Aguilarite from the Camoola Reef, Maratoto Valley, New Zealand
نویسندگان
چکیده
Aguilarite, Ag4SeS, occurs in a hydrothermal vein deposit associated with sphalerite, chalcopyrite, galena, and native silver. Physical and chemical data agree with descriptions from Guanajuato (type locality). Differential thermal analysis of synthetic material indicates an inversion temperature of i22• T ~ The mineral crystallized late in the paragenetic sequence, probably slightly above 2oo ~
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