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Conference Paper: Platinum-group minerals in the Jinchuan complex, China
| Title | Platinum-group minerals in the Jinchuan complex, China |
|---|---|
| Authors | |
| Issue Date | 2005 |
| Citation | The 10th International Platinum Symposium on "Platinum-Group Elements - from Genesis to Beneficiation and Environmental Impacts", Oulu, Finland, 8-11 August 2005, p. 219-222 How to Cite? |
| Abstract | Platinum-group elements (PGE) and minerals (PGM), most commonly froodite
(PdBi2), michenerite (PdTeBi), padrnaite (PdBiSe), sperrylite (PtAsz) and irarsite (IrAsS),
have been analysed from the Jinchuan Ni-Cu-PGE sulphide deposit in the south western
margin of the North China Craton in China. PGM are most common in undeformed altered
samples formed as PGE were expelled from their magmatic base metal sulphide hosts during
alteration and then subsequently partially removed during shearing. It is proposed that the
Se-bearing PGM are associated with the presence of marbles in the host lithologies to the
Jinchuan complex. |
| Persistent Identifier | http://hdl.handle.net/10722/117212 |
| ISBN |
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Prichard, HM | en_HK |
| dc.contributor.author | Fisher, PC | en_HK |
| dc.contributor.author | McDonald, I | en_HK |
| dc.contributor.author | Zhou, MF | en_HK |
| dc.contributor.author | Wang, CY | en_HK |
| dc.date.accessioned | 2010-09-26T07:06:25Z | - |
| dc.date.available | 2010-09-26T07:06:25Z | - |
| dc.date.issued | 2005 | en_HK |
| dc.identifier.citation | The 10th International Platinum Symposium on "Platinum-Group Elements - from Genesis to Beneficiation and Environmental Impacts", Oulu, Finland, 8-11 August 2005, p. 219-222 | - |
| dc.identifier.isbn | 951-690-931-0 | - |
| dc.identifier.uri | http://hdl.handle.net/10722/117212 | - |
| dc.description.abstract | Platinum-group elements (PGE) and minerals (PGM), most commonly froodite (PdBi2), michenerite (PdTeBi), padrnaite (PdBiSe), sperrylite (PtAsz) and irarsite (IrAsS), have been analysed from the Jinchuan Ni-Cu-PGE sulphide deposit in the south western margin of the North China Craton in China. PGM are most common in undeformed altered samples formed as PGE were expelled from their magmatic base metal sulphide hosts during alteration and then subsequently partially removed during shearing. It is proposed that the Se-bearing PGM are associated with the presence of marbles in the host lithologies to the Jinchuan complex. | - |
| dc.language | eng | en_HK |
| dc.relation.ispartof | 10th International Platinum Symposium, "Platinum-Group Elements - from Genesis to Beneficiation and Environmental Impacts" August 8-11, 2005 Oulu, Finland: Extended abstracts | en_HK |
| dc.title | Platinum-group minerals in the Jinchuan complex, China | en_HK |
| dc.type | Conference_Paper | en_HK |
| dc.identifier.email | Zhou, MF: mfzhou@hkucc.hku.hk | en_HK |
| dc.identifier.authority | Zhou, MF=rp00844 | en_HK |
| dc.description.nature | link_to_OA_fulltext | - |
| dc.identifier.hkuros | 109887 | en_HK |