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https://hdl.handle.net/2440/13826
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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Pring, A. | - |
dc.date.issued | 1998 | - |
dc.identifier.citation | Neues Jahrbuch fuer Geologie und Palaeontologie (Abhandlungen), 1998; 1(1):36-48 | - |
dc.identifier.issn | 0028-3649 | - |
dc.identifier.uri | http://hdl.handle.net/2440/13826 | - |
dc.description.abstract | The selenide assemblage at Iron Monarch, South Australia, has been characterized using electron microprobe analyses. The principal selenide minerals are: eucairite (Ag1.03Cu0.98Se0.99S0.01), naumannite (Ag2.03Cu0.02Se0.96S0.04) and bohdanowiczite (Ag0.96Cu0.04Bi1.01Se1.98S 0.02) and these occur with francisite in barite. Also present are clausthalite, bismuthinite, wittichenite and a number of copper sulfides. The occurrence is of hydrothermal origin and is thought to be associated with the intrusion of quartz diorite dykes, at temperatures between 133°C and 250°C. The compositions of coexisting sulfides and selenides show strong partitioning of Se into the Ag rich minerals and S into the Cu rich minerals. | - |
dc.language.iso | en | - |
dc.publisher | E. Schweizerbart | - |
dc.title | Selenides and sulphides from Iron Monarch, South Australia | - |
dc.type | Journal article | - |
pubs.publication-status | Published | - |
Appears in Collections: | Aurora harvest 7 Geology & Geophysics publications |
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