Takanelite

takanelite

nsutite

braunite

halloysite

Images

Formula: (Mn2+,Ca)2x(Mn4+)1-xO2.0.7H2O
Hydrated oxide, birnessite group, forms a series with ranciéite, manganese-bearing mineral
Crystal system: Hexagonal
Specific gravity: 3.41 measured, 3.98 calculated
Hardness: 5
Streak: Dark brown
Colour: Grey, black, grey-brown
Luminescence: Not fluorescent under UV
Solubility: Etch reactions with concentrated hydrochloric acid and with concentrated nitric acid
Environments

Sedimentary environments
Metamorphic environments

Localities

At the type locality, the Nomura mine, Nomura, Seiyo City, Ehime Prefecture, Japan, takanelite occurs in irregularly shaped nodules 1 to 15 cm across, composed of microscopic intergrowths with braunite, halloysite, goethite and quartz, in the oxidation zone of the braunite - rhodochrosite - caryopilite bedded deposit in low-grade metamorphosed cherts (AM 56.1487-1489).

At the Janggun mine, Bonghwa County, North Gyeongsang Province, South Korea, takanelite occurs as massive or colloform (kidney-shaped) bands in nsutite-rich ores of the supergene zone derived through oxidation of rhodochrosite. It is usually replaced by nsutite or pyrolusite along the colloform bands or in a random fashion, showing gradational contacts. The manganese ore containing this mineral is grey in colour and very hard because of the presence of abundant nsutite. It is characterized by small, grey shiny or greasy colloform areas (AM 76.1426-1430).

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