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Main, J. V., Rodgers, K. A., Kobe, H. W., Woods, C. P. (1972) Aguilarite from the Camoola Reef, Maratoto Valley, New Zealand. Mineralogical Magazine, 38 (300) 961-964 doi:10.1180/minmag.1972.038.300.07

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Reference TypeJournal (article/letter/editorial)
TitleAguilarite from the Camoola Reef, Maratoto Valley, New Zealand
JournalMineralogical Magazine
AuthorsMain, J. V.Author
Rodgers, K. A.Author
Kobe, H. W.Author
Woods, C. P.Author
Year1972 (December)Volume38
Issue300
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_38/38-300-961.pdf+
DOIdoi:10.1180/minmag.1972.038.300.07Search in ResearchGate
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Mindat Ref. ID6613Long-form Identifiermindat:1:5:6613:0
GUID0
Full ReferenceMain, J. V., Rodgers, K. A., Kobe, H. W., Woods, C. P. (1972) Aguilarite from the Camoola Reef, Maratoto Valley, New Zealand. Mineralogical Magazine, 38 (300) 961-964 doi:10.1180/minmag.1972.038.300.07
Plain TextMain, J. V., Rodgers, K. A., Kobe, H. W., Woods, C. P. (1972) Aguilarite from the Camoola Reef, Maratoto Valley, New Zealand. Mineralogical Magazine, 38 (300) 961-964 doi:10.1180/minmag.1972.038.300.07
In(1972, December) Mineralogical Magazine Vol. 38 (300) Mineralogical Society
Abstract/NotesSummaryAguilarite, 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 122±1 °C. The mineral crystallized late in the paragenetic sequence, probably slightly above 200 °C.


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