INDEPTH-Ⅲ地震层析成像——藏北印度岩石圈俯冲断落的证据  

Seismic Imaging of the Subducting Indian Lithosphere beneath North Tibet

作　　者：赵文津[1] 薛光琦[2] 赵逊[1] 吴珍汉[3] 史大年[2] 刘葵[2] 江万[2] 熊嘉育[1] 

机构地区：[1]中国地质科学院,北京100037 [2]中国地质科学院矿产资源研究所,北京100037 [3]中国地质科学院地质力学研究所,北京100081

出　　处：《地球学报》2004年第1期1-10,共10页Acta Geoscientica Sinica

基　　金：国土资源部项目 (95 0 12 0 7);国家科技部项目(9792 4)资助

摘　　要：德庆 龙尾错剖面层析速度结构剖面揭示了在高原地壳发生缩短与增厚后 ,高速的印度大陆地幔岩石圈分为两层以不同角度向北伸展到羌塘盆地的中部 ( 33°N～ 34°N之间 )。上层在拉萨地块岩石圈 (速度为 7.9～ 8.0km/s)之下向北伸展过程中发生断裂 ,形成若干断块 ,并下沉 ;下层以较大角度向北俯冲下去 ,并在 32°N之下进入软流圈 ;发现北部有一浅一深 2条低速带 ,可能代表地幔内温度较高的热流体的流动通道 ,并产生强烈的各向异性。浅处低速带与深部低速带有联系 ;此低速带与东部Wittlinger发现的 34.5°N深部的高温低速体没有直接联系 ,后者呈NW—SE走向。A tomographic image of the upper mantle beneath Central Tibet from INDEPTH III seismic data has revealed two high velocity layers in the Lower Velocity Zone of the Upper Mantle. It is referred that these two layers are the northward continuation of Indian high velocity lithosphere. While the upper layer was broken down and subsided in its northward extending process beneath the Lhasa Block Lithosphere, the other layer was subducting gently into the asthenosphere under 32°N. It is suggested that the two lo wer velocity belts, located just north of 33°N at different depths, are not related to the deep Lower Velocity Body at 35.5°N disco vered by Wittlinger in 1996, and that they might have originated from another thermo fluid source at 32°N,91°E.

关 键 词：地震波 层析成像 地幔 热流体 低速层 反演 印度大陆高速岩石圈 

分 类 号：P315[天文地球—地震学]