A 3-D electrical resistivity model beneath the focal zone of the 2008 Iwate-Miyagi Nairiku earthquake (M 7.2)

• Published in: Earth, planets, and space Vol. 66; no. 1; p. 1
• Main Authors: Ichihara, Hiroshi, Sakanaka, Shin'ya, Mishina, Masaaki, Uyeshima, Makoto, Nishitani, Tadashi, Ogawa, Yasuo, Yamaya, Yusuke, Mogi, Toru, Amita, Kazuhiro, Miura, Takuya
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 10.06.2014; Springer Nature B.V
• Subjects: 1. Geomagnetism; Earth and Environmental Science; Earth Sciences; Geofluid processes in subduction zones and mantle dynamics; Geology; Geophysics/Geodesy; Letter; Magnetotelluric; Inland earthquake; Iwate-Miyagi earthquake; 3-D resistivity
• ISSN: 1880-5981; 1880-5981
• DOI: 10.1186/1880-5981-66-50

The 2008 Iwate-Miyagi Nairiku earthquake (M 7.2) was a shallow inland earthquake that occurred in the volcanic front of the northeastern Japan arc. To understand why the earthquake occurred beneath an active volcanic area, in which ductile crust generally impedes fault rupture, we conducted magnetotelluric surveys at 14 stations around the epicentral area 2 months after the earthquake. Based on 56 sets of magnetotelluric impedances measured by the present and previous surveys, we estimated the three-dimensional (3-D) electrical resistivity distribution. The inverted 3-D resistivity model showed a shallow conductive zone beneath the Kitakami Lowland and a few conductive patches beneath active volcanic areas. The shallow conductive zone is interpreted as Tertiary sedimentary rocks. The deeper conductive patches probably relate to volcanic activities and possibly indicate high-temperature anomalies. Aftershocks were distributed mainly in the resistive zone, interpreted as a brittle zone, and not in these conductive areas, interpreted as ductile zones. The size of the brittle zone seems large enough for a fault rupture area capable of generating an M 7-class earthquake, despite the areas distributed among the ductile zones. This interpretation implies that 3-D elastic heterogeneity, due to regional geology and volcanic activities, controls the size of the fault rupture zone. Additionally, the elastic heterogeneities could result in local stress concentration around the earthquake area and cause faulting.