Ni-rich mineral nepouite explains the exceptional green color of speleothems Martin Vlieghe, Gaëtan Rochez, Stéphane Pire-Stevenne, Jean-Yves Storme, Augustin Dekoninck, Yves Vanbrabant, Olivier Namur, Yishen Zhang, Alicia Van Ham-Meert, JeanPierre Donnadieu, Michel Berbigé, Jean-Luc Hasbroucq & Johan Yans Abstract:Speleothems are secondary mineral structures typically found in karstic caves and usually composed of calcite or aragonite. Despite being naturally white, some might exhibit unusual colors, such as blue, black, red, yellow or green.
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