造山带火山岩浆作用

夏林圻. 造山带火山岩浆作用[J]. 西北地质, 2001, 34(3): 18-28.
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.
XIA Lin-qi. Volcano-magmatism of orogenic belts[J]. Northwestern Geology, 2001, 34(3): 18-28.
Citation: XIA Lin-qi. Volcano-magmatism of orogenic belts[J]. Northwestern Geology, 2001, 34(3): 18-28.

造山带火山岩浆作用

Volcano-magmatism of orogenic belts

  • 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.纵观我国以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作用与之相伴.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动力学等重大科学问题.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:板块内部火山岩浆活动、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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收稿日期:  2001-07-12
刊出日期:  2001-09-15

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