李敏娟^1,,
沈旭章^1,2,,,
张元生¹,
刘旭宙¹,
梅秀苹¹
1. 中国地震局兰州地震研究所, 兰州 730000
2. 中山大学地球科学与工程学院, 广州 510275

基金项目: 国家自然基金项目（41704057，41574077和41730212），国家重点研发计划（2017YFC1500100），中国地质调查项目（DD20160028）资助


详细信息

作者简介: 李敏娟, 女, 1992年生, 硕士在读, 主要从事地震层析成像方面的研究.E-mail:m1553497399@163.com

通讯作者: 沈旭章, 男, 博士, 教授, 主要从事地球深部结构, 地震学和定点形变观测方面的研究.E-mail:shenxzh5@mail.sysu.edu.cn

中图分类号: P315

收稿日期:2017-11-22
修回日期:2018-04-02
上线日期:2018-05-05

Fine crustal structures of northeast margin of the Tibetan Plateau and structural features of Jiuzhaigou earthquake focal area constrained by the data from a high-density seismic array

LI MinJuan^1,,
SHEN XuZhang^1,2,,,
ZHANG YuanSheng¹,
LIU XuZhou¹,
MEI XiuPing¹
1. Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China
2. School of Earth Science and Engineering, SunYat-sen University, Guangzhou 510275, China


More Information

Corresponding author: SHEN XuZhang,E-mail:shenxzh5@mail.sysu.edu.cn

MSC: P315

--> Received Date: 22 November 2017
Revised Date: 02 April 2018
Available Online: 05 May 2018


摘要
摘要:基于青藏高原东北缘密集宽频带野外流动观测台阵以及固定台站资料，利用双差层析成像方法对地震位置和研究区的地壳速度结构进行了反演.最终用于联合反演的地震事件合计9644个.结果显示青藏高原东北缘速度结构具有明显的横向不均匀性.从整体上看，青藏高原地区表现为低速异常，鄂尔多斯表现为高速异常，而扬子地块亦表现为高速异常.不同深度处速度结构表现不一致，同一深度处P波速度结构和S波速度结构也有明显差异.由西秦岭北缘断裂带、临潭—宕昌断裂以及礼县—罗家堡断裂围限的地震活动强烈的区域中，P波速度结构由深度0 km时呈现的低速异常，逐渐过渡到5 km时高低速相间分布的特征；而S波速度结构在此区域中，由近地表 0 km时高低速相间分布的特征，逐渐过渡到30 km时几乎表现为低速异常.2017年8月8日九寨沟7级地震所在的塔藏断裂、岷江断裂和雪山断裂围限区域，在深度20 km处的P波速度结构和周围存在明显差异，九寨沟地震处于高速异常与低速异常的过渡带内.此外，2013年7月22日发生在青藏高原东北缘的岷漳县6.6级地震，震源区所在的临潭—宕昌断裂附近的P波速度结构在15 km深度处也有明显特征，震源位置所在区域也处于高低速过渡带.该区域这种地壳内部高低速过渡带可能是应力比较容易积累而发生中强地震的一个重要场所.
关键词: 青藏高原东北缘/
九寨沟地震/
双差层析成像/
高低速过渡带

Abstract:We applied the double difference tomography method to simultaneously invert the seismic event locations and the crustal structure of the northeastern Tibetan Plateau with the observations of a high-density temporary seismic array and permanent seismic stations. In total 9644 seismic events are selected for inversion. The results indicate that the velocity structure in the northeastern Tibetan plateau has obvious lateral heterogeneity. Overall, this plateau has low-velocity anomalies, while the Ordos and Yangtze blocks have high-velocity anomalies. The velocity structures at different depths are variable, while the velocity structure of P-waves and S-waves at the same depth are also different. In the region with strong seismic activity enclosed by the faults, such as the West Qinling, Lintan-Dangchang and the Lixian-Luojiapu faults, the velocity structure of P-waves changes from low-velocity anomalies at depth 0km into alternating high and low anomalies at depth 5 km. And in this region, the S wave velocity structure is characterized by the distribution of alternating high and low velocity anomalies at depth 0 km near the surface, and almost low-velocity anomalies at depth 30km. There is a prominent anomaly of the P-wave velocity at depth 20km beneath the area surrounded by the Minjiang, Tazang and Xueshan faults where the Jiuzhaigou M7 earthquake occurred on 8 August 2017. The hypocenter of this event is located in a transition zone between the high- and low-velocity anomalies. In addition, the Min-Zhang M_S6.6 earthquake of 22 July 2013 also took place in such a transition zone. Likely such a transition zone is relatively easy to accumulate stress, leading to occurrence of major earthquakes in this area.
Key words:Northeastern Tibetan plateau/
Jiuzhaigou earthquake/
Double difference tomography method/
Transition zone between high-and low-velocity anomalies



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