中国东部燕山期埃达克岩的特征及其构造—成矿意义

张旗 王焰 等. 中国东部燕山期埃达克岩的特征及其构造—成矿意义[J]. 岩石学报, 2001, 17(2): 236-244.
引用本文: 张旗 王焰 等. 中国东部燕山期埃达克岩的特征及其构造—成矿意义[J]. 岩石学报, 2001, 17(2): 236-244.
ZHANG Qi,WANG Yan,QIAN Qing,YANG JinHui,WANG YuanLong,ZHAO TaiPing and GUO GuangJunInstitute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China.. The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China.[J]. Acta Petrologica Sinica, 2001, 17(2): 236-244.
Citation: ZHANG Qi,WANG Yan,QIAN Qing,YANG JinHui,WANG YuanLong,ZHAO TaiPing and GUO GuangJunInstitute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China.. The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China.[J]. Acta Petrologica Sinica, 2001, 17(2): 236-244.

中国东部燕山期埃达克岩的特征及其构造—成矿意义

  • 基金项目:

    国家973项目“大规模成矿作用与大型矿集区预测”(G1999043206-05)和中国科学院知识创新工程基金(KZCX 1-07)课题资助项目.

The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China.

  • 埃达克岩是一套中酸性的火成岩,以亏损HREE和无负铕异常为特征,表明其形成深度很大,源区有石榴石残留。中国东部燕山期有许多中酸性岩浆岩类似埃达克岩的地球化学特征,但其形成环境却与消减作用无关。因此,本文将埃达克岩分为O型和C型两类:O型埃达克岩富Na,其成因与板块的消减作用有关;C型埃达克岩富K(大部分仍然是钠质的,少数为钾质的),可能是玄武岩底侵到加厚的陆壳(>50km)底部导致的下地壳麻粒岩部分熔融的产物。C型运行达克岩对解释中国东部燕山期许多地质现象是有启发的。由于C型埃达克岩保存了下地壳的许多印记,因此,还可以利用C型埃达克岩来反演下地壳的组成,探讨与下地壳及壳-幔过程有关的成矿作用问题。
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出版历程
修回日期:  2000-12-26
刊出日期:  2001-05-31

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