任昱^1,4,,
赵明辉^1,2,4,,,
张佳政^1,2,
吕作勇³,
庞新明^1,4,
丘学林^1,2,4
1. 中国科学院边缘海与大洋地质重点实验室, 中国科学院南海海洋研究所, 广州 510301
2. 中国科学院南海生态环境工程创新研究院, 广州 510301
3. 中国地震局地震监测与减灾技术重点实验室, 广东省地震局, 广州 510070
4. 中国科学院大学, 地球与行星科学学院, 北京 100049

基金项目: 国家自然科学基金项目（91958212，91428204，41730532，41576070，41676043，41606064），促进海峡两岸科技合作联合基金（U1505232）和国家自然科学基金委员会共享航次（NORC2015-08，NORC2016-08）联合资助


详细信息

作者简介: 任昱, 男, 1995年生, 硕士, 研究方向为海洋地球物理.E-mail:yren@scsio.ac.cn

通讯作者: 赵明辉, 女, 1967年生, 博士, 研究员, 主要从事海洋地球物理与深部结构研究.E-mail:mhzhao@scsio.ac.cn

中图分类号: P315,P738

收稿日期:2019-01-07
修回日期:2019-07-04
上线日期:2020-05-05

Constraint on the shape of the Manila subduction slab from earthquake relocation using long-term ocean bottom seismometer data

REN Yu^1,4,,
ZHAO MingHui^1,2,4,,,
ZHANG JiaZheng^1,2,
LV ZuoYong³,
PANG XinMing^1,4,
QIU XueLin^1,2,4
1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
2. Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
3. Key Laboratory of Earthquake Monitoring and Disaster Mitigation Technology, China Earthquake Administration, Guangdong Earthquake Agency, Guangzhou 510070, China
4. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China


More Information

Corresponding author: ZHAO MingHui,E-mail:mhzhao@scsio.ac.cn

MSC: P315,P738

--> Received Date: 07 January 2019
Revised Date: 04 July 2019
Available Online: 05 May 2020


摘要
摘要:将宽频带OBS用于海底天然地震长期观测，在国内尚处于实验阶段.2015年在马尼拉俯冲带北段开展了为期6个月的宽频带海底天然地震观测试验.根据回收的1台海底地震仪（OBS04）与国际地震台网的718台陆地地震台站，共记录到7562个P波走时和5002个S波走时数据，利用Hyposat地震定位方法，对马尼拉俯冲带北部（119°E—123°E，19°N—22°N）在2015年8月至2016年2月期间的264个地震进行了重定位.地震重定位的结果及定位误差分析表明，在海域布设的OBS04台站让地震观测的空间分布更为合理，提高了地震定位精度；重定位后的震中分布更为集中，与地质构造吻合良好；浅部的地震活动较为活跃，分布密集，与浅部断层发育有关；重定位后的4条震源深度投影剖面，从不同角度较好地约束了俯冲板片上边界的板片形态，板片倾角在浅部0~30 km区间约为10°~22°，随着深度的增加，俯冲板片逐渐变陡，在深度120~180 km处倾角约为41°~58°.该项研究为马尼拉俯冲带北段的板片形态提供了重要约束，而且为今后长期天然地震观测提供了重要而宝贵的经验与借鉴.
关键词: 地震观测/
宽频带海底地震仪/
马尼拉俯冲带/
地震重定位

Abstract:The broadband Ocean Bottom Seismometer (OBS) observation is still in the experimental stage. One experiment was carried out for 6 months in the northern Manila subduction zone in 2015. We picked 7562 P-wave and 5002 S-wave travel-times recorded by a broadband station (OBS04) and 718 land stations. Totally 264 earthquakes that occurred from August 2015 to February 2016 in the study area (119°E—123°E, 19°N—22°N) were relocated using the Hyposat method. The results show that the hypocenter accuracy has been improved due to the addition of OBS04 deployed near the Manila Trench and reasonable spatial distribution of seismic stations. The hypocenters of relocated earthquakes are much more concentrated and fit well with geological structures than before. Shallow seismic events are dominant and concentrating in this area, which are related to the faults in crust. Four projection profiles of focal depths of relocated earthquakes reveal the upper boundary of the slab in the northern seismic concentrating region. The angles of the subduction slab increase from 10°~22° in the shallow (0~30 km) to 41°~58° in the deep subsurface (120~180 km). This research provides a significant constraint on the slab shape of the northern Manila subduction zone as well as valuable experiences and references for broadband OBS observation in the future.
Key words:Earthquake observation/
Ocean Bottom Seismometer (OBS)/
Manila subduction zone/
Earthquake relocating



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