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 |
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Hauptverfasser: | , , , , |
Format: | Artikel |
Sprache: | eng |
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