摘要
<正>在碰撞造山造山带以外的构造背景中,尤其是在大陆岛弧构造背景中,随着地质年代学技术的快速发展(如SHRIMP、Triton-TIMS,LA-MC-ICP-MS等),在最近几年来,越来越多的研究来确定大型花岗岩岩体的构建过程(Coleman et al.,2004;Glazner et al.,2004;Miller et al.,2007;Schoene and Bowring,2010),已成为国际岩浆作用研究的热点之一,并为深入探讨花岗岩岩体侵位的热效应和理
引文
Coleman D S,Gray W,Glazner A F.2004.Rethinking the emplacement and evolution of zoned plutons:Geochronologic evidence for incremental assembly of the Tuolumne Intrusive Suite,California.Geology,32(5):433-436.
Glazner A F,Bartley J M,Coleman D S,et al.2004.Are plutons assembled over millions of years by amalgamation from small magma chambers?GSA today,14(4/5):4-12.
Miller J S,Matzel J E,Miller C F,et al.2007.Zircon growth and recycling during the assembly of large,composite arc plutons.Journal of Volcanology and Geothermal Research,167(1):282-299.
Schoene B,Bowring S A.2010.Rates and mechanisms of Mesoarchean magmatic arc construction,eastern Kaapvaal craton,Swaziland.Geological Society of America Bulletin,122(3-4):408-429.
王晓先.2013.吉隆地区喜马拉雅造山带中新世构造演化.北京大学,1-116.