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Article: Heterogeneous Os isotope compositions in the Kalatongke sulfide deposit, NW China: the role of crustal contamination
| Title | Heterogeneous Os isotope compositions in the Kalatongke sulfide deposit, NW China: the role of crustal contamination |
|---|---|
| Authors | |
| Keywords | Crustal contamination Re-Os isotopes Sulfide segregation Sulfide-bearing intrusions Sulfides |
| Issue Date | 2012 |
| Publisher | Springer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00126/index.htm |
| Citation | Mineralium Deposita, 2012, v. 47 n. 7, p. 731-738 How to Cite? |
| Abstract | Re-Os isotope compositions of mantle-derived magmas are highly sensitive to crustal contamination because the crust and mantle have very different Os isotope compositions. Crustal contamination may trigger S saturation and thus the formation of magmatic Ni-Cu-(PGE) sulfide deposits. The ∼287-Ma Kalatongke norite intrusion of NW China are hosted in carboniferous tuffaceous rocks and contain both disseminated and massive sulfide mineralization. The Re-Os isotope compositions in the intrusion are highly variable. Norite and massive sulfide ores have γ Os values ranging from +59 to +160 and a Re-Os isochron age of 239 ± 51 Ma, whereas disseminated sulfide ores have γ Os values from +117 to +198 and a Re-Os isochron age of 349 ± 34 Ma. The variability of Os isotope compositions can be explained as the emplacement of two distinct magma pulses. Massive sulfide ores and barren norite in the intrusion formed from the same magma pulse, whereas the disseminated sulfide ores with more radiogenic Os isotopes formed from another magma pulse which underwent different degrees of crustal contamination. Re-Os isotopes may not be suitable for dating sulfide-bearing intrusions that underwent variable degrees of crustal contamination to form magmatic sulfide deposits. © 2012 The Author(s). |
| Persistent Identifier | http://hdl.handle.net/10722/147111 |
| ISSN | 2023 Impact Factor: 4.4 2023 SCImago Journal Rankings: 1.913 |
| ISI Accession Number ID | |
| References | Amelin Y, Li CS, Naldrett AJ (1999) Geochronology of the Voisey’s Bay intrusion, Labrador, Canada, by precise U–Pb dating of coexisting baddeleyite, zircon, and apatite. Lithos 47:33–51 doi: 10.1016/S0024-4937(99)00006-7 Brenan JM (2002) Re–Os fractionation in magmatic sulfide melt by monosulfide solid solution. Earth Planet Sci Lett 199:257–268 doi: 10.1016/S0012-821X(02)00581-2 Brenan JM (2008) Re–Os fractionation by sulfide melt–silicate melt partitioning: a new spin. Chem Geol 248:140–165 doi: 10.1016/j.chemgeo.2007.09.003 Brenan JM, Cherniak DJ, Rose LA (2000) Diffusion of osmium in pyrrhotite and pyrite: implications for closure of the Re–Os isotopic system. Earth Planet Sci Lett 180:399–413 doi: 10.1016/S0012-821X(00)00165-5 Campbell IH, Naldrett AJ (1979) The influence of silicate:sulfide ratios on the geochemistry of magmatic sulfides. Econ Geol 74:1503–1506 doi: 10.2113/gsecongeo.74.6.1503 Campbell IH, Czamanske GK, Fedorenko VA, Hill RI, Stepanov V, Kunilov VE (1992) Synchronism of the Siberian traps and the Permian–Triassic boundary. Science 258:1760–1763 doi: 10.1126/science.258.5089.1760 Cohen AS, Burnham OM, Hawkesworth CJ, Lightfoot PC (2000) Pre-emplacement Re–Os ages from ultramafic inclusions in the sublayer of the Sudbury Igneous Complex, Ontario. Chem Geol 165:37–46 doi: 10.1016/S0009-2541(99)00162-X DePaolo DJ (1981) Trace element and isotopic effects of the combined wallrock assimilation and fractional crystallization. Earth Planet Sci Lett 53:189–202 doi: 10.1016/0012-821X(81)90153-9 Du AD, Wu SQ, Sun DZ, Wang