| 造山带火山岩浆作用 |
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| 引用本文： | 夏林圻.造山带火山岩浆作用[J].西北地质,2001,34(3):18-28. |
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| 作者姓名： | 夏林圻 |
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| 作者单位： | 西安地质矿产研究所, |
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| 摘 要： | 造山带火山岩石学研究的主要目的在于重溯造山带的构造－岩浆演化历史。纵观我国到至全球的大陆造山带形成－演化历史，一个造山带往往经历了古大陆裂解，洋陆转换，陆块拼合，碰撞，陆内伸展－盆山耦合和新构造隆升（陆内造山）等众多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆民之相伴。因此，我们可以根据造山带形成－演化不同阶段火山岩浆作用的特点来重溯造山带的的构造－岩浆演化历史，并进而从更大尺度上加以对比，探索全球动力学乃至比较行星学等重大学问题。本文对造山带火山岩石学研究中的一些重要问题进行了讨论和评述，这些问题包括有：板块内部火册浆活动，离散板块边界上的火山岩浆活动，会聚板块边缘的火山岩浆活动。
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| 关 键 词： | 造山带 火山岩 岩浆作用 板块构造 古大陆裂解 全球动力学 |
| 文章编号： | 1009-6248(2001)03-0018-11 |
| 修稿时间： | 2001年7月12日 |
Volcano-magmatism of orogenic belts |
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| XIA Lin-qi.Volcano-magmatism of orogenic belts[J].Northwestern Geology,2001,34(3):18-28. |
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| Authors: | XIA Lin-qi |
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| Abstract: | The main aim of study on volcanic rocks of orogenic belts is to retrace the history of tectono magmatic evolution of orogenic belts Scanning the formation evolutionary histories of continental orogenic belts in both our country and whole workd,an orogenic belt has often undergone numerous and various tectono evolutionary stages,such as palaeo continental break up,ocean land transition,continental matching collision,intracontinental extension basin range coupling,new tectonic uplift(intracontinental orogeny),etc ,which are respectively companied with characteristic volcano magmatism We might retrace the history of tectono magmatic evolution of volcanic magmatism at different stages of formation evolution of orogenic belts and further explore some important scientific problems of global dynamics and comparative planetary dynamics by means of comparison in larger scales Some important problems on the studies of volcanic rocks of orogenic belts,which include the volcanic magmatism within plate,volcanic magmatism at constructive plate margins and volcanic magmatism at destructive plate margins,are discussed and reviewed in this paper |
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| Keywords: | orogenic belt volcanic rock magmatism plate tectonics review |
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