首页> 外文期刊>International Geology Review >Geochronology, geochemistry, and Nd-Hf isotopes of early Palaeozoic-early Mesozoic I-type granites from the Hufang composite pluton, Fujian, South China: crust-mantle interactions and tectonic implications
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Geochronology, geochemistry, and Nd-Hf isotopes of early Palaeozoic-early Mesozoic I-type granites from the Hufang composite pluton, Fujian, South China: crust-mantle interactions and tectonic implications

机译:中国南方福建呼房复合岩体中的早古生代-中生代I型花岗岩的年代学,地球化学和Nd-Hf同位素:地壳-地幔相互作用及其构造意义

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The Hufang composite pluton of the Qingliu-Mingxi area of western Fujian is located in the eastern part of the South China Block (SCB). The pluton consists of three granitic intrusions: the Weipu (WP) alkali-feldspar-granite, the Shaxi (SX) biotite-granite, and the Qinxi (QX) alkali-feldspar-granite. Zircon U-Pb ages obtained for the three intrusions are 434 ± 3, 409 ± 3, and 224 ± 2 Ma, respectively, indicating that the Hufang composite pluton is made up of intrusions of both the Caledonian and Indosinian ages. All three intrusive bodies are weakly peraluminous to metaluminous and fall in the high-K calc-alkaline and shoshonite series. They are enriched in large ion lithophile elements (LILEs) and light rare earth elements (LREEs) and display moderate negative Eu anomalies and roughly flat patterns of heavy rare earth elements (HREEs). Integrated geological and geochemical data suggest that all three granitic intrusions are I-type and were emplaced in post-collisional extensional settings. All of the analysed rocks show homogeneous Nd isotopic compositions, with ϵNd(t) values ranging from −0.25 to +1.32 for the Caledonian SX biotite-granite and from −1.01 to −0.82 for the Indosinian QX alkali-feldspar-granite. However, they display highly variable zircon Hf isotopic compositions, with ϵHf(t) values of −5.9 to +3.8 and −2.4 to +10.2 for the Caledonian WP and SX granites, respectively, and −12.2 to −5.0 for the Indosinian QX granite. These Nd-Hf isotopic characteristics are best explained by binary mixing between juvenile, mantle-derived magma and the evolved crustal components. We suggest that crust-mantle interactions played an important role in the SCB generation of the Caledonian and Indosinian granitoids.View full textDownload full textKeywordsI-type granites, Caledonian, Indosinian, crust-mantle interaction, post-collisional extension, South 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/10.1080/00206814.2010.496542
机译:闽西清流-明溪地区的虎房复合岩体位于华南区块(SCB)东部。岩体由三个花岗岩侵入体组成:威普(WP)碱长石-花岗岩,沙溪(SX)黑云母-花岗岩和秦溪(QX)碱-长石-花岗岩。三种侵入体获得的锆石U-Pb年龄分别为434±3、409±3和224±2 Ma,表明Hufang复合岩体由加里东和印度支那时期的侵入体组成。这三个侵入体均呈弱铝质至金属质,属于高K钙碱性和钠钾铁矾系列。它们富含大型离子亲石元素(LILE)和轻稀土元素(LREE),并显示出中等程度的负Eu异常和重稀土元素(HREE)的大致平坦模式。综合的地质和地球化学数据表明,所有三个花岗岩侵入体都是I型的,并且都位于碰撞后的伸展环境中。所有分析的岩石均显示出均匀的Nd同位素组成,对于Caledonian SX黑云母-花岗岩和âµ Nd (t)值范围从0.25到+1.32。 Indosinian QX碱长石-花岗岩的“ 1.01至0.82”。但是,它们显示出高度可变的锆石Hf同位素组成,其ϵ Hf (t)值分别为5.9到+3.8和2.4到+10.2。加里东期WP和SX花岗岩,印度支那QX花岗岩的“ 12.2至5.0”。这些Nd-Hf同位素特征最好通过地幔衍生的岩浆和演化的地壳组分之间的二元混合来解释。我们认为,地幔-地幔相互作用在古苏格兰和印度支那的花岗岩的SCB世代中起着重要作用。查看全文下载全文关键词I型花岗岩,古苏格兰,印度支那,地壳-地幔相互作用,碰撞后扩展,华南地区相关var addthis_config = {ui_cobrand:“ Taylor&Francis Online”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2010.496542

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