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廣島大學地學研究報告 14 号
1965-02-22 発行
Thermal Studies of Some Minerals, No. 2
UMEGAKI Yoshiharu
ONO Takashi
Abstract
For the purpose of discerning the inner structures of chlorite group from one another, thermal variations of the related specimens collected from a chromite deposit in serpentinite have been continuously traced during the heated states at various temperatures up to ca. 950°C kept respectively for long enough hours by means of X-ray diffractometer ac-companying the specific heating apparatus and a few data obtained through infra-red absorption have been added to for reference.
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PP. 345 - 368