Reference Type | Journal (article/letter/editorial) |
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Title | Aguilarite from the Camoola Reef, Maratoto
Valley, New Zealand |
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Journal | Mineralogical Magazine |
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Authors | Main, J. V. | Author |
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Rodgers, K. A. | Author |
Kobe, H. W. | Author |
Woods, C. P. | Author |
Year | 1972 (December) | Volume | 38 |
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Issue | 300 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-300-961.pdf+ |
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DOI | doi:10.1180/minmag.1972.038.300.07Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6613 | Long-form Identifier | mindat:1:5:6613:0 |
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|
GUID | 0 |
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Full Reference | 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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Plain Text | 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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In | (1972, December) Mineralogical Magazine Vol. 38 (300) Mineralogical Society |
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Abstract/Notes | SummaryAguilarite, 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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