標 本 名: | 斜黝簾石- エピドート ( Clinozoisite-Epidote Series )
| 化学組成: | Ca2(Al,Fe3+,Cr)3[O|OH|SiO4|Si2O7] | サ イ ズ: | | 重量: | | 透明: | | 数量: | | 産地: | Tormiq valley (Tormic; Tormik; Tormig), Haramosh Mts., Skardu District, Baltistan, Northern Areas, パキスタン (Pakistan) | Here you get a clinozoisite crystal with predominantly cutting grade transparency. The specimen shows several healing fissures evidence for some tectonic activities during the crystal growth. The crystal shows only fracture planes at the base the other side is terminated and another twin crystal is angular attached. Pretty big specimen with a strong luster, fine transparency and crystal striations.
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