Structural characteristics of the Littoral Fault Zone in East Guangdong offshore area, northern South China Sea, from new high-resolution seismic reflection data
ID:3018 View Protection:PRIVATE Updated Time:2023-04-12 19:37:21 Hits:1929 Oral Presentation

Start Time:2023-05-06 13:35(Asia/Shanghai)

Duration:10min

Session:6A 6A、海洋地球科学 » 6A-16A-1 海洋地球科学

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Abstract
Two destructive earthquakes in 1600 and 1918, with magnitudes of 7.0 and 7.5, highlight that the offshore area of East Guangdong is one of the most seismically active regions in the rifted northern margin of the South China Sea (SCS). However, the location and extent of the main active faults in this area remain poorly constrained. Using newly acquired high-resolution multi-channel seismic (MCS) reflection data, we investigate the detailed offshore fault structure of East Guangdong. The interpreted data reveal the location, continuity and geometry of the NEE-strike Littoral Fault Zone (LFZ). The LFZ consists of a series of large basement faults which form a terraced sidewall fault zone and correspond to negative high gravity anomalies. It is distributed roughly parallel to the coastline at a distance about 30-60 km with a fault zone width of about 25-60 km. The fault zone was active during the Cenozoic, and recorded significant intraplate deformation during the continental rifting with fault displacement of kilometer level. As the significant basement changes and the low velocity characteristics derived from wide-angle seismic data, we propose the LFZ to be a lithospheric-scale fault zone separating the northern margin of the SCS from the South China Block. The listric faults in the LFZ control the formation and development of sedimentary basins or depressions. Many active faults were identified near the seafloor, which correspond well to the locations of the recent earthquakes. The NEE-trending LFZ intersected with the NW-trending active faults, resulting in a weak tectonic zone in the crust, which is probably the reason for frequent seismicity and strong earthquakes distribution in this area. Intense Cenozoic magmatism, Middle Miocene in age, was identified in the profile near the Nanpeng Islands. The widely developed fault structures provide pathways for the upward migration of magma. The NW-trending faults may have caused the fault zone to be dislocated and blocked the westward transport of magma.
 
Keywords
Littoral Fault Zone,multi-channel seismic profile,East Guangdong offshore area,Northern South China Sea,offshore active faults
Speaker
张严心
广东省地震局

Submission Author
张严心 广东省地震局
叶秀薇 广东省地震局
万奎元 中国科学院南海海洋研究所
吕作勇 广东省地震局
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Important Date
  • Conference Date

    May 05

    2023

    to

    May 08

    2023

  • Mar 31 2023

    Draft paper submission deadline

  • May 25 2023

    Registration deadline

Sponsored By
青年地学论坛理事会
中国科学院青年创新促进会地学分会
Organized By
武汉大学
中国科学院精密测量科学与技术创新研究院
中国地质大学(武汉)
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