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柴西北地区碎屑锆石裂变径迹年龄记录的阿尔金山早新生代隆升事件
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摘要
<正>阿尔金山作为青藏高原地理意义上的北界,对限定青藏高原的隆升和变形机制有重要意义[1-6]。研究阿尔金山体系在响应印度-欧亚板块碰撞过程中构造演化特性的工作,已经广泛开展[3,5,7-20]。大量热年代学数据显示,阿尔金山渐新世(40~30Ma)以来发生阶段性隆升,而新生代初期隆升的热年代学记录极少。山体是其相邻盆地的主要物源,盆地碎屑矿物若未发生退火,其记录的信息对理解山体隆升特征及历史至关重要。柴达木盆地夹持在昆仑山、阿尔金山和祁连山之间,新生代发展演化受周
引文
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