Genesis of Cryogenian Datangpo manganese deposit: Hydrothermal influence and episodic post-glacial ventilation of Nanhua Basin, South China
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New elemental and Srsingle bondclass="glyphImg imgLazyJSB">Nd isotope data from Cryogenian Datangpo manganese deposit, Guizhou, China

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The two main components of the Mn-ore deposit are Mn-carbonates and Mn-bearing aluminosilicates.

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Mn-carbonates formed by reaction of hydrothermally sourced Mn and sedimentary organic matter

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Aluminosilicates derived from weathering of Neoproterozoic continental basalts on Yangtze Block

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The Datangpo Mn deposit conforms to the “episodic ventilation” model of metallogenesis.

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