In a broad sense, it is a general term for epidote group minerals with the chemical composition X2Y3Z3 (O,OH,F) 13 (where X is Ca,Ce3 + ,La3 + ,Y3 + ,Th,Fe2 + ,Mn2 + ,Mn3 + ,Y is Al,Fe3 + ,Mn3 + ,Fe2 + ,Mn2 + ,Ti,Z are Si,Be). In a narrow sense, it is a mineral with the chemical composition Ca2 (Al, Fe3 + ) 3Si3O12 (OH) that belongs to the epidote group along with zoisite , pomegranate, and allanite . Minerals with low Fe3 + content and close to Ca2Al3Si3O12 (OH) are sometimes called clinozoisite, and those with high Fe3 + content and close to Ca2Al2Fe3 + Si3O12 (OH) are sometimes called pistacite. Source: Heibonsha World Encyclopedia, 2nd Edition Information |
広義には化学組成X2Y3Z3(O,OH,F)13(ここでXはCa,Ce3+,La3+,Y3+,Th,Fe2+,Mn2+,Mn3+,YはAl,Fe3+,Mn3+,Fe2+,Mn2+,Ti,ZはSi,Be)で表される緑レン石族鉱物の総称。狭義には,ゾイサイト,紅レン石,褐レン石とともに緑レン石族に属する,化学組成Ca2(Al,Fe3+)3Si3O12(OH)の鉱物。Fe3+が少なくCa2Al3Si3O12(OH)に近い成分のものをクリノゾイサイトclinozoisite,Fe3+が多くCa2Al2Fe3+Si3O12(OH)に近いものをピスタサイトpistaciteと呼ぶことがある。
出典 株式会社平凡社世界大百科事典 第2版について 情報 |
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