王爽^1,2,,
孙新蕾^1,,,
秦加岭^1,2,
何立朋^1,2,
邓阳凡¹
1. 同位素地球化学国家重点实验室, 中国科学院广州地球化学研究所, 广州 510640
2. 中国科学院大学, 北京 100049

基金项目: 广州市科技计划项目（201707020029），国家自然科学基金（41774053）和同位素地球化学国家重点实验室（中国科学院广州地球化学研究所）基金（SKLabIG-16-03）共同资助


详细信息

作者简介: 王爽, 女, 1992年生, 现于中国科学院广州地球化学研究所攻读博士学位, 主要从事地震学方面的研究.E-mail:wang_shuang9279@163.com

通讯作者: 孙新蕾, 女, 研究员, 1976年生, 主要从事地球内部结构及动力学方面的研究.E-mail:xsun@gig.ac.cn

中图分类号: P315

收稿日期:2017-07-13
修回日期:2017-09-11
上线日期:2018-02-05

Fine fault structure of Xinfengjiang water reservoir area from high-frequency ambient noise tomography

WANG Shuang^1,2,,
SUN XinLei^1,,,
QIN JiaLing^1,2,
HE LiPeng^1,2,
DENG YangFan¹
1. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China
2. University of Chinese Academy of Sciences, Beijing 100049, China


More Information

Corresponding author: SUN XinLei,E-mail:xsun@gig.ac.cn

MSC: P315

--> Received Date: 13 July 2017
Revised Date: 11 September 2017
Available Online: 05 February 2018


摘要
摘要:广东河源新丰江水库位于华南典型断层上，自1959年水库蓄水以来，库区地震活动性明显增强，并发生了6.1级触发地震.然而我们对其地下结构的了解还远远不够，对库区地震的研究也因此存在很多不确定性.为了研究库区浅层地下结构，我们在2015年初在新丰江库区人字石断裂周边布设了42个短周期地震仪的密集地震台网.台间距大约为100~500 m，时间跨度为1个月.我们对获得的每个台站的连续信号分段进行处理，并对任意台站对的信号进行互相关和叠加处理，恢复所有台站对间的经验格林函数（EGF）.然后利用多次滤波分析方法测量瑞利波群速度频散曲线，并反演该区域的群速度分布和三维剪切波速度结构.我们的结果表明，对于这样比较密集的台站间距，高频（0.2~1.2 s）频散信号基本可以得到很好的恢复，且该频段信号对浅层地下结构（< 1 km）较为敏感.剪切波速度分布表明该区域人字石断裂位置出现明显的低速分布，并且低速区在断裂南端向两侧延伸，有可能代表与人字石断裂交错的小断裂区域.同时，人字石断裂把该区域划分成了东西两部分，两侧整体上呈现高速异常，与地表山丘相吻合.我们的结果得到了新丰江人字石断裂附近的近地浅层的小尺度精细速度结构，为进一步理解该区域的构造以及地震发生提供了重要依据.
关键词: 新丰江水库/
密集台网/
环境噪声/
层析成像

Abstract:The Xinfengjiang (XFJ) water reservoir in Guangdong, China locates in Yanshanian granites. After the impoundment of the reservoir in 1959, numerous earthquakes occurred, including the M6.1 one in 1962. XFJ water reservoir is one of the most active seismic zones in Guangdong. However, the underground structure of this area is not yet well understood, and there are uncertainties about the mechanism of reservoir earthquakes. To investigate the shallow crustal structure near XFJ water reservoir area, we deployed 42 short period stations near Renzishi Fault (RZSF), with inter-station distance between 100~500 m in year 2015. We retrieved the empirical Green's function (EGF) of all possible station pairs, and obtained their Rayleigh wave group velocity dispersion. Finally, we inverted Rayleigh group velocity and 3D shear wave velocity beneath RZSF area. Our results show that for such dense spacing stations, high frequency (0.2~1.2 s) dispersion signals can be well retrieved, which are important to resolve shallow crustal structure (< 1 km). Shear wave velocity maps show obvious low velocity anomalies beneath RZSF, and this slow anomaly extend to both sides of the fault in the south. The two sides of the RZSF show relatively high velocities, which may correlate with surficial geology. Our results show fine structures of the distribution and geometry of fractures near the RZSF, and provide important constraints in understanding the geological tectonics and seismicity in XFJ water reservoir area.
Key words:Xinfengjiang water reservoir/
Dense array/
Ambient noise/
Tomography



PDF全文下载地址:

http://www.geophy.cn/data/article/export-pdf?id=dqwlxb_14358