File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

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

TitlePGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County, Inner Mongolia: Indicator to source of metallogenic elements
Authors
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/
Citation
Chinese Science Bulletin, 2002, v. 47 n. 13, p. 1119-1124 How to Cite?
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.
Persistent Identifierhttp://hdl.handle.net/10722/151154
ISSN
2014 Impact Factor: 1.579
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorChu, Xen_US
dc.contributor.authorSun, Men_US
dc.contributor.authorZhou, Men_US
dc.date.accessioned2012-06-26T06:17:44Z-
dc.date.available2012-06-26T06:17:44Z-
dc.date.issued2002en_US
dc.identifier.citationChinese Science Bulletin, 2002, v. 47 n. 13, p. 1119-1124en_US
dc.identifier.issn1001-6538en_US
dc.identifier.urihttp://hdl.handle.net/10722/151154-
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.en_US
dc.languageengen_US
dc.publisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/en_US
dc.relation.ispartofChinese Science Bulletinen_US
dc.subjectDa Hinggan Areaen_US
dc.subjectHypomagmaen_US
dc.subjectPge Patternen_US
dc.subjectPolymetallic Depositen_US
dc.titlePGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County, Inner Mongolia: Indicator to source of metallogenic elementsen_US
dc.typeArticleen_US
dc.identifier.emailSun, M:minsun@hku.hken_US
dc.identifier.emailZhou, M:mfzhou@hkucc.hku.hken_US
dc.identifier.authoritySun, M=rp00780en_US
dc.identifier.authorityZhou, M=rp00844en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1360/02tb9251en_US
dc.identifier.scopuseid_2-s2.0-20544447711en_US
dc.identifier.hkuros71240-
dc.identifier.hkuros72243-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-20544447711&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume47en_US
dc.identifier.issue13en_US
dc.identifier.spage1119en_US
dc.identifier.epage1124en_US
dc.identifier.isiWOS:000176393200014-
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridChu, X=7102057269en_US
dc.identifier.scopusauthoridSun, M=25932315800en_US
dc.identifier.scopusauthoridZhou, M=7403506005en_US

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats