1966-2016年地球磁场沿波兰主要构造单元剖面的相对长期变化(Zgorzelec-Wiżajny剖面)

IF 0.4 Q4 ENVIRONMENTAL SCIENCES
Anna Wojas, T. Grabowska
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引用次数: 0

摘要

本文总结了1966-2016年近50年来Zgorzelec-Wiżajny剖面(Z-W剖面)总磁场强度(TMI)的相对局地长期变化研究。Z-W剖面(约650公里长)穿过欧洲的主要构造单元,包括古生代台地(PP)的Variscan褶皱带、跨欧洲缝合带(TESZ)和东欧克拉通(EEC)的波兰部分。在剖面的31个地点进行了TMI测量,并将其简化为位于贝尔斯克的中央地球物理观测站的基础记录。基于相对地磁场值随时间变化的线性近似,计算了以纳特斯拉[nT]为单位的相对年时间变化(相对长期变化)。相对地磁场值的研究表明,与PP和TESZ相比,EEC地磁场的长期变化较慢。然而,它们显示出这些变化的幅度较低。一个有趣的现象是,从2000年开始,TMI的相对值(趋势)的时间发生了快速变化,也表示为每年的相对长期变化,在PP地区尤其明显。在定性意义上,相对长期变化显示了与波兰境内主要地质单元的相关性,也是岩石圈地震和地热模型的重要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Relative secular variations of the Earth’s magnetic field in the years 1966–2016 along the profile across the main tectonic units of Poland (Zgorzelec-Wiżajny profile)
The paper summarizes 50 years of research on relative local secular variations of the total magnetic intensity (TMI) along Zgorzelec-Wiżajny profile (Z-W profile) through the years 1966–2016. The Z-W profile (approximately 650 km length) cuts through Europe’s major tectonic units, including a zone of Variscan folds in the Paleozoic platform (PP), the Trans-European Suture Zone (TESZ) and the Polish part of the East European Craton (EEC). Measurements of TMI were made at 31 sites of the profile and reduced to the base recordings at the Central Geophysical Observatory in Belsk. Based on linear approximations of relative geomagnetic field values changes in time, relative annual changes in time (relative secular variations) expressed in nanoteslas [nT] per year were calculated. The study on relative geomagnetic field values revealed slower secular variations of the geomagnetic field in EEC as compared to those in PP and TESZ. However, they show lower amplitudes of these variations. An interesting phenomenon are rapid changes in the time of the relative values (trends) of TMI starting from the year 2000, also expressed as the relative secular variations per year, particularly visible in PP area. In the qualitative sense, relative secular variations show a correlation with the main geological units in the Polish territory and also important elements in the seismic and geothermal model of the lithosphere.
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