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- W3118591711 abstract "The Okinawa Trough is an active back-arc basin of the Ryukyu island arc-trench system caused by the Phillippine Sea plate subduction. Its unique location makes it attractive to study the lithosphere of continental margins, and it is of great significance to understand the dynamic mechanism of the trench-arc-basin convergent plate boundary. In this paper, we developed the spectral correlation method to calculate the effective elastic thickness of the lithosphere in the study area. The results show that the effective elastic thickness of the lithosphere is distributed in the range of 9–30 km and the lithosphere strength gradually decreases accordingly. Comparing the spatial variations of effective elastic thickness with the data sets of tectonic activities, we conclude that: The spatial variations of the effective elastic thickness have the negative correlation with that of the heat flow. The thermal tectonic activities of the trough gradually become intense from north to south. There are close links between the spatial variations of the effective elastic thickness and the distribution earthquakes. Most of earthquakes are distributed in the relatively lower effective elastic thickness areas or steep effective elastic thickness gradient zones, which indicate that the weak lithosphere and areas with steep change of effective elastic thickness are prone to accumulate and then release tectonic stresses causing earthquakes. The total characteristics of tectonic activities of the Okinawa Trough indicate a strong trend from north to south in the deep region, and the opposite in the shallow region." @default.
- W3118591711 created "2021-01-18" @default.
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- W3118591711 date "2021-04-01" @default.
- W3118591711 modified "2023-10-18" @default.
- W3118591711 title "Spatial variations of effective elastic thickness of the lithosphere in the Okinawa Trough" @default.
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- W3118591711 doi "https://doi.org/10.1016/j.jseaes.2021.104670" @default.
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