| 甘肃北山小西弓金矿区石英正长斑岩LA-ICP-MS锆石U-Pb年龄和地球化学特征 |
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| 引用本文： | 朱 江,吕新彪,彭三国,龚银杰,邱啸飞,肖广玲.甘肃北山小西弓金矿区石英正长斑岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J].地质通报,2015,34(8):1460-1469. |
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| 作者姓名： | 朱 江 吕新彪 彭三国 龚银杰 邱啸飞 肖广玲 |
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| 作者单位： | 1.中国地质调查局武汉地质调查中心，湖北 武汉 430205； 2.中国地质调查局花岗岩成岩成矿地质研究中心，湖北 武汉 430205；3.中国地质大学（武汉）资源学院，湖北 武汉 430074；4.山东地质矿产勘查开发局，山东 济南 250014 |
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| 基金项目： | 国家305项目（编号：2011BAB06B04-05）和中国地质调查局项目（编号：1212011220515） |
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| 摘 要： | 通过高精度的LA-ICP-MS锆石U-Pb测年,获得北山南带小西弓金矿区石英正长斑岩的形成年龄为247.5±2.2Ma,属中三叠世。地球化学分析表明,该岩体为准铝质、钾玄岩系列,主量元素高硅(Si O_2=65.8%~66.2%)、富碱(Na_2O+K_2O=8.99%~9.41%)、低钙(Ca O=1.72%~2.19%)、贫镁(Mg O=0.63%~0.70%);轻稀土元素富集,重稀土元素亏损,弱负Eu异常。大离子亲石元素Rb、Th、U、K和Pb富集,同时Ba、Sr、P、Ti和Eu亏损,并具高104*Ga/Al值和高Zr+Nb+Ce+Y含量,表现出A型花岗岩的特征。北山南带三叠纪岩浆活动强烈,高分异I型-A型花岗岩大量发育,暗示区域内三叠纪处于造山后伸展环境。
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| 关 键 词： | LA-ICP-MS锆石U-Pb年龄 地球化学特征 A型花岗岩 石英正长斑岩 北山 |
LA-ICP-MS zircon U-Pb geochronology and geochemical characteristics of the quartz syenite porphyry in the Xiaoxigong gold deposit and their geological implications |
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| Institution: | 1. Wuhan Center of Geological Survey, CGS, Wuhan 430205, Hubei, China;2. Research Center of Granitic Diagenesis and Mineralization, CGS, Wuhan 430205, Hubei, China;3. Faculty of Resources, China University of Geosciences, Wuhan 430074, Hubei, China;4. Shandong Bureau of Geology and Mineral Resources, Jinan 250014, Shandong, China |
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| Abstract: | The Xiaoxigong quartz syenite porphyry is located in the south of the Beishan orogenic belt, Northwest China. LA-ICP-MS zircon U-Pb dating yielded a weighted mean 206Pb/238U age of 247.5±2.2Ma for the quartz syenite porphyry, implying middle Triassic intrusion. Geochemical analyses show that the porphyry is enriched in Si, K, Na, and REE, and depleted in Mg and Ca, with SiO2 being 65.8%-66.2%, Na2O+K2O 8.99%-9.41%, CaO 1.72%-2.19%, and MgO 0.63%-0.70%. REE are characterized by negative Eu anomalies. The porphyry is enriched in Rb, Th, U, K, Pb, Nb, Zr and Hf and depleted in Ba, Sr, P, Ti and Eu. The quartz syenite porphyry has high Zr+Nb+Ce+Y abundances and 104?Ga/Al ratios. Petrologic and major and trace elements data all indicate that the Xiaoxigong quartz syenite porphyry is a typical A-type granite. The magma probably originated from partial melting of the crust due to underplating mantle-derived magmas and was emplaced in a post-orogenic extensional tectonic setting. |
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| Keywords: | LA-ICP-MS zircon U-Pb ages geochemical characteristics A-type granite quartz syenite porphyry Beishan region |
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