喜马拉雅造山带晚奥陶纪-早志留纪地质事件记录
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摘要
<正>青藏高原是由"多陆块、多岛弧"组成,自新元古代以来,经历了长期的构造岩浆作用,记录了"多洋盆、多俯冲、多期碰撞和多期造山"的动力学作用过程(Hsu et al.,1995;Yin and Harrison,2000),又称为"造山的高原"(Dewey,et al.,2005;许志琴等,2006)。现有数据表明,自~750 Ma以来,喜马拉雅陆块与冈瓦纳超大陆的微陆块(拉萨、羌塘等)经历了多期构造活动(Hodges,2000;Yin and
引文
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