| 北秦岭灰池子复式岩体的地质特征及其成因 |
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| 引用本文： | 李伍平 王涛. 北秦岭灰池子复式岩体的地质特征及其成因[J]. 矿物岩石, 1995, 15(3): 8-15 |
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| 作者姓名： | 李伍平 王涛 |
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| 作者单位： | 西安地质学院资源经济系 |
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| 摘 要： | 灰池子复式岩体是北秦岭加里东造山带规模最大的花岗岩体，其成因争论较大。本文在１：５万区调工作的基础上，通过岩石学、岩石化学和同位素等方面的讨论，认为该岩体属于岩浆成因，其源岩与秦岭群无关，而是来自于地壳中的幔壳混合物，属于Ｈ型花岗岩。
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| 关 键 词： | 北秦岭 复式岩体 H型花岗岩 花岗岩 地质特征 |
GEOLOGIC FEATURE AND ITS GENESIS OF HUICHIZI COMPLEX PLUTON IN THE NORTH QINLING |
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| LjWuping,Wang Tao. GEOLOGIC FEATURE AND ITS GENESIS OF HUICHIZI COMPLEX PLUTON IN THE NORTH QINLING[J]. Journal of Mineralogy and Petrology, 1995, 15(3): 8-15 |
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| Authors: | LjWuping Wang Tao |
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| Abstract: | Huichizi complex pluton is the largest scale granitoid pluton of the north Qiniing Caledo-nian orogenic zone,and its genisis is a controversy.Based on the work of 1:50 000 regional geo-logical surveying and the study of petrology,petrochemisty,geochemistry,and isotope analyses,the author consider that this complex pltiton takes the origin from the magma of the maxture ofthe crust'Sand the mantle's substances remainedinthe crust,and without relation to the rock ofQinling group.It belong to H-type(Hybrid)granitoid. |
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| Keywords: | the north Qinling Huichizi complex pluton H-type(Hybrid)granitoid |
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