格尔木台地磁短周期变化与周围地震的对应关系
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
计算分析了位于青藏高原东北部的格尔木地磁台1987年1月至1997年3月的地磁周期T=9~200min的复转换函数A的模|A|、B的模|B|、总方差σz的帕金森矢量或韦氏矢量,并将其与同期格尔木周围350km范围内MS≥5.0的8个地震进行了对比研究,发现周期为9,75min的|A|、周期为9min的|B|在震前有明显异常,总方差σz亦有一定的对应效果,帕金森或韦氏矢量在震前指向震中位置。
In this paper,the consecutive monthly variations of complex transfer function moduli |A| and |B| of geomagnetic field in the periods of T =9~200 min,the total variance σ z ,the magnetic azimuth α p and the Parkinson or Wiess vector from Jan.1987 to Mar.1997 at Seismic Station of Golmud,which is located in the northeast of Qinghai Plateau,were calculated and analyzed.They were compared and studied with eight earthquakes( M S≥5 0)occurred at the same time within the range of 350 km around the station.It was found that |A| of period 9,75 min and |B| of 9 min were strikingly anomalous prior to the earthquakes.The total variance σ z and the local earthquakes also have a certain corresponding effect.The Parkinson or Wiess vector pointed to the epicenters before these earthquakes.
引文

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心