| 基于大地电磁测深的藏南雅鲁藏布江缝合带电性结构研究 |
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| 引用本文： | 徐新学,陈宇坤,高武平,袁航,闫成国,雷清,郑军.基于大地电磁测深的藏南雅鲁藏布江缝合带电性结构研究[J].地震学报,2020,42(4):406-418. |
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| 作者姓名： | 徐新学 陈宇坤 高武平 袁航 闫成国 雷清 郑军 |
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| 作者单位： | 1.中国天津 300170 天津市地球物理勘探中心 |
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| 基金项目： | “日喀则市活动断层探测与地震危险性评价”项目（藏震函[2011]77号）资助 |
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| 摘 要： | 为研究日喀则市活动断裂深浅部构造关系及深部孕震机制，跨雅鲁藏布江谢通门—日喀则段部署了48个宽频大地电磁测深点，剖面长度为108 km。在二维反演的基础上对壳幔200 km深度范围内的电性结构进行了探测研究。剖面自南向北依次经过喜马拉雅地块、雅鲁藏布江缝合带和拉萨—冈底斯地块。喜马拉雅地块地壳表现为高阻特性，其北侧的仲巴—郎杰学陆缘移置混杂地体发育了深达上地幔盖层的巨厚的北倾低阻体；雅鲁藏布江主缝合带表现为喇叭状低阻通道，宽约10 km，存在深浅部两处低阻体，浅部南倾深部北倾，低阻通道南部发育近似直立或南倾的高阻日喀则蛇绿岩，北部发育近直立的高阻冈底斯花岗岩体，整体表现为两个高阻异常体中间夹一个连通壳幔的带状低阻通道；拉萨—冈底斯地块以高阻为主，中下地壳普遍发育低阻体。缝合带附近因板块俯冲作用导致壳幔局部增厚或减薄，表现为电性的梯度变化，表现为低阻特性的部分则是壳幔物质的运移通道。
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| 关 键 词： | 雅鲁藏布江缝合带 大地电磁测深 电性结构 |
| 收稿时间： | 2019-11-18 |
The electrical structure beneath the Yarlung Zangbo suture zone in southern Tibet |
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| Affiliation: | 1.Tianjin Geophysical Exploration Center，Tianjin 300170，China2.Tianjin Earthquake Agency，Tianjin 300201，China |
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| Abstract: | In order to study the tectonic relationship between the shallow and deep active faults as well as deep seismogenic machanism around Xigaze city in South Tibet, totally 48 wide-band magnetotelluric sounding points were deployed on a 108 km long line across the Xietongmen-Xigaze section of the Yarlung Zangbo suture zone （YZSZ） , hence 2D inversion technique was employed to reveal the deep electrical structure whose depth range is less than 200 km. This south-north trending profile passes through the Himalayan block, YZSZ and Lhasa-Gangdise block in turn. Most of the crust beneath the Himalayan block is of high resistance, and at the north side of the Zhongba-Langjie xue continental margin displaced mixed terrane, it develops a huge north-dipping high conductive body that stretches downward into the upper mantle. There exists a 10 km wide trumpet-shaped low resistance tunnel and two typical high conductive bodies beneath the YZSZ, of which the shallow one is south-dipping whereas the deep one is north-dipping. Besides, in the crust and upper mantle beneath the YZSZ, there also develops two high resistance bodies, the southern one is nearly vertical or south-dipping ophiolite, and the northern one is upright Gangdise granite. Hence it expresses like a low-resistance channel clamped by those two bodies stretching downward into the upper mantle. Lhasa-Gangdise block is dominated by high resistance and the high conductive bodies are generally developed within the middle and lower crust. The subduction of Indian plate leads to the local thicken and thinning of the crust and mantle, therefore there exhibits an obvious gradient change nearby themajor suture belt （MSB） , and the YZSZ control the migration channel of crust-mantle material. |
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