明年龄为3550–3650 cal BP,与Hekla-S / Kebister tephra(3720 cal yr BP)的年龄相近,Hekla-S / Kebister tephra(BP 3720 cal yr)以前曾在斯堪的那维亚的多个地点发现。冰岛中全新世的Sn-2特非拉缺乏详细的地球化学分析和测年,但地球化学组成可能与Sn-1特非拉相似。 LBA-2特弗拉暂时与Sn-2特弗拉相关,我们还建议在冰岛中部Dyngjufjoll地区发现的'x'特弗拉层(ca 3500 BP)(Sigvaldason et al。1992)可以与Sn-2特非拉。

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