摘要
<正>新生代以来,印度板块向欧亚板块的俯冲和碰撞导致了青藏高原的隆升(Molnar et al.,1975)。阿尔金断裂作为青藏高原的西北边界,其北东向的形变分配,对解释青藏高原的动力学机制有重要意义。目前,对于阿尔金断裂的形变分配方式主要存在以下观点:1)中新世中期,断裂延伸进入蒙古、俄罗斯,甚至鄂霍茨克海地区(Worrall et al.,1996);2)断裂在东延至阿拉善块体南缘处以一簇
引文
1.Molnar P et al.,Cenozoic tectonics of Asia:Effects of a continental collision[J].Science,1975,189:419-426.
2.Worrall D M,et al.,Tertiary tectonics of t he Sea of Okhotsk,Russia:Far-field effects of the India-Eurasia collision[J],Tectonics,1996,15:813-826.
3.Zhang P Z,et al.,Late Quaternary and present-day rates of slip along the Altyn Tagh Fault,northern margin of the Tibetan Plateau[J],Tectonic,2007,26,TC5010,doi:10.1029/2006TC002014.
4.陈文彬等,阿拉善地块南缘的左旋走滑断裂与阿尔金断裂带的东延[J].地震地质,2006,28(2):319-324。