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首页> 外文期刊>International Geology Review >Origin of the Dexing Cu-bearing porphyries, SE China: elemental and Sr-Nd-Pb-Hf isotopic constraints
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Origin of the Dexing Cu-bearing porphyries, SE China: elemental and Sr-Nd-Pb-Hf isotopic constraints

机译:中国东南德兴含铜斑岩的起源:元素和Sr-Nd-Pb-Hf同位素约束

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The Dexing porphyry copper deposit, part of the circum-Pacific porphyry copper ore belt, is the largest porphyry copper deposit in China. We present new LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating, bulk-rock elemental and Sr-Nd-Pb isotopic as well as in situ zircon Hf isotopic geochemistry for these ore-bearing porphyries, in an attempt to better constrain their petrogenesis. LA-ICP-MS zircon U-Pb dating shows that the Dexing porphyries were emplaced in the early Middle Jurassic (171 Ma); molybdenite Re-Os dating indicates that the associated Cu-Mo mineralization was contemporaneous (171 Ma) with the igneous intrusion. The rocks are mainly high-K calc-alkaline and show adakitic affinities, including high Sr and low Y and Yb contents, high Sr/Y and La/Yb ratios, and high Mg# (higher than pure crustal melts). These porphyries have initial 87Sr/86Sr ratios of 0.7044−0.7047, ϵNd(T) values of -1.5 to +0.6, and ϵHf(T) (in situ zircon) values of +2.6 to +4.6. They show unusually radiogenic Pb isotopic compositions with initial 206Pb/204Pb ratios up to 18.41 and 207Pb/204Pb up to 15.61. These isotopic compositions are distinctly different from either Pacific MORB or Yangtze lower crust but are similar to the subducting sediments in the western Pacific trenches. Detailed elemental and isotopic data suggest that the Dexing porphyries were emplaced in a continental arc setting coupled with westward subduction of the palaeo-Pacific plate. Partial melting involved the subducted slab (mainly the overlying sediments), with generated melts interacting with the lithospheric mantle wedge, thereby forming the investigated high-K calc-alkaline porphyry magmas.View full textDownload full textKeywordshigh-K calc-alkaline porphyries, porphyry copper deposit, Sr-Nd-Hf-Pb isotopes, Dexing ore deposit, Southeast ChinaRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00206814.2010.548119
机译:德兴斑岩铜矿床是环太平洋斑岩铜矿带的一部分,是中国最大的斑岩铜矿床。我们针对这些含矿斑岩提出了新的LA-ICP-MS锆石U-Pb和辉钼矿Re-Os定年,块状岩石元素和Sr-Nd-Pb同位素以及原位锆石Hf同位素地球化学,以期更好地限制其成岩作用。 LA-ICP-MS锆石U-Pb测年表明,德兴斑岩位于早侏罗世中期(171 Ma)。辉钼矿的Re-Os年代表明,相关的Cu-Mo矿化与火成岩侵入同时发生(171 Ma)。这些岩石主要是高K钙碱性物质,并显示出亲和力,包括高Sr和低Y和Yb含量,高Sr / Y和La / Yb比以及高Mg#(高于纯地壳熔体)。这些斑岩的初始 87 Sr / 86 Sr比率为0.7044ˆ0.7047,Ïn(T)值为-1.5至+0.6和ϵsub Hf(T)(原位锆石)值从+2.6到+4.6。它们显示出异常的放射源Pb同位素组成,其初始 206 Pb / 204 Pb比率高达18.41和 207 Pb / 204 Pb高达15.61。这些同位素组成与太平洋MORB或扬子下地壳明显不同,但与西太平洋海沟中的俯冲沉积物相似。详细的元素和同位素数据表明,德兴斑岩位于大陆弧环境中,并伴有古太平洋板块向西俯冲。部分熔融涉及俯冲板块(主要是上覆的沉积物),生成的熔体与岩石圈地幔楔相互作用,从而形成了被研究的高K钙碱性斑岩岩浆。矿床,Sr-Nd-Hf-Pb同位素,德兴矿床,中国东南相关var addthis_config = {ui_cobrand:“泰勒和弗朗西斯在线”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg ,google,更多“,pubid:” ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2010.548119

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