標 本 名: | エピドート / ダイオプサイド / クリノクロア石 / 磁鉄鉱（マグネタイト)
| 化学組成: | Ca3Fe3+2(SiO4)3 / CaMgSi2O6 / (Mg,Fe2+)5 Al[(OH)8|AlSi3O10] / Fe2+Fe23+O4 | サ イ ズ: | | 重量: | | 透明: | | 数量: | | 産地: | Marki Khel, Khogyani, Nangarhar Province (Ningarhar Province), アフガニスタン (Afghanistan) | This is a paragenesis with olive-green epidote, diopside, magnetite octahedrons and clinochlore crystals. Except a few tiny damages along the periphery of the specimen nothing is damaged. Some more internal crystals seem to be damaged but I affect fully recrystallized. Nice paragenesis from Pakistan
| 
