| 苏欣栋.鄂东南成矿区壳幔结构及其特征[J].地质与勘探,1995,(1):18-25 |
| 鄂东南成矿区壳幔结构及其特征 |
| Crust-Mantle Structure and Characteristics of Southeast Hubei Metallogenic Province |
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| DOI： |
| 中文关键词: 鄂东南 成矿区 壳幔结构 |
| 英文关键词: Sotheast Guangdong,crust-mantle,characteristics,model |
| 基金项目: |
| 苏欣栋 |
| 中南冶金地质研究 |
| 摘要点击次数: 2239 |
| 全文下载次数: 1370 |
| 中文摘要: |
| 鄂东南成矿区壳幔具有典型的层状结构，各层具有鲜明的地质、地球地球化学特征。硅镁层为地球形成时的原始地壳，硅铝层和上构造层为地球形成后膨涨增生而成。建立了壳、幔结构综合理想模式。 |
| 英文摘要: |
| Crust-Mantle of Southeast Hubei Metallogenic Province possesses a typical layered structure.Each layer is characertistic of itsgeolgy,geophysics and geochemisty. Si-Mg layer is the original crust which was formed during thde earth formation,Si-Al lay-er and upper tectonic layer was formed after the earth formation.The ideal synthetic model of crustmantle has been outlined. |
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