Shallow 3D Structure Investigation of Some Cities in the Guangdong–Hong Kong–Macao Greater Bay Area

Xiuwei Ye, Liwei Wang, Cheng Xiong, Xiaona Wang, Genggeng Wen, Dayong Yu, Zhen Guo, Weitao Wang, Zuoyong Lv, Huaping Wu, Yanxin Zhang
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Abstract

The Guangdong–Hong Kong–Macao Greater Bay Area (GBA), known as the fourth largest bay area in the world, is a world-class urban agglomeration located on the southeastern coast of China. Littoral fault zones that might trigger strong earthquakes are located offshore of the GBA, making it particularly crucial to pay attention to seismic disasters caused by the site-amplification effect of the strong earthquakes. Therefore, it is essential to determine the fine subsurface structure of the GBA urban agglomeration. In this study, we present the newly collected short-period dense array seismic data in the core urban area of the GBA, which covers a detection area of 60×60  km2 and consists of a backbone observation network and a basic observation network. The backbone observation network included 720 seismic stations spaced 2.25 km apart that recorded continuously for 30–35 days. The basic observation network has a total of 6214 seismic stations that were spaced 0.75 km apart and recorded continuously for 3–10 days. In addition, 63 excitation shots generated by methane detonation source were fired within the observation network. According to the preliminary analysis, the seismic stations recorded both clear active source signals and an abundance of passive source signals, indicating the high quality of the data. The high density of the seismic array and the high-quality seismic data provide important constraints for constructing the shallow fine crustal structure model and the 3D sedimentary thickness model.
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粤港澳大湾区部分城市浅层三维结构调查
粤港澳大湾区(GBA)被称为世界第四大湾区,是位于中国东南沿海的世界级城市群。可能引发强震的沿岸断裂带位于粤港澳大湾区的近海,因此关注强震的场址放大效应引发的地震灾害尤为重要。因此,确定 GBA 城市群的精细地下结构至关重要。在本研究中,我们展示了新收集的 GBA 核心城区短周期密集阵地震数据,其探测面积为 60×60 km2,由骨干观测网和基本观测网组成。骨干观测网包括 720 个地震台站,间距 2.25 公里,连续记录 30-35 天。基本观测网共有 6214 个地震台站,间距 0.75 千米,连续记录 3-10 天。此外,还在观测网内发射了 63 个由甲烷引爆源产生的激发炮。根据初步分析,地震台站既记录了清晰的主动源信号,也记录了大量的被动源信号,表明数据质量很高。高密度的地震阵列和高质量的地震数据为构建浅部精细地壳结构模型和三维沉积厚度模型提供了重要的约束条件。
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