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Stratigraphy and paleomagnetism of a 2.9-km composite lava section in Eyjafjordur, Northern Iceland: a reconnaissance study

机译:冰岛北部Eyjafjordur一段2.9公里的复合熔岩区的地层学和古磁性:一项勘测研究

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摘要

Eight mountainside profiles in lava flows south of the fjord Eyjafjordur, Northern Iceland, were sampled for paleomagnetic studies. The sampling was concurrent with pilot stratigraphic mapping of the lava sequences in these and several supplementary profiles. The eight profiles are correlated with minor overlaps so that they form a composite section of 2.9 km thickness, estimated to cover the age range between about 9 and 5 million years ago (Hardarson et al. 1999). Paleomagnetic measurements made on 319 lavas generally yield primary remanence directions of high stability and within-unit consistency. Evidence for at least 17 reversals of the geomagnetic field is seen, as well as numerous field excursions. Frequent clustering of directions in successive lavas indicates that the volcanism was episodic.
机译:在冰岛北部的峡湾艾雅峡湾(Eyjafjordur)以南的熔岩流中,有八个山腰剖面被采样用于古地磁研究。采样与这些以及其他几个补充剖面中的熔岩序列的中试地层测绘同时进行。八个剖面与少量重叠相关,因此它们形成了一个2.9 km厚度的复合剖面,估计覆盖了大约9到500万年前的年龄范围(Hardarson等,1999)。在319个熔岩上进行的古磁测量通常会得出主要的剩磁方向,即高稳定性和单元内一致性。可以看到至少17次地磁场逆转的证据,以及大量的磁场偏移。连续熔岩中方向的频繁聚集表明该火山是偶发性的。

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