Okinawa Trough

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The Okinawa Trough in context of back-arc basins of the world

The Okinawa Trough (沖縄トラフ, Okinawa Torafu) (also called Chinese: 中琉界沟, literally "China-Ryukyu Border Trough"[1]) is a seabed feature of the East China Sea. It is an active, initial back-arc rifting basin which has formed behind the Ryukyu arc-trench system in the West Pacific. It developed where the Philippine Sea Plate is subducting under the Eurasia Plate.[2]

It is a back-arc basin formed by extension within the continental lithosphere behind the far deeper Ryukyu Trench-arc system.[3] The thickness of the crust in the northern Okinawa Trough is 30 km, thinning to 10 km in the southern Okinawa Trough.[4] It has a large section more than 1,000 metres (3,300 ft) deep and a maximum depth of 2,716 metres (8,911 ft).

The Okinawa Trough still in an early stage of evolving from arc type to back-arc activity, and features volcanoes such as the Yonaguni Knoll IV.

Implications for the China–Japan maritime boundary

Notes

References

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