:The Na<SUB>2</SUB>O anomaly in the footwall acid lavas
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概要
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Previous studies of geochemical prospecting in the Hokuroku region have revealed that acid lavas underlying kuroko deposits are in general significantly depleted in Na<SUB> 2</SUB>O in comparison with those on which no kuroko deposits exist. The Na<SUB> 2</SUB>O content of the footwall acid lavas may thus provide a practical geochemical indicator which enables us to delimit a promising area for prospecting around the known kuroko deposits.<BR>The Na<SUB> 2</SUB>O variation in the footwall acid lavas has extensively been examined in the vicinity of the Uchinotai-Uwamuki deposits, Kosaka mine and of the Fukazawa deposits, Hanaoka mine. The following results have been obtained:<BR>1) The most economical threshold to delimit the promising area can be set at Na<SUB> 2</SUB>O = 0.36 wt% in the Uchinotai-Uwamuki area and at Na<SUB> 2</SUB>O = 0.32 wt% in the Fukazawa area.<BR>2) The promising areas thus defined are two or three times as large as the presently known extents of these deposits.<BR>3) Some new orebodies have successfully been discoverd by this method.
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