李永飞, 郜晓勇, 卞雄飞, 陈树旺, 丁秋红. 大兴安岭北段龙江盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J]. 地质通报, 2013, 32(8): 1195-1211.
    引用本文: 李永飞, 郜晓勇, 卞雄飞, 陈树旺, 丁秋红. 大兴安岭北段龙江盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J]. 地质通报, 2013, 32(8): 1195-1211.
    LI Yong-fei, GAO Xiao-yong, BIAN Xiong-fei, CHEN Shu-wang, DING Qiu-hong. LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Mesozoic volcanic rocks from Longjiang basin in northern Da Hinggan Mountains and their geological implications[J]. Geological Bulletin of China, 2013, 32(8): 1195-1211.
    Citation: LI Yong-fei, GAO Xiao-yong, BIAN Xiong-fei, CHEN Shu-wang, DING Qiu-hong. LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Mesozoic volcanic rocks from Longjiang basin in northern Da Hinggan Mountains and their geological implications[J]. Geological Bulletin of China, 2013, 32(8): 1195-1211.

    大兴安岭北段龙江盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义

    LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Mesozoic volcanic rocks from Longjiang basin in northern Da Hinggan Mountains and their geological implications

    • 摘要: 大兴安岭北段龙江盆地中生代火山岩主要为一套中酸性岩石,岩石化学成分显示其主要为英安岩与流纹岩,少量安山岩。各类岩石的LA-ICP-MS锆石U-Pb定年结果显示,其形成于122.2~126.5Ma之间的早白垩世。火山岩为高钾钙碱性系列岩石,稀土元素总量较高(ΣREE=103.22×10-6~249.29×10-6),轻重稀土元素分馏明显((La/Yb)N=6.29~25.89),负Eu异常(Eu/Eu?鄢=0.48~0.84)。富集大离子亲石元素Rb、Ba、Th、U、K和LREE,亏损高场强元素Nb、Ta、P、Ti;火山岩稀土元素与微量元素标准化配分曲线与地壳配分曲线近乎一致,为一套壳源岩浆系列火山岩;大部分岩石300 

      Abstract: The Longjiang Formation in northern Da Hinggan Mountains is composed mainly of dacite and rhyolite with minor andesite. the LA-ICP-MS zircon U-Pb dating of these rocks yielded ages of 122.2~126.5Ma, corresponding to Early Cretaceous. These volcanic rocks are of high potassium calc-alkaline series possessing such geochemical characteristics as high ΣREE, remarkable (La/Yb)N values and negative Eu anomalies. In the spidergram, the rocks show pronounced enrichment of Rb, Ba, Th, U, K and depletion of Nb, Ta, P, Ti, much identical with the characteristics of the upper crust. Most of these rocks have typical adakitic characteristics, as shown by the data 300 

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