小兴安岭霍吉河钼矿区含矿花岗岩类特征及成矿年龄

张琳琳, 刘翠, 周肃, 孙凯, 邱瑞照, 冯瑶. 小兴安岭霍吉河钼矿区含矿花岗岩类特征及成矿年龄[J]. 岩石学报, 2014, 30(11): 3419-3431.
引用本文: 张琳琳, 刘翠, 周肃, 孙凯, 邱瑞照, 冯瑶. 小兴安岭霍吉河钼矿区含矿花岗岩类特征及成矿年龄[J]. 岩石学报, 2014, 30(11): 3419-3431.
ZHANG LinLin, LIU Cui, ZHOU Su, SUN Kai, QIU RuiZhao, FENG Yao. Characteristics of ore-bearing granites and ore-forming age of the Huojihe molybdenum deposit in Lesser Xing'an Range[J]. Acta Petrologica Sinica, 2014, 30(11): 3419-3431.
Citation: ZHANG LinLin, LIU Cui, ZHOU Su, SUN Kai, QIU RuiZhao, FENG Yao. Characteristics of ore-bearing granites and ore-forming age of the Huojihe molybdenum deposit in Lesser Xing'an Range[J]. Acta Petrologica Sinica, 2014, 30(11): 3419-3431.

小兴安岭霍吉河钼矿区含矿花岗岩类特征及成矿年龄

  • 基金项目:

    本文受中国地质调查局项目(1212011121075、1212010911028、1212010711814、12120114020901、1212011220921、1212011121266)、科技部国际合作专项(2011DFA22460、2010DFB23390)和国家重点基础研究发展计划项目(2011CB808901)联合资助.

详细信息

Characteristics of ore-bearing granites and ore-forming age of the Huojihe molybdenum deposit in Lesser Xing'an Range

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  • 黑龙江霍吉河钼矿区内含矿花岗岩类岩石组合为黑云母二长花岗岩、二长花岗岩和花岗细晶岩,属高钾钙碱性岩-钾玄岩系列准铝质-过铝质岩石,具有轻稀土富集、重稀土亏损分馏模式;富集不相容元素(Cs、Th)并表现为Ta和Nb负异常以及Pb、Sr正异常,显示俯冲带地球化学特征.含矿岩浆岩明显富集Mo、Cu、Pb、Zn、W、Cr等金属元素.岩石全岩铅同位素来源比较复杂,具有混合成因铅特征.辉钼矿Re-Os模式年龄为180.7±2.5Ma和181.3±2.6Ma,钼矿成矿时代为早侏罗世.霍吉河钼矿是在蒙古-鄂霍茨克洋和古太平洋相向联合俯冲作用下,导致霍吉河地区发生地壳增生和壳幔相互作用以及后来的拆沉作用,形成了该区花岗质岩石和钼矿床.高度演化的花岗岩体(脉)可以作为今后本区钼矿床的找矿方向.
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出版历程
收稿日期:  2014-02-10
修回日期:  2014-06-10
刊出日期:  2014-11-30

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