Constraining the timing of brittle deformation and faulting in the Toki granite, central Japan

S. Yamasaki; Horst Zwingmann; K. Yamada; T. Tagami; K. Umeda

doi:10.1016/j.chemgeo.2013.05.005

Constraining the timing of brittle deformation and faulting in the Toki granite, central Japan

S. Yamasaki, Horst Zwingmann, K. Yamada, T. Tagami, K. Umeda

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28 Citations (Scopus)

Abstract

Constraining of the timing of fault zone formation is of fundamental geotectonic importance to understand structural evolution and brittle fault processes. Here, we present authigenic illite K-Ar age data from brittle fault zones comprising two gouges within the Toki granite, central Japan. The gouge samples were collected at depths of 252.9 and 403.7. m from a shaft at the Mizunami Underground Research Laboratory, and were separated into five grain-size fractions (

Original language	English
Pages (from-to)	168-174
Journal	Chemical Geology
Volume	351
DOIs	https://doi.org/10.1016/j.chemgeo.2013.05.005
Publication status	Published - 2013

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10.1016/j.chemgeo.2013.05.005

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title = "Constraining the timing of brittle deformation and faulting in the Toki granite, central Japan",

abstract = "Constraining of the timing of fault zone formation is of fundamental geotectonic importance to understand structural evolution and brittle fault processes. Here, we present authigenic illite K-Ar age data from brittle fault zones comprising two gouges within the Toki granite, central Japan. The gouge samples were collected at depths of 252.9 and 403.7. m from a shaft at the Mizunami Underground Research Laboratory, and were separated into five grain-size fractions (",

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AU - Yamasaki, S.

AU - Zwingmann, Horst

AU - Yamada, K.

AU - Tagami, T.

AU - Umeda, K.

PY - 2013

Y1 - 2013

N2 - Constraining of the timing of fault zone formation is of fundamental geotectonic importance to understand structural evolution and brittle fault processes. Here, we present authigenic illite K-Ar age data from brittle fault zones comprising two gouges within the Toki granite, central Japan. The gouge samples were collected at depths of 252.9 and 403.7. m from a shaft at the Mizunami Underground Research Laboratory, and were separated into five grain-size fractions (

AB - Constraining of the timing of fault zone formation is of fundamental geotectonic importance to understand structural evolution and brittle fault processes. Here, we present authigenic illite K-Ar age data from brittle fault zones comprising two gouges within the Toki granite, central Japan. The gouge samples were collected at depths of 252.9 and 403.7. m from a shaft at the Mizunami Underground Research Laboratory, and were separated into five grain-size fractions (

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DO - 10.1016/j.chemgeo.2013.05.005

M3 - Article

SN - 0009-2541

VL - 351

SP - 168

EP - 174

JO - Chemical Geology

JF - Chemical Geology

ER -

Constraining the timing of brittle deformation and faulting in the Toki granite, central Japan

Abstract

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