| 引用本文： |
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李晓峰,梁金城,冯佐海.广西海洋山花岗体侵岩位机制[J].广西科学,1997,4(3):188-191. [点击复制]
- Li Xiaofeng,Liang Jincheng,Feng Zuohai.The Emplacement Mechanism of Haiyangshan Granite Plutons[J].Guangxi Sciences,1997,4(3):188-191. [点击复制]
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| 摘要: |
| 海洋山花岗岩体位于华南加里东花岗岩带内。岩体中岩石具有较低的应变结构;奥陶系围岩受到的变形变质作用较低,但作用时间较长。各种构造型式表明:该岩体的侵位机制是以同构造穹窿为主,并兼具有某些气球膨胀特征。 |
| 关键词: 花岗岩 侵位机制 海洋山/广西 |
| DOI： |
| 投稿时间：1997-02-18 |
| 基金项目: |
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| The Emplacement Mechanism of Haiyangshan Granite Plutons |
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Li Xiaofeng, Liang Jincheng, Feng Zuohai
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| (Guilin Institute of Technology, 12 Jianganlu, Guilin, Guangxi, 541000) |
| Abstract: |
| The Haiyangshan granite plutons is in the Caledonian granitonian belt.The rock has lower strain fabric and it's wall rock has lower deformation and metamorphism.All tectonic traces indicate that Haiyangshan granite plutons was an active emplacement mechanism dominating by simultaneous tectonic dome and shared with balloon expension. |
| Key words: granite emplacement mechanism Haiyangshan/Guangxi |
