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Faroe Marine Ash Zone IV: a new MIS 3 ash zone on the Faroe Islands margin

机译:法罗海洋灰区IV:法罗群岛边缘的新MIS 3灰区

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摘要

A basaltic tephra layer from MIS 3 has been discovered by analysis of cores from the Faroe Islands margin. The tephra layer appears up to 20 cm thick in some records. After the first main fall-out event the tephra is believed to be mainly deposited and redistributed by bottom currents. Geochemical analyses suggest that the tephra is relatively undisturbed by allochtonous tephra grains and unmixed. The peak occurrences are in the lower part of GIS (Greenland Interstadial) 12 and we suggest naming this new tephra Faroe Marine Ash Zone IV (FMAZ IV), following the nomenclature adopted for previous ash zones found on the Faroe Islands margin. Geochemical analyses of the tephra show affinities with the Grímsvötn volcanic system in the Eastern Volcanic Zone in south Iceland. The average age of FMAZ IV from four independent age models is 46 800±1000 years BP. We suggest that the V5 ash zone, found on the Reykjanes Ridge is a correlative to the FMAZ IV.
机译:通过对法罗群岛边缘的岩心进行分析,发现了MIS 3的玄武特非拉层。在某些记录中,特弗拉层的厚度高达20厘米。在第一次主要的跌落事件之后,据信特非拉主要由海底电流沉积和重新分布。地球化学分析表明,该球茎相对不受异物球茎粒的干扰,并且没有混合。高峰出现在GIS(格陵兰际)的下部,我们建议根据法罗群岛边缘发现的先前灰区的命名法,命名这个新的特非拉法罗海洋灰区IV(FMAZ IV)。对特发拉的地球化学分析显示,它与冰岛南部东部火山区的Grímsvötn火山系统具有相似性。来自四个独立年龄模型的FMAZ IV的平均年龄为46 800±1000年BP。我们建议在雷克雅尼斯海岭上发现的V5灰区与FMAZ IV有关。

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