SX, Qu WJ, Markey R, Stein H, Morgan J, Malinovskiy D (2004) Preparation and certification of Re–Os dating reference materials: molybdenite HLP and JDC. Geostand Geoanal Res 28:41–52 doi: 10.1111/j.1751-908X.2004.tb01042.x Ebel DS, Naldrett AJ (1996) Fractional crystallization of sulfide ore liquid at high temperature. Econ Geol 91:607–637 doi: 10.2113/gsecongeo.91.3.607 Foster JG, Lambert DD, Frick LR, Maas R (1996) Re–Os isotopic evidence for genesis of Archaean nickel ores from uncontaminated komatiites. Nature 382:703–706 doi: 10.1038/382703a0 Gannoun A, Burton KW, Thomas LE, Parkison IJ, Calsteren P, van Schiano P (2004) Osmium isotope heterogeneity in the constituent phases of mid-ocean ridge basalts. Science 303:70–72 doi: 10.1126/science.1090266 Han CM, Xiao WJ, Zhao GC, Qu WJ, Du AD (2007) Re–Os dating of the Kalatongke Cu–Ni sulfide deposit, Altay Shan, NW China, and resulting geodynamic implications. Ore Geol Rev 32:452–468 doi: 10.1016/j.oregeorev.2006.11.004 Kamo SL, Czamanske GK, Krogh TE (1996) A minimum U–Pb age for Siberian flood-basalt volcanism. Geochim Cosmochim Acta 60:3505–3511 doi: 10.1016/0016-7037(96)00173-1 Keays RR, Lightfoot PC (2010) Crustal sulfur is required to form magmatic Ni–Cu sulfide deposits: evidence from chalcophile element signatures of Siberian and Deccan Traps basalts. Miner Deposita 45:241–257 doi: 10.1007/s00126-009-0271-1 Lesher CM, Burnham OM (2001) Multicomponent elemental and isotopic mixing in Ni–Cu–(PGE) ores at Kambalda, Western Australia. Can Mineral 39:421–446 doi: 10.2113/gscanmin.39.2.421 Mao JW, Pirajno F, Zhang ZH, Chai FM, Wu H, Chen SP, Cheng SL, Yang JM, Zhang CQ (2008) Cu–Ni sulphide deposits in the Chinese Tianshan and Altay orogens (Xinjiang Autonomous Region): principal characteristics and ore-forming processes. J Asian Earth Sci 32:184–203 doi: 10.1016/j.jseaes.2007.10.006 Pirajno F, Mao JW, Zhang ZC, Zhang ZH, Chai FM (2008) The association of mafic-ultramafic intrusions and A-type magmatism in the Tian Shan and Altay orogens, NW China: implications for geodynamic evolution and potential for the discovery of new ore deposits. J Asian Earth Sci 32:165–183 doi: 10.1016/j.jseaes.2007.10.012 Ripley EM, Park YR, Li C, Naldrett AJ (1999) Sulfur and oxygen isotopic evidence of country rock contamination in the Voisey’s Bay Ni–Cu–Co deposit, Labrador, Canada. Lithos 47:53–68 doi: 10.1016/S0024-4937(99)00007-9 Ripley EM, Park YR, Lambert DD, Frick LR (2001) Re–Os isotopic variations in carbonaceous pelites hosting the Duluth Complex: implications for metamorphic and metasomatic process associated with mafic magma chambers. Geochim Cosmochim Acta 65:2965–2978 doi: 10.1016/S0016-7037(01)00635-4 Sengör AMC, Natal’in BA, Burtman US (1993) Evolution of the Altaid Tectonic Collage and Paleozoic Crustal growth in Eurasia. Nature 364:209–304 doi: 10.1038/364299a0 Shirey SB, Walker RJ (1998) The Re–Os isotope system in cosmochemistry and high-temperature geochemistry. Annual Rev Earth Planet Sci 26:423–500 doi: 10.1146/annurev.earth.26.1.423 Song XY, Li XR (2009) Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment. Miner Deposita 44:303–327 doi: 10.1007/s00126-008-0219-x Walker RJ, Morgan JW, Naldrett AJ, Li C, Fassett JD (1991) Re–Os isotope systematics of Ni–Cu sulfide ores, Sudbury Igneous Complex, Ontario: evidence for a major crustal component. Earth Planet Sci Lett 105:416–429 doi: 10.1016/0012-821X(91)90182-H Walker RJ, Morgan JW, Horan MF, Czamanske GK, Krogstad EJ, Fedorenko VA, Kunilov VE (1994) Re–Os isotopic evidence for an enriched-mantle source for the Noril’sk-type, ore-bearing intrusions, Siberia. Geochim Cosmochim Acta 58:4179–4197 