东昆仑印支期花岗岩及其对古特提斯洋闭合的启示
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摘要
<正>青藏高原北缘的东昆仑造山带出露大量与古特提斯洋北向俯冲及随后陆陆碰撞相关的花岗质岩类。本文通过对东昆仑格尔木、诺木洪、香日德以及都兰等地花岗岩类详细的野外调研及锆石U-Pb年代学、Hf同位素和地球化学研究,结合已有研究成果,探讨了东昆仑印支期花岗岩类的成因及其对古特提斯演化的启示。
引文
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