Article: PGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County, Inner Mongolia: Indicator to source of metallogenic elements

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TitlePGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County, Inner Mongolia: Indicator to source of metallogenic elements
AuthorsChu, X2
Sun, M1
Zhou, M1
KeywordsDa Hinggan Area
Hypomagma
Pge Pattern
Polymetallic Deposit
Issue Date2002
PublisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/
CitationChinese Science Bulletin, 2002, v. 47 n. 13, p. 1119-1124 [How to Cite?]
DOI: http://dx.doi.org/10.1360/02tb9251
AbstractBy comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle Iherzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.
ISSN1001-6538
2011 Impact Factor: 1.321
2011 SCImago Journal Rankings: 0.102
DOIhttp://dx.doi.org/10.1360/02tb9251
ISI Accession Number IDWOS:000176393200014
ReferencesReferences in Scopus
DC Field
Value
dc.contributor.authorChu, X
dc.contributor.authorSun, M
dc.contributor.authorZhou, M
dc.date.accessioned2012-06-26T06:17:44Z
dc.date.available2012-06-26T06:17:44Z
dc.date.issued2002
dc.description.abstractBy comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle Iherzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.
dc.description.natureLink_to_subscribed_fulltext
dc.identifier.citationChinese Science Bulletin, 2002, v. 47 n. 13, p. 1119-1124 [How to Cite?]
DOI: http://dx.doi.org/10.1360/02tb9251
dc.identifier.doihttp://dx.doi.org/10.1360/02tb9251
dc.identifier.epage1124
dc.identifier.hkuros71240
dc.identifier.hkuros72243
dc.identifier.isiWOS:000176393200014
dc.identifier.issn1001-6538
2011 Impact Factor: 1.321
2011 SCImago Journal Rankings: 0.102
dc.identifier.issue13
dc.identifier.scopuseid_2-s2.0-20544447711
dc.identifier.spage1119
dc.identifier.urihttp://hdl.handle.net/10722/151154
dc.identifier.volume47
dc.languageeng
dc.publisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/
dc.publisher.placeChina
dc.relation.ispartofChinese Science Bulletin
dc.relation.referencesReferences in Scopus
dc.subjectDa Hinggan Area
dc.subjectHypomagma
dc.subjectPge Pattern
dc.subjectPolymetallic Deposit
dc.titlePGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County, Inner Mongolia: Indicator to source of metallogenic elements
dc.typeArticle
Author Affiliations
  1. The University of Hong Kong
  2. Institute of Geology and Geophysics Chinese Academy of Sciences