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Report No.

Is a fracture in Toki granite a trace of high temperature fluid in the past?

Nohara, Tsuyoshi  ; Tsuchiya, Noriyoshi*

A trace of a high-temperature fluid in the Toki granite is investigated using pre-existing boring core of MIU. Fractures filled with secondary formed biotite and pores filled with quarts are recognized. It is considered that these filling minerals are traces of a high-temperature fluid in the past.



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