The crustal structure of the Eastern Subbasin of the South China Sea: constraints from receiver functions

Author:

Liu Yanan123ORCID,Liu Baohua34,Liu Chenguang123,Hua Qingfeng23

Affiliation:

1. College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

2. The First Institute of Oceanography, Ministry of Natural Resources of China, Qingdao 266061, China

3. Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China

4. National Deep Sea Center, Ministry of Natural Resources of China, Qingdao 266061, China

Abstract

SUMMARY The crustal structure is a window to understand the tectonic evolution of an area. Through the first large-scale passive-source ocean bottom seismometer (OBS) array observation experiment in the Eastern Subbasin of the South China Sea (ESSCS), we calculated and obtained the respective receiver functions of these stations. As OBS works on the seafloor, where the working environment is different from that for its land-based counterpart, the effects of the sea-water layer and the oceanic low-velocity sediment layer on the seismic signals must be evaluated. Receiver functions’ synthetic test demonstrates the following: the presence of the sea-water layer produces a strong negative-amplitude phase (Pwp) in the receiver function, and the arrival time of this phase is delayed as the thickness of the sea-water layer increases; the presence of the low-velocity sediment layer produces a strong positive-amplitude phase (Pseds) which causes a delay in the arrival time of the Moho-related phases of the receiver function and makes them difficult to distinguish. On the basis of phase identification and synthetic tests, we estimate crustal thickness beneath each of the stations using two approaches. The first approach utilizes the observed arrival time of Moho phases, and the second approach finds the optimal crustal thickness by comparing the synthetic and observed receiver functions, which leads to more reliable results. The results of the second method show that the thickness of the sediment in the study area is mainly controlled by seafloor topography, the thickness of the crust in the seamount area is affected by the magma supply during the expansion stage and the post-spreading magmatism, and the crust in the flat basin is only affected by the magma supply during the expansion period. Moreover, the crust in the area affected by magmatic activity after the expansion stage is thicker than that in the area not affected.

Funder

National Natural Science Foundation of China

National Program on Global Change and Air-Sea Interaction

China Ocean Mineral Resources R&D Association

Taishan Scholar Project of Shandong Province

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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