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zone of sulfide deposits is less stable and is often altered to secondary minerals, such as Anglesite.....more
and are therefore more stable.主要由銅和硫所構成，偶而也含有少量的鐵。有一組似雲母般的完全底面解理，可撕裂成極薄的片體，且具有彈性。 銅藍在地表的分布並不多，通常以次生礦.....more
deposits is less stable and is often altered to secondary minerals, such as Anglesite and white lead.....more