doi: 10.1016/0016-7037(94)90272-0 Walker RJ, Storey M, Kerr AC, Tarney J, Arndt NT (1999) Implications of 187Os isotopic heterogeneities in a mantle plume: evidence from Gorgona Island and Curacao. Geochim Cosmochim Acta 63:713–728 doi: 10.1016/S0016-7037(99)00041-1 Watson EB (1982) Basalt contamination by continental crust: some experiments and models. Contrib Mineral Petrol 80:73–87 doi: 10.1007/BF00376736 Windley BF, Kroner A, Guo J, Qu G, Li Y, Zhang C (2002) Neoproterozoic to Paleozoic geology of the Altai Orogen, NW China: new zircon age data and tectonic evolution. J Geol 110:719–737 doi: 10.1086/342866 Yang G, Du AD, Lu JR, Qu WJ, Chen JF (2005) Re–Os (ICP-MS) dating of the massive sulfide ores from the Jinchuan Ni–Cu–PGE deposit. Sci China Ser D Earth Sci 48:1672–1677 doi: 10.1360/02YD0124 Yang SH, Qu WJ, Tian L, Chen JF, Du AD, Yang G (2008) Origin of the inconsistent apparent Re–Os age of the Jinchuan Ni–Cu sulfide ore deposit, China: post-segregation diffusion of Os. Chem Geol 247:401–418 doi: 10.1016/j.chemgeo.2007.11.002 Zhang ZH, Mao JW, Du AD, Pirajno F, Wang ZL, Chai FM, Zhang ZC, Yang JM (2008) Re–Os dating of two Cu-Ni sulfide deposits in northern Xinjiang, NW China and its geological significance. J Asian Earth Sci 32:204–217 doi: 10.1016/j.jseaes.2007.10.005 Zhou MF, Lesher CM, Yang Z, Li J, Sun M (2004) Geochemistry and petrogenesis of 270 Ma Ni–Cu–(PGE) sulfide-bearing mafic intrusions in the Huangshan district, Eastern Xinjiang, Northwest China: implications for the tectonic evolution of the Central Asian orogenic Belt. Chem Geol 209:233–257 doi: 10.1016/j.chemgeo.2004.05.005 Zhou MF, Zhao JH, Jiang CY, Gao JF, Wang W, Yang SH (2009) OIB-like, heterogeneous mantle sources of Permian basaltic magmatism in the western Tarim Basin, NW China: implications for a possible Permian large igneous province. Lithos 113:583–594 doi: 10.1016/j.lithos.2009.06.027 |
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Gao, JF | en_HK |
| dc.contributor.author | Zhou, MF | en_HK |
| dc.contributor.author | Lightfoot, PC | en_HK |
| dc.contributor.author | Qu, W | en_HK |
| dc.date.accessioned | 2012-05-28T08:17:48Z | - |
| dc.date.available | 2012-05-28T08:17:48Z | - |
| dc.date.issued | 2012 | en_HK |
| dc.identifier.citation | Mineralium Deposita, 2012, v. 47 n. 7, p. 731-738 | en_HK |
| dc.identifier.issn | 0026-4598 | en_HK |
| dc.identifier.uri | http://hdl.handle.net/10722/147111 | - |
| dc.description.abstract | Re-Os isotope compositions of mantle-derived magmas are highly sensitive to crustal contamination because the crust and mantle have very different Os isotope compositions. Crustal contamination may trigger S saturation and thus the formation of magmatic Ni-Cu-(PGE) sulfide deposits. The ∼287-Ma Kalatongke norite intrusion of NW China are hosted in carboniferous tuffaceous rocks and contain both disseminated and massive sulfide mineralization. The Re-Os isotope compositions in the intrusion are highly variable. Norite and massive sulfide ores have γ Os values ranging from +59 to +160 and a Re-Os isochron age of 239 ± 51 Ma, whereas disseminated sulfide ores have γ Os values from +117 to +198 and a Re-Os isochron age of 349 ± 34 Ma. The variability of Os isotope compositions can be explained as the emplacement of two distinct magma pulses. Massive sulfide ores and barren norite in the intrusion formed from the same magma pulse, whereas the disseminated sulfide ores with more radiogenic Os isotopes formed from another magma pulse which underwent different degrees of crustal contamination. Re-Os isotopes may not be suitable for dating sulfide-bearing intrusions that underwent variable degrees of crustal contamination to form magmatic sulfide deposits. © 2012 The Author(s). | en_HK |
