- Okinawa Plate
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The Okinawa Plate is a long narrow tectonic plate stretching from the northern end of Taiwan to the southern tip of the island of Kyūshū. To the east lies the Ryukyu Trench and the Pacific Plate. It is separated from the Yangtze Plate (often considered part of the Eurasian Plate) by a rift that forms the Okinawa Trough which is a Back arc basin.
References
Bird, P. (2003) An updated digital model of plate boundaries, Geochemistry Geophysics Geosystems, 4(3), 1027, doi:10.1029/2001GC000252. [1]
Tectonic plates of East Asia (Eurasian Plate-Pacific Plate Convergence Zone) Large Small Faults and rift zones Baikal Rift Zone · Fukozu Fault · Idosawa Fault · Itoigawa-Shizuoka Tectonic Line · Izu-Bonin-Mariana Arc · Izu Convergence Zone · Japan Median Tectonic Line · Longmenshan Fault · Neodani Fault · Nojima Fault · Northeastern Japan Arc · Philippine Fault System · Senya Fault · Tanna Fault · Ulakhan FaultTrenches and troughs Kuril Trench · Mariana Trench · Japan · Izu-Ogasawara Trench · Japan Trench · Nankai Trough · Sagami Trough · Suruga Trough · Okinawa Trough · Ryukyu Trench · Philippines: · North Luzon Trough · West Luzon Trough · Manila Trench · Philippine Trench · Cotabato Trench · East Luzon Trench · Sulu Trench · Negros Trench · Palawan Trench ·Other Boso Triple JunctionThis tectonics article is a stub. You can help Wikipedia by expanding it.