Temporal changes in electrical resistivity at Sakurajima volcano from continuous magnetotelluric observations

• Published in: Journal of volcanology and geothermal research Vol. 199; no. 1-2; pp. 165 - 175
• Main Authors: AIZAWA, Koki, KANDA, Wataru, OGAWA, Yasuo, IGUCHI, Masato, YOKOO, Akihiko, YAKIWARA, Hiroshi, SUGANO, Takayuki
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier 2011
• Subjects: Crystalline rocks; Earth sciences; Earth, ocean, space; Exact sciences and technology; Igneous and metamorphic rocks petrology, volcanic processes, magmas; Marine; Far East; Asia; Japan; INW, Japan; degassing; mixing; fracture networks; ground water; impedance; apparent resistivity; frequency; aquifers; hydrothermal system; craters; electrical resistivity; direction; inverse problem; magnetotellurics; volcanoes; equipment; volatile; magmas; tensor; intrusions; quality; depth; uplifts; tiltmeters; sea level; volatiles; resistivity
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/j.jvolgeores.2010.11.003

Continuous magnetotelluric (MT) measurements were conducted from May 2008 to July 2009 at Sakurajima, one of the most active volcanoes in Japan. Two observation sites were established at locations 3.3 km east and 3 km west-northwest of the summit crater. At both observation sites, the high-quality component of the impedance tensor (Zyx) showed variations in apparent resistivity of approximately +/- 20% and phase change of +/- 2 degree , which continued for 20-180 days in the frequency range between 320 and 4 Hz. The start of the period of changes in apparent resistivity approximately coincided with the start of uplift in the direction of the summit crater, as observed by a tiltmeter, which is one of the most reliable pieces of equipment with which to detect magma intrusion beneath a volcano. A 2D inversion of MT impedance suggests that the resistivity change occurred at a depth around sea level. One of the possible implications of the present finding is that the degassed volatiles migrated not only vertically through the conduit but also laterally through a fracture network, mixing with shallow groundwater beneath sea level and thereby causing the observed resistivity change.