| dc.language | eng | en_US |
| dc.publisher | Springer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00126/index.htm | en_HK |
| dc.relation.ispartof | Mineralium Deposita | en_HK |
| dc.rights | The Author(s) | en_US |
| dc.rights | This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License. | en_US |
| dc.subject | Crustal contamination | en_HK |
| dc.subject | Re-Os isotopes | en_HK |
| dc.subject | Sulfide segregation | en_HK |
| dc.subject | Sulfide-bearing intrusions | en_HK |
| dc.subject | Sulfides | en_HK |
| dc.title | Heterogeneous Os isotope compositions in the Kalatongke sulfide deposit, NW China: the role of crustal contamination | en_HK |
| dc.type | Article | en_HK |
| dc.identifier.openurl | http://www.springerlink.com/link-out/?id=2104&code=9X152K74TH663603&MUD=MP | en_US |
| dc.identifier.email | Zhou, MF:mfzhou@hkucc.hku.hk | en_HK |
| dc.identifier.authority | Zhou, MF=rp00844 | en_HK |
| dc.description.nature | published_or_final_version | en_US |
| dc.identifier.doi | 10.1007/s00126-012-0414-7 | en_HK |
| dc.identifier.scopus | eid_2-s2.0-84866906191 | en_HK |
| dc.relation.references | Amelin Y, Li CS, Naldrett AJ (1999) Geochronology of the Voisey’s Bay intrusion, Labrador, Canada, by precise U–Pb dating of coexisting baddeleyite, zircon, and apatite. Lithos 47:33–51 | en_US |
| dc.relation.references | doi: 10.1016/S0024-4937(99)00006-7 | en_US |
| dc.relation.references | Brenan JM (2002) Re–Os fractionation in magmatic sulfide melt by monosulfide solid solution. Earth Planet Sci Lett 199:257–268 | en_US |
| dc.relation.references | doi: 10.1016/S0012-821X(02)00581-2 | en_US |
| dc.relation.references | Brenan JM (2008) Re–Os fractionation by sulfide melt–silicate melt partitioning: a new spin. Chem Geol 248:140–165 | en_US |
| dc.relation.references | doi: 10.1016/j.chemgeo.2007.09.003 | en_US |
| dc.relation.references | Brenan JM, Cherniak DJ, Rose LA (2000) Diffusion of osmium in pyrrhotite and pyrite: implications for closure of the Re–Os isotopic system. Earth Planet Sci Lett 180:399–413 | en_US |
| dc.relation.references | doi: 10.1016/S0012-821X(00)00165-5 | en_US |
| dc.relation.references | Campbell IH, Naldrett AJ (1979) The influence of silicate:sulfide ratios on the geochemistry of magmatic sulfides. Econ Geol 74:1503–1506 | en_US |
| dc.relation.references | doi: 10.2113/gsecongeo.74.6.1503 | en_US |
| dc.relation.references | Campbell IH, Czamanske GK, Fedorenko VA, Hill RI, Stepanov V, Kunilov VE (1992) Synchronism of the Siberian traps and the Permian–Triassic boundary. Science 258:1760–1763 | en_US |
| dc.relation.references | doi: 10.1126/science.258.5089.1760 | en_US |
| dc.relation.references | Cohen AS, Burnham OM, Hawkesworth CJ, Lightfoot PC (2000) Pre-emplacement Re–Os ages from ultramafic inclusions in the sublayer of the Sudbury Igneous Complex, Ontario. Chem Geol 165:37–46 | en_US |
| dc.relation.references | doi: 10.1016/S0009-2541(99)00162-X | en_US |
| dc.relation.references | DePaolo DJ (1981) Trace element and isotopic effects of the combined wallrock assimilation and fractional crystallization. Earth Planet Sci Lett 53:189–202 | en_US |
| dc.relation.references | doi: 10.1016/0012-821X(81)90153-9 | en_US |
| dc.relation.references | Du AD, Wu SQ, Sun DZ, Wang SX, Qu WJ, Markey R, Stein H, Morgan J, Malinovskiy D (2004) Preparation and certification of Re–Os dating reference materials: molybdenite HLP and JDC. Geostand Geoanal Res 28:41–52 | en_US |
| dc.relation.references | doi: 10.1111/j.1751-908X.2004.tb01042.x | en_US |
