褶皱带橄榄岩-榴辉岩杂岩和稳定地块含金刚石岩筒的成因特征

著录项

• 来源
  《地学前缘》 |2007年第2期|108-128|共21页
• 作者

  A.A. Marakushev; A.V. Bobrov; N.A. Paneyakh; V.K. Garanin; Lu Fengxiang; Sang Longkang; Chen Meihua;

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• 作者单位

  Department of Petrology, Geological Faculty, M.V. Lomonosov Moscow State University, Leninskie Gory, Moscow 119992, Russia;

  Institute of Experimental Mineralogy, Russian Academy of Sciences, Chernogolovka, Moscow 142432, Russia;

  Department of Petrology, Geological Faculty, M.V. Lomonosov Moscow State University, Leninskie Gory, Moscow 119992, Russia;

  Institute of Geology of Ore Deposits, Mineralogy, Petrography, and Geochemistry, Russian Academy of Sciences, Staromonetnyi per. 35, Moscow 119017, Russia;

  Department of Petrology, Geological Faculty, M.V. Lomonosov Moscow State University, Leninskie Gory, Moscow 119992, Russia;

  Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China;

  Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China;

  Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China;

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• 原文格式 PDF
• 正文语种 chi
• 中图分类 侵入岩、深成岩;
• 关键词

  褶皱带; 稳定地块; 金刚石远景; 层状侵入体; 金伯利岩筒; 原生岩浆;