藏南特提斯喜马拉雅带辉绿岩始新世——渐新世变质作用
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摘要
<正>印度—欧亚陆陆碰撞作用是新生代最壮观的地质事件之一,导致了喜马拉雅造山带和青藏高原的崛起,深远地影响着区域甚至全球气候。厘定印度—欧亚陆陆碰撞作用的起始时间是深入理解该碰撞事件构造岩浆作用和环境资源效应等重要地质过程的关键时间坐标。随着印度大陆岩石圈的北向俯冲,碰撞带上下两盘都发生缩短增厚和相应的变质作用。特提斯喜马拉雅带位于碰撞带的下盘,
引文
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