匈牙利b kk Mts二叠-三叠纪剖面的古地磁

E. Márton
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引用次数: 4

摘要

在二叠纪/三叠纪的分界线上,陆地和海洋生物都遭到了严重的破坏。这种急剧减少可能是由于一个全球性事件。为了证明这一点,需要将彼此相距很远的部分进行关联,这是一项艰巨的任务,特别是在海洋和陆地部分之间。磁地层对比是一种与环境无关的方法。该方法旨在应用于Bukk Mts的二叠纪/三叠纪边界剖面的精确测年,其中包括具有高浓度磁球的地层。由于北鹿山古生代-中生代岩石具有反变质和强烈构造作用,因此决定在收集大量样品进行磁地层学调查之前,先对两个不同倾角剖面的样品进行初步的古地磁研究。本研究的结果可以总结如下。这些剖面的岩石具有倾斜前时代的遗迹,而且……
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Paleomagnetism of Permian-Triassic sections, Bükk Mts, Hungary
At the Permian/Triassic boundary, terrestrial as well as marine life was seriously decimated. The drastic reduction was possibly due to a global event. In order to demonstrate this, sections at great distance from one another need to be correlated, which is a difficult task, especially between marine and land sections. One of the methods, which is independent of the environment, is magnetostratigraphic correlation. It was intended to apply this method for precise dating to Permian/Triassic boundary sections from the Bukk Mts, which include strata with high concentrations of magnetospherules. Since the Paleozoic-Mesozoic rocks of the Bukk Mts are anchimetamorphosed and intensively tectonized, it was decided to carry out a pilot paleomagnetic study on samples from two sections with different dips, before collecting a large number of samples for the intended magnetostratigraphy survey. The results of this study can be summarized as follows. The rocks of the sections possess remanences of pre-tilting age, and...
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