Cuprozheshengite

cuprozheshengite

theisite

veszelyite

hemimorphite

Images

Formula: Pb4CuZn2(AsO4)2(PO4)2(OH)2
Arsenate-phosphate, dongchuanite group
Crystal System: Triclinic
Specific gravity: 5.91 calculated
Hardness: 2½ to 3
Colour: Apple-green to greenish blue
Environments

Hydrothermal environments

Cuprozheshengite is a new mineral, approved in 2021 and to date (September 2024) reported only from the type localities.

Localities

There are two co-type localities, the Laochang ore field (Laochang Mine), Gejiu Sn-polymetallic ore field, Gejiu City, Honghe, Yunnan, China, and the Dongchuan Cu Mine, Sanguozhuang, Dongchuan District, Kunming, also in Yunnan, China.
At the type localities cuprozheshengite occurs as sub-millimeter greenish-blue hemispherical aggregates of microscopic blade-like crystals (AM 109.7.1248-1257).
The cuprozheshengite hemispheres are typically 0.3 to 1 mm in diameter and blades have lengths up to 0.2 mm but widths of only 10 to 50 μm. Cuprozheshengite occurs as a supergene mineral in fractures from copper sulphides along a regional redox boundary. Associated minerals include theisite, as well as hemimorphite, veszelyite and galena (Mindat).
All four dongchuanite group minerals occur at the Dongchuan copper mine. On the holotype specimen of cuprozheshengite, the cuprozheshengite is associated with veszelyite and galena. The new (in 2021) mineral arsenoveszelyite also occurs in this assemblage. These minerals occur in stratiform sediment-hosted copper deposits hosted within Mesoproterozoic (1,600 to 1,000 million years ago) rocks (AM 109.2174).
Cuprozheshengite from Sanguozhuang - Image

Back to Minerals