宁芜北段某些次火山岩和蚀变岩中的稀土元素 |
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引用本文: | 汪建明,陈可睦,宁仁祖.宁芜北段某些次火山岩和蚀变岩中的稀土元素[J].岩石矿物学杂志,1985,4(2):97-103. |
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作者姓名: | 汪建明 陈可睦 宁仁祖 |
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作者单位: | 江苏省地质矿产局实验室
(汪建明,陈可睦),江苏省地质矿产局实验室(宁仁祖) |
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摘 要: | 宁芜北段铁、铜、金的矿化大都与区内广泛发育的次火山岩有关。前人曾做过大量工作。在此基础上,本文试图从次火山岩及其在蚀变过程中稀土元素的地球化学恃征方面进行分析,进一步了解它的成因、蚀变及其与矿化的关系,借以提供一些地质找矿的信息。
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The Rare Earth Elements in some Sub-Volcanic and Altered rocks in North Nanjing-Wuhu area |
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Abstract: | In North Nanjing-Wuhu area, the gabbrodiorite porphyrite, augite-trachy-
andesite porphyrite and the quartz-monzonite porphyry of Dawaqg Shan
volcanic cycle together with the hauyne-trachyte porphyry of Niangniang
Shan cycle are all the comagmatic products formed. at various stages of
magma event. All these rocks display light REE enriched patterns which plot
parallel to each other. As a consequence of evolution of magma, the HREE
are fractionated and concentrated in the minerals crystallized in the early
stage, while the LREE are remained in the residue and concentrated in the
latter formed rocks with increasing in negative Eu anomaly. It indicates that
the magmatic differentiation is dominated by the fractional crystallization of
the mafic minerals, while that of the plogioclase is quite mild in this area. In
accordance with the rock assemblages, the data of stable isotopes as well as
the features of the REE patterns, it may be suggested that this rock series
may have been derived from upper mantle with some portions of partially
melted oceanic cxust and contaminated by spore continental cxustal materials.
The REE are mobile during hydrothermal alteration. Although there is
no significant variation in their total concentration in the process of So-called
dark-colored alteration, they are migrated away in large amounts during the
light-colored alteration, enlarging the (La/Yb)N ratio and negative Eu
anomaly. |
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