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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 2
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
2012 Impact Factor: 1.319
2012 SCImago Journal Rankings: 0.382
 
DOIhttp://dx.doi.org/10.1360/02tb9251
 
ISI Accession Number IDWOS:000176393200014
 
ReferencesReferences in Scopus
 
DC FieldValue
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
2012 Impact Factor: 1.319
2012 SCImago Journal Rankings: 0.382
 
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
 
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Author Affiliations
  1. The University of Hong Kong
  2. Institute of Geology and Geophysics Chinese Academy of Sciences