安第斯埃达克岩 :三种成因模式(英文)

被引:81
作者
Robert W KAY
Suzanne Mahlburg KAY
机构
[1] Department of Geological Sciences
[2] Cornell University
[3] Cornell University Ithaca NY -
[4] USA
[5] Ithaca NY
关键词
埃达克岩; 成因模式; 安第斯;
D O I
暂无
中图分类号
P588.1 [岩浆岩(火成岩)];
学科分类号
摘要
在安第斯埃达克岩是常见的。由这种岩石的痕量元素特征揭示的高压组成矿物 ,表明其有三种可能的成因。这三种成因按相对重要性依次为 :安第斯地壳的构造加厚 ;弧前壳的俯冲 -侵蚀 ;年轻洋壳的俯冲。在过去 30 Ma,每种成因模式的埃达克岩在智利 -阿根廷安第斯地区均有喷发。它们的产状与智利 -阿根廷边缘快速变化的构造背景中特定构造条件和事件相吻合。埃达克岩在过去安第斯边缘的产状可望成为矿化的优异构造标志 ,也可用于指导找矿
引用
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页码:303 / 311
页数:9
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