The Okinawa trough in context of back-arc basins of the world.
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


Okinawa trough
Okinawa trough

The existence of the Okinawa Trough complicates descriptive issues in the East China Sea.[5] According to Professor Ji Guoxing of the Asia-Pacific Department at Shanghai Institute for International Studies,

Legal Procedure

On August 15, 2013, China's mission did a presentation to the Commission on the Limits of the Continental Shelf[6][failed verification] (CLCS) established under the United Nations Convention on the Law of the Sea (UNCLOS). The presentation was on the proposal that demarcates the limits of the outer continental shelf beyond 200 nm in part of the East China Sea.[7] China states that China's continental shelf in the East China Sea extends to China-Ryukyu Border Trough naturally, which has been over 200 nautical miles away from the mainland baseline of Chinese territorial waters. According to UNCLOS, any country claiming continental shelves beyond 200 nm shall provide relevant scientific evidence to CLCS. To collect solid data, China deployed 14 scientific survey ships, covering an area of 250,000 square kilometers.[8][9][failed verification]


  1. ^ "Chronology of Defending Diaoyu Islands". Tsinghua University (Beijing) Library. Retrieved 3 June 2013. 横渡中琉界沟黑水沟,进入"琉球大洋",乃因此沟以东属琉球海域,以西包括钓鱼台列屿乃属中国海域。
  2. ^ Thakur, Naresh Kumar et al. (2010). Exploration of Gas Hydrates: Geophysical Techniques, p. 119., p. 119, at Google Books
  3. ^ Sibuet, Jean-Claude et al. "Back arc extension in the Okinawa Trough," Journal of Geophysical Research, Vol. 92, Issue B13, p. 14041-14063.
  4. ^ Backarc basins : tectonics and magmatism. Taylor, Brian, 1953-. New York. 11 November 2013. ISBN 9781461518433. OCLC 883383730.((cite book)): CS1 maint: others (link)
  5. ^ a b c Ji, Guoxing. (1995). "Maritime Jurisdiction in the Three China Seas," p. 10. UC Berkeley: UC Institute on Global Conflict and Cooperation; retrieved 15 Nov 2010.
  6. ^ "CLCS - Home Page".
  7. ^ State Oceanic Administration (August 16, 2013). "China Did a Presentation to CLCS on Demarcating Limits of Over-200-nm Outer Continental Shelf of the East China Sea" (in Chinese). Beijing, China. ((cite web)): Missing or empty |url= (help)[full citation needed]
  8. ^ State Oceanic Administration (August 16, 2013). "Legally and Scientifically Sound--Discussions about China's Proposal on Demarcating Outer Continental Shelf in the East China Sea" (in Chinese). Beijing, China. ((cite web)): Missing or empty |url= (help)[full citation needed]
  9. ^ Xinjing Bao (August 16, 2013). "Experts Discusses China's Proposal" (in Chinese). Retrieved August 16, 2013.