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Anisotropy of magnetic susceptibility of the Pyrenean granites

机译:比利牛斯山脉花岗岩的磁化率各向异性

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In this paper, we report on a compilation of more than 2200 sites (more than 10,000 individual measurements) where anisotropy of magnetic susceptibility (AMS) was studied in granites from the Variscan Pyrenees. The standardization and homogenization of this information has allowed us to produce three Main Maps that synthesize all the information related with the AMS of the Pyrenean granites. We also describe the problems found during the construction of the database (variable geo-positioning, different published information, etc.). The information derived from 21 granite bodies, the database, and the synthesis maps (magnetic susceptibility, Km, and the orientation of the magnetic foliation, plane perpendicular to k3, and of the magnetic lineation, k1) allow us to see for the first time a complete image of this important kinematic and petrographic indicator.
机译:在本文中,我们报告了一个汇总的2200多个站点(超过10,000个单独的测量值),在这些站点中研究了Variscan比利牛斯山脉花岗岩中的磁化率各向异性(AMS)。此信息的标准化和均质化使我们能够制作出三个主图,这些图综合了与比利牛斯山脉花岗岩AMS相关的所有信息。我们还将描述在数据库构建过程中发现的问题(可变地理位置,不同的发布信息等)。来自21个花岗岩体,数据库和合成图的信息(磁化率Km以及磁叶的方向,垂直于k3的平面和磁线k1的方向)使我们第一次看到这个重要的运动学和岩石学指标的完整图像。

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