| dc.relation.references | Ebel DS, Naldrett AJ (1996) Fractional crystallization of sulfide ore liquid at high temperature. Econ Geol 91:607–637 | en_US |
| dc.relation.references | doi: 10.2113/gsecongeo.91.3.607 | en_US |
| dc.relation.references | Foster JG, Lambert DD, Frick LR, Maas R (1996) Re–Os isotopic evidence for genesis of Archaean nickel ores from uncontaminated komatiites. Nature 382:703–706 | en_US |
| dc.relation.references | doi: 10.1038/382703a0 | en_US |
| dc.relation.references | Gannoun A, Burton KW, Thomas LE, Parkison IJ, Calsteren P, van Schiano P (2004) Osmium isotope heterogeneity in the constituent phases of mid-ocean ridge basalts. Science 303:70–72 | en_US |
| dc.relation.references | doi: 10.1126/science.1090266 | en_US |
| dc.relation.references | Han CM, Xiao WJ, Zhao GC, Qu WJ, Du AD (2007) Re–Os dating of the Kalatongke Cu–Ni sulfide deposit, Altay Shan, NW China, and resulting geodynamic implications. Ore Geol Rev 32:452–468 | en_US |
| dc.relation.references | doi: 10.1016/j.oregeorev.2006.11.004 | en_US |
| dc.relation.references | Kamo SL, Czamanske GK, Krogh TE (1996) A minimum U–Pb age for Siberian flood-basalt volcanism. Geochim Cosmochim Acta 60:3505–3511 | en_US |
| dc.relation.references | doi: 10.1016/0016-7037(96)00173-1 | en_US |
| dc.relation.references | Keays RR, Lightfoot PC (2010) Crustal sulfur is required to form magmatic Ni–Cu sulfide deposits: evidence from chalcophile element signatures of Siberian and Deccan Traps basalts. Miner Deposita 45:241–257 | en_US |
| dc.relation.references | doi: 10.1007/s00126-009-0271-1 | en_US |
| dc.relation.references | Lesher CM, Burnham OM (2001) Multicomponent elemental and isotopic mixing in Ni–Cu–(PGE) ores at Kambalda, Western Australia. Can Mineral 39:421–446 | en_US |
| dc.relation.references | doi: 10.2113/gscanmin.39.2.421 | en_US |
| dc.relation.references | Mao JW, Pirajno F, Zhang ZH, Chai FM, Wu H, Chen SP, Cheng SL, Yang JM, Zhang CQ (2008) Cu–Ni sulphide deposits in the Chinese Tianshan and Altay orogens (Xinjiang Autonomous Region): principal characteristics and ore-forming processes. J Asian Earth Sci 32:184–203 | en_US |
| dc.relation.references | doi: 10.1016/j.jseaes.2007.10.006 | en_US |
| dc.relation.references | Pirajno F, Mao JW, Zhang ZC, Zhang ZH, Chai FM (2008) The association of mafic-ultramafic intrusions and A-type magmatism in the Tian Shan and Altay orogens, NW China: implications for geodynamic evolution and potential for the discovery of new ore deposits. J Asian Earth Sci 32:165–183 | en_US |
| dc.relation.references | doi: 10.1016/j.jseaes.2007.10.012 | en_US |
| dc.relation.references | Ripley EM, Park YR, Li C, Naldrett AJ (1999) Sulfur and oxygen isotopic evidence of country rock contamination in the Voisey’s Bay Ni–Cu–Co deposit, Labrador, Canada. Lithos 47:53–68 | en_US |
| dc.relation.references | doi: 10.1016/S0024-4937(99)00007-9 | en_US |
| dc.relation.references | Ripley EM, Park YR, Lambert DD, Frick LR (2001) Re–Os isotopic variations in carbonaceous pelites hosting the Duluth Complex: implications for metamorphic and metasomatic process associated with mafic magma chambers. Geochim Cosmochim Acta 65:2965–2978 | en_US |
| dc.relation.references | doi: 10.1016/S0016-7037(01)00635-4 | en_US |
| dc.relation.references | Sengör AMC, Natal’in BA, Burtman US (1993) Evolution of the Altaid Tectonic Collage and Paleozoic Crustal growth in Eurasia. Nature 364:209–304 | en_US |
| dc.relation.references | doi: 10.1038/364299a0 | en_US |
| dc.relation.references | Shirey SB, Walker RJ (1998) The Re–Os isotope system in cosmochemistry and high-temperature geochemistry. Annual Rev Earth Planet Sci 26:423–500 | en_US |
