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Article: Late paleoproterozoic to early mesoproterozoic tangdan sedimentary rock-hosted strata-bound copper deposit, yunnan province, southwest china

TitleLate paleoproterozoic to early mesoproterozoic tangdan sedimentary rock-hosted strata-bound copper deposit, yunnan province, southwest china
Authors
Issue Date2012
PublisherSociety of Economic Geologists, Inc.. The Journal's web site is located at http://www.segweb.org/publications/journal.aspx
Citation
Economic Geology, 2012, v. 107 n. 2, p. 357-375 How to Cite?
AbstractSedimentary rock-hosted strata-bound copper deposits are widespread in the Kangdian region of the Central Yunnan and southern Sichuan provinces, southwest China. The deposits occur within weakly metamorphosed rocks of the late Paleoproterozoic to early Mesoproterozoic Dongchuan Group and are spatially associated with discordant breccia bodies that are interpreted as having formed from salt diapirs. The Tangdan deposit, the largest in the region, consists of stratiform and discordant orebodies predominantly hosted in dolostones immediately above hematitic sandstones and siltstones and in black shales above the dolostones. Host rocks for the deposit display a complex paragenetic sequence of alteration and mineralization. Early sodic alteration resulted in the growth of both albite and ferroan dolomite. Later potassic alteration resulted in the precipitation of potassium feldspar and locally biotite in argillaceous layers. Sulfide mineralization was temporally and spatially associated with silicification that postdated both sodic and potassic alteration. Textures suggest that silicification may have preferentially affected evaporite minerals in the dolostones. Copper sulfides form bedding-parallel disseminations, veinlets and, to a lesser extent, stockworks. Copper sulfides are dominated by chalcopyrite with lesser bornite and chalcocite. Hypogene chalcopyrite and bornite from the Tangdan deposit have d34S values that range from -12.7 to +9.3% and cluster between -3 to +5% The values suggest derivation from Mesoproterozoic marine sulfates. The dolostone host rocks have relatively homogeneous C and O isotope values ranging from 0.2 to 1.3% d13CV-PDB and from 19.1 to 22.4% d18OV-SNOW. Carbonate minerals in quartz sulfide veins display both a trend toward lighter oxygen isotope values and a trend to significantly lighter carbon isotope values. The light carbon isotope values suggest involvement of organic carbon in the mineralizing process. Alteration and mineralization at Tangdan probably occurred via interaction of oxidized saline brines derived from the underlying red-bed sequence with partially to wholly lithified dolostones. Sulfide precipitation was likely due to both redox reactions and mineralizing fluid pH changes resulting from dolomite and sulfate dissolution. The styles of alteration and mineralization at the Tangdan deposit are similar to those observed in the Central African Copperbelt, particularly the dolostone-hosted orebodies in the Mines Series of the Democratic Republic of Congo. © 2012 Society of Economic Geologists, Inc.
Persistent Identifierhttp://hdl.handle.net/10722/151365
ISSN
2015 Impact Factor: 2.487
References

 

DC FieldValueLanguage
dc.contributor.authorZhao, XFen_US
dc.contributor.authorZhou, MFen_US
dc.contributor.authorHitzman, MWen_US
dc.contributor.authorLi, JWen_US
dc.contributor.authorBennett, Men_US
dc.contributor.authorMeighan, Cen_US
dc.contributor.authorAnderson, Een_US
dc.date.accessioned2012-06-26T06:21:12Z-
dc.date.available2012-06-26T06:21:12Z-
dc.date.issued2012en_US
dc.identifier.citationEconomic Geology, 2012, v. 107 n. 2, p. 357-375en_US
dc.identifier.issn0361-0128en_US
dc.identifier.urihttp://hdl.handle.net/10722/151365-
dc.description.abstractSedimentary rock-hosted strata-bound copper deposits are widespread in the Kangdian region of the Central Yunnan and southern Sichuan provinces, southwest China. The deposits occur within weakly metamorphosed rocks of the late Paleoproterozoic to early Mesoproterozoic Dongchuan Group and are spatially associated with discordant breccia bodies that are interpreted as having formed from salt diapirs. The Tangdan deposit, the largest in the region, consists of stratiform and discordant orebodies predominantly hosted in dolostones immediately above hematitic sandstones and siltstones and in black shales above the dolostones. Host rocks for the deposit display a complex paragenetic sequence of alteration and mineralization. Early sodic alteration resulted in the growth of both albite and ferroan dolomite. Later potassic alteration resulted in the precipitation of potassium feldspar and locally biotite in argillaceous layers. Sulfide mineralization was temporally and spatially associated with silicification that postdated both sodic and potassic alteration. Textures suggest that silicification may have preferentially affected evaporite minerals in the dolostones. Copper sulfides form bedding-parallel disseminations, veinlets and, to a lesser extent, stockworks. Copper sulfides are dominated by chalcopyrite with lesser bornite and chalcocite. Hypogene chalcopyrite and bornite from the Tangdan deposit have d34S values that range from -12.7 to +9.3% and cluster between -3 to +5% The values suggest derivation from Mesoproterozoic marine sulfates. The dolostone host rocks have relatively homogeneous C and O isotope values ranging from 0.2 to 1.3% d13CV-PDB and from 19.1 to 22.4% d18OV-SNOW. Carbonate minerals in quartz sulfide veins display both a trend toward lighter oxygen isotope values and a trend to significantly lighter carbon isotope values. The light carbon isotope values suggest involvement of organic carbon in the mineralizing process. Alteration and mineralization at Tangdan probably occurred via interaction of oxidized saline brines derived from the underlying red-bed sequence with partially to wholly lithified dolostones. Sulfide precipitation was likely due to both redox reactions and mineralizing fluid pH changes resulting from dolomite and sulfate dissolution. The styles of alteration and mineralization at the Tangdan deposit are similar to those observed in the Central African Copperbelt, particularly the dolostone-hosted orebodies in the Mines Series of the Democratic Republic of Congo. © 2012 Society of Economic Geologists, Inc.en_US
dc.languageengen_US
dc.publisherSociety of Economic Geologists, Inc.. The Journal's web site is located at http://www.segweb.org/publications/journal.aspxen_US
dc.relation.ispartofEconomic Geologyen_US
dc.titleLate paleoproterozoic to early mesoproterozoic tangdan sedimentary rock-hosted strata-bound copper deposit, yunnan province, southwest chinaen_US
dc.typeArticleen_US
dc.identifier.emailZhou, MF:mfzhou@hkucc.hku.hken_US
dc.identifier.authorityZhou, MF=rp00844en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.2113/econgeo.107.2.357en_US
dc.identifier.scopuseid_2-s2.0-84863391851-
dc.identifier.hkuros206533-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-84858653175&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume107en_US
dc.identifier.issue2en_US
dc.identifier.spage357en_US
dc.identifier.epage375en_US
dc.identifier.eissn1554-0774-
dc.publisher.placeUnited Statesen_US
dc.identifier.scopusauthoridZhao, XF=55113262200en_US
dc.identifier.scopusauthoridZhou, MF=7403506005en_US
dc.identifier.scopusauthoridHitzman, MW=55116049100en_US
dc.identifier.scopusauthoridLi, JW=55116579100en_US
dc.identifier.scopusauthoridBennett, M=55117676900en_US
dc.identifier.scopusauthoridMeighan, C=55114520200en_US
dc.identifier.scopusauthoridAnderson, E=55113084000en_US

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