Extensive normal faulting during exhumation revealed by the spatial variation of phengite K – A r ages in the S ambagawa metamorphic rocks, central S hikoku, SW J apan

Metamorphic rocks experience change in the mode of deformation from ductile flow to brittle failure during their exhumation. We investigated the spatial variation of phengite K – A r ages of pelitic schist of the S ambagawa metamorphic rocks (sensu lato) from the S aruta R iver area, central S hikok...

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Veröffentlicht in:The island arc 2015-06, Vol.24 (2), p.245-262
Hauptverfasser: Takeshita, Toru, Yagi, Koshi, Gouzu, Chitaro, Hyodo, Hironobu, Itaya, Tetsumaru
Format: Artikel
Sprache:eng
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