1. [地质云]滑坡
峨眉山大火成岩省地壳横波速度结构特征及其动力学意义
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摘要
<正>大火成岩省的成因是国际地学界研究的热点。广泛分布于我国川滇黔三省的二叠纪峨眉山玄武岩是中国境内目前唯一被国际学术界认可的大火成岩省,一般认为其形成与二叠纪末期(约258-259Ma)的地幔柱作用有关。自中生代以来,峨眉山大火成岩省至少经历了特提斯洋闭合和印度-亚洲大陆碰撞等重大地质事件,其地质时-空过程和现今所处的构造环境非常复杂。目前关于峨眉山大火成岩省的主
引文
1.Chen,Y.,Badal,J.,Hu,J.,Love and Rayleigh wave tomography of the Qinghai-Tibet Plateau and surrounding areas.Pure and Applied Geophysics,2010,167(10),1171-1203.
    2.Chen,Y.,Xu,Y.,Xu,T.,et al.Magmatic underplating and crustal growth in the Emeishan Large Igneous Province,SWChina,revealed by a passive seismic experiment.Earth and Planetary Science Letters,2015,revised.
    3.He,B.,Xu,Y.,Chung,S.,et al.Sedimentary evidence for a rapid,kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts.Earth and Planetary Science Letters,2003,213(3),391-405.
    4.徐涛,张忠杰,刘宝峰,等.峨眉山大火成岩省地壳速度结构与古地幔柱活动遗迹:来自丽江-清镇宽角地震资料的约束.中国科学:地球科学,2015,45(5):561-576.