HR: 1340h
AN: T23A-0567    [Abstracts]
TI: Zircon fission-track thermochronology of the Nojima Fault zone, Japan
AU: * Tagami, T
EM: tagami@kueps.kyoto-u.ac.jp
AF: Div. Earth Planet. Sci., Kyoto Univ., Sakyo-ku, Kyoto, 606-8502 Japan
AU: Murakami, M
EM: murakami@kueps.kyoto-u.ac.jp,
AF: Div. Earth Planet. Sci., Kyoto Univ., Sakyo-ku, Kyoto, 606-8502 Japan
AB: Fission track (FT) thermochronologic analysis was performed on zircon separates from rocks in and around the Nojima fault, which was activated during the 1995 Kobe earthquake. Samples were collected from the University Group 500 m (UG-500) borehole, Geological Survey of Japan 750 m (GSJ-750) borehole, the fault trench at Hirabayashi, and nearby outcrops. Zircon FT data from the UG-500 borehole record ~2.5 Ma cooling in the zircon partial annealing zone (ZPAZ) for samples within ~3 m from the fault plane, whereas those of the GSJ-750 borehole record ~35 Ma cooling within ~25 m from the fault. On the basis of one-dimensional heat conduction modeling as well as the consistency between the degree of FT annealing and the degree of deformation/alteration of borehole rocks, these cooling ages in both boreholes are interpreted as consequences of ancient thermal overprints by heat transfer or dispersion via fluids in the fault zone. For the fault trench samples, zircon FTs of the 2 - 10 mm thick pseudotachylyte layer were totally reset (or remained reset) and subsequently cooled at ~56 Ma, which is interpreted as the time of final cooling through ZPAZ immediately after the pseudotachylyte formation. It is, therefore, suggested that the present Nojima fault system was reactivated in the Middle Quaternary from an ancient fault initiated at ~56 Ma at mid-crustal depths.
DE: 8130 Heat generation and transport
DE: 8164 Stresses--crust and lithosphere
DE: 5418 Heat flow
DE: 1035 Geochronology
DE: 1045 Low-temperature geochemistry
SC: Tectonophysics [T]
MN: 2004 AGU Fall Meeting