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.

Language	:	Japanese
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Meeting title	:	日本地質学会第124年学術大会(2017愛媛)
Held date	:	2017/09
Location (city)	:	松山
Location (country)	:	日本
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Keywords	:	Underground Research Laboratory; Fracture; Granite; Quarts; Permeability
Research Facility	:	超深地層研究所
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Registration No. : BB20170558
JAEA Abstracts No. :
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