菲律宾塔尔火山主火山湖磁力及水深测量:序报

洋一 笹井, 誠 原田, Julio P. Sabit, J. Zlotnicki, 良和 田中, Juan M. Cordon, 誠也 上田, 年恭 長尾, Jame S. Sincioco
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引用次数: 2

摘要

对菲律宾塔阿尔火山岛上的主火山口湖(Main Crater Lake, MCL)进行了地磁和地形测量,以确定该火山的喷发机制。在MCL北部附近的湖底发现了一个土丘,这在1986年的调查中没有出现。它被称为M丘,形成于1986年至2008年之间,在1990年代初MCL东北岸开始的新喷气孔活动期间。地磁测量未发现与土丘对应的总磁场(TMF)异常,说明土丘M是非磁性的。该地点与2005年初火山危机期间ASTER卫星探测到的高温区域的位置一致。M丘可能含有火山气体沉积的化学物质(氯化物或硫化物?)在火山岛的两个地热区设置了两台连续记录的质子磁力计。在火山岛上6个月的TMF变化记录显示了监测火山活动的良好稳定性和精度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
フィリピン・タール火山・主火口湖の磁気および水深測量 : 序報
A geomagnetic and topographic survey of the Main Crater Lake (MCL) on Volcano Island, Taal volcano, the Philippines, was conducted to identify the eruption mechanism of the volcano. A mound at the lake bottom was found near the northern part of MCL, which was not present at the 1986 survey. Called mound M, it was formed between 1986 and 2008 during a period of new fumarole activity, which started on the northeastern shore of MCL in the early 1990's. A geomagnetic survey found no Total Magnetic Field (TMF) anomaly corresponding to the mound, which implies that mound M is non-magnetic. The site coincides with the location of a high-temperature area detected by the ASTER satellite during the early 2005 volcanic crisis. The mound M might contain chemicals (chloride or sulphide?) deposited from volcanic gas. Two continuously-recording proton magnetometers were set up at two geothermal areas on Volcano Island. Recordings of TMF variations obtained over six months on Volcano Island showed excellent stability and precision for monitoring the volcanic activity.
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