| dc.relation.references | doi: 10.1146/annurev.earth.26.1.423 | en_US |
| dc.relation.references | Song XY, Li XR (2009) Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment. Miner Deposita 44:303–327 | en_US |
| dc.relation.references | doi: 10.1007/s00126-008-0219-x | en_US |
| dc.relation.references | Walker RJ, Morgan JW, Naldrett AJ, Li C, Fassett JD (1991) Re–Os isotope systematics of Ni–Cu sulfide ores, Sudbury Igneous Complex, Ontario: evidence for a major crustal component. Earth Planet Sci Lett 105:416–429 | en_US |
| dc.relation.references | doi: 10.1016/0012-821X(91)90182-H | en_US |
| dc.relation.references | Walker RJ, Morgan JW, Horan MF, Czamanske GK, Krogstad EJ, Fedorenko VA, Kunilov VE (1994) Re–Os isotopic evidence for an enriched-mantle source for the Noril’sk-type, ore-bearing intrusions, Siberia. Geochim Cosmochim Acta 58:4179–4197 | en_US |
| dc.relation.references | doi: 10.1016/0016-7037(94)90272-0 | en_US |
| dc.relation.references | Walker RJ, Storey M, Kerr AC, Tarney J, Arndt NT (1999) Implications of 187Os isotopic heterogeneities in a mantle plume: evidence from Gorgona Island and Curacao. Geochim Cosmochim Acta 63:713–728 | en_US |
| dc.relation.references | doi: 10.1016/S0016-7037(99)00041-1 | en_US |
| dc.relation.references | Watson EB (1982) Basalt contamination by continental crust: some experiments and models. Contrib Mineral Petrol 80:73–87 | en_US |
| dc.relation.references | doi: 10.1007/BF00376736 | en_US |
| dc.relation.references | Windley BF, Kroner A, Guo J, Qu G, Li Y, Zhang C (2002) Neoproterozoic to Paleozoic geology of the Altai Orogen, NW China: new zircon age data and tectonic evolution. J Geol 110:719–737 | en_US |
| dc.relation.references | doi: 10.1086/342866 | en_US |
| dc.relation.references | Yang G, Du AD, Lu JR, Qu WJ, Chen JF (2005) Re–Os (ICP-MS) dating of the massive sulfide ores from the Jinchuan Ni–Cu–PGE deposit. Sci China Ser D Earth Sci 48:1672–1677 | en_US |
| dc.relation.references | doi: 10.1360/02YD0124 | en_US |
| dc.relation.references | Yang SH, Qu WJ, Tian L, Chen JF, Du AD, Yang G (2008) Origin of the inconsistent apparent Re–Os age of the Jinchuan Ni–Cu sulfide ore deposit, China: post-segregation diffusion of Os. Chem Geol 247:401–418 | en_US |
| dc.relation.references | doi: 10.1016/j.chemgeo.2007.11.002 | en_US |
| dc.relation.references | Zhang ZH, Mao JW, Du AD, Pirajno F, Wang ZL, Chai FM, Zhang ZC, Yang JM (2008) Re–Os dating of two Cu-Ni sulfide deposits in northern Xinjiang, NW China and its geological significance. J Asian Earth Sci 32:204–217 | en_US |
| dc.relation.references | doi: 10.1016/j.jseaes.2007.10.005 | en_US |
| dc.relation.references | Zhou MF, Lesher CM, Yang Z, Li J, Sun M (2004) Geochemistry and petrogenesis of 270 Ma Ni–Cu–(PGE) sulfide-bearing mafic intrusions in the Huangshan district, Eastern Xinjiang, Northwest China: implications for the tectonic evolution of the Central Asian orogenic Belt. Chem Geol 209:233–257 | en_US |
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| dc.identifier.spage | 1 | en_HK |
| dc.identifier.epage | 8 | en_HK |
| dc.identifier.eissn | 1432-1866 | en_US |
| dc.identifier.isi | WOS:000309232200002 | - |
| dc.publisher.place | Germany | en_HK |
| dc.description.other | Springer Open Choice, 28 May 2012 | en_US |
| dc.identifier.scopusauthorid | Gao, JF=25638167000 | en_HK |
| dc.identifier.scopusauthorid | Zhou, MF=7403506005 | en_HK |
| dc.identifier.scopusauthorid | Lightfoot, PC=7102963749 | en_HK |
| dc.identifier.scopusauthorid | Qu, W=8982620500 | en_HK |
| dc.identifier.citeulike | 10629755 | - |
| dc.identifier.issnl | 0026-4598 | - |