Geochemical and mineralogical characteristics of fault gouge in the Median Tectonic Line, Japan: evidence for earthquake slip

• Published in: Earth, planets, and space planets, and space, 2014-05, Vol.66 (1), p.1, Article 36
• Main Authors: Ishikawa, Tsuyoshi, Hirono, Tetsuro, Matsuta, Noriko, Kawamoto, Kazuro, Fujimoto, Koichiro, Kameda, Jun, Nishio, Yoshiro, Maekawa, Yuka, Honda, Go
• Format: Article
• Language: English
• Subjects: 4. Seismology; Earth and Environmental Science; Earth Sciences; Geology; Geophysics/Geodesy; New Perspective of Subduction Zone Earthquake
• ISSN: 1880-5981; 1880-5981
• DOI: 10.1186/1880-5981-66-36

We carried out geochemical and mineralogical analyses on fault-zone rocks from the Anko section of the Median Tectonic Line in Nagano Prefecture, Japan, to investigate coseismic physicochemical processes in the fault zone. The latest fault zone in the Anko section contains cataclasite, fault breccia, and fault gouge of granitic composition, and brecciated basic schist. Protoliths of the granitic composition are from the Ryoke metamorphic belt and those of the basic schist from the Sambagawa metamorphic belt. X-ray diffraction analyses show a selective decrease of clay minerals coupled with an increase of amorphous phase in an intensely deformed layer of black gouge (5- to 10-cm thick). SEM observation reveals that the black gouge is characterized by a drastic reduction of grain size and abundant ultrafine particles of submicrometer to several tens of nanometers with well-rounded spheroidal shapes. These observations for the black gouge are indicative of strong mineral lattice distortion and granulation associated with earthquake slip. Geochemically, the black gouge is characterized by distinctly higher Li content and 87 Sr/ 86 Sr isotope ratio than surrounding cataclasites, breccias, and gouges, which have similar major element compositions. Model analysis reveals that the trace element composition of the black gouge is consistent with high-temperature (up to 250°C) coseismic fluid-rock interactions. Thermal and kinetic constraints indicate that there have been repeated slips on the fault at moderate depths (e.g., 600 m), although the tectonic process by which the fault zone has been uplifted and exposed in this area is not well understood.