The Ryukyu Arc is an island arc which extends from the south of Kyushu along the Ryukyu Islands to the northeast of Taiwan, spanning about 1,200 kilometres (750 mi).[2][3][4] It is located along a section of the convergent plate boundary where the Philippine Sea Plate is subducting northwestward beneath the Eurasian Plate along the Ryukyu Trench.[3][4][5] The arc has an overall northeast to southwest trend and is located northwest of the Pacific Ocean and southeast of the East China Sea.[6] It runs parallel to the Okinawa Trough, an active volcanic arc, and the Ryukyu Trench.[7] The Ryukyu Arc, based on its geomorphology, can be segmented from north to south into Northern Ryukyu, Central Ryukyu, and Southern Ryukyu; the Tokara Strait separates Northern Ryukyu and Central Ryukyu at about 130˚E while the Kerama Gap separates Central Ryukyu and Southern Ryukyu at about 127 ˚E.[2][5][7] The geological units of the arc include igneous, sedimentary, and metamorphic rocks, ranging from the Paleozoic to Cenozoic in age.
^ abKizaki, K. (1978). "Tectonics of the Ryukyu Island Arc". Journal of Physics of the Earth. 26 (Supplement): S301–S307. doi:10.4294/jpe1952.26.Supplement_S301.
^ abShinjo, R.; Kato, Y. (2000). "Geochemical constraints on the origin of bimodal magmatism at the Okinawa Trough, an incipient back-arc basin". Lithos. 54 (3–4): 117–137. Bibcode:2000Litho..54..117S. doi:10.1016/S0024-4937(00)00034-7.
^ abPark, J.-O.; Tokuyama, H.; Shinohara, M.; Suyehiro, K.; Taira, A. (1998). "Seismic record of tectonic evolution and backarc rifting in the southern Ryukyu island arc system". Tectonophysics. 294 (1–2): 21–42. Bibcode:1998Tectp.294...21P. doi:10.1016/S0040-1951(98)00150-4.
^ abShinjo, R.; Chung, S.-L.; Kato, Y.; Kimura, M. (1999). "Geochemical and Sr-Nd isotopic characteristics of volcanic rocks from the Okinawa Trough and Ryukyu Arc: Implications for the evolution of a young, intracontinental back arc basin". Journal of Geophysical Research: Solid Earth. 104 (B5): 10591–10608. Bibcode:1999JGR...10410591S. doi:10.1029/1999JB900040.
^Nakae, S. (2013). "The radiolarian evidence for the accretion of the Fu-saki Formation with the inferred oceanic plate stratigraphy: A case of weakly-metamorphosed accretionary complex in Ishigaki Jima, southern Ryukyu Arc, Japan". Journal of Asian Earth Sciences. 73: 21–30. Bibcode:2013JAESc..73...21N. doi:10.1016/j.jseaes.2013.04.022.
^ abKizaki, K. (1986). "Geology and tectonics of the Ryukyu Islands". Tectonophysics. 125 (1–3): 193–207. Bibcode:1986Tectp.125..193K. doi:10.1016/0040-1951(86)90014-4.
The RyukyuArc is an island arc which extends from the south of Kyushu along the Ryukyu Islands to the northeast of Taiwan, spanning about 1,200 kilometres...
Ryukyu Islands (琉球列島, Ryūkyū-rettō), also known as the Nansei Islands (南西諸島, Nansei-shotō, lit. "Southwest Islands") or the RyukyuArc (琉球弧, Ryūkyū-ko)...
back arc region parallel to the trench, a transect spanning the trench, fore arc and back arc region, and a transect spanning the Ryukyu volcanic arc. The...
Ryukyu dog (琉球犬, Ryūkyū-inu or Ryūkyū-ken) is an endangered, medium-sized breed of dog indigenous to Okinawa, Japan. There were as few as 400 Ryukyu as...
consists of three island arcs from north to south: the Northeastern Japan Arc, the Southwestern Japan Arc, and the Ryukyu Island Arc. The Daitō Islands, the...
"Quaternary Paleo-Geography of the RyukyuArc". Journal of Geography. 105 (3). 1996. "Construction and breakup of the Ryukyu Landbridge and their tectonic...
China-Ryukyu Border Trough ) 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...
contrast subducting northwards beneath the Eurasian Plate, forming the RyukyuArc. Within 200 km of this earthquake, there have been nine events of M≥7...
Plate is in contrast subducting beneath the Eurasian Plate, forming the RyukyuArc. Taiwan's Central Weather Administration (CWA) measured the earthquake's...
in the middle of the Yonaguni Depression, a relatively deep gap in the Ryukyuarc, where the warm Kuroshio Current enters the East China Sea from the Philippine...
the Ryukyu Trench and the island arc that forms the Ryukyu Islands. The Okinawa Plate is bounded on the western side by the Okinawa Trough, a back arc basin...
Subduction zones with high obliquity angles include Sunda trench (ca. 60°) and Ryukyuarc (ca. 50°). Obliquity in plate convergence causes differences in dipping...
Island arcs are long chains of active volcanoes with intense seismic activity found along convergent tectonic plate boundaries. Most island arcs originate...
transporting larvae from southerly coral reefs to downstream reefs along the RyukyuArc. Western boundary currents are used by certain species of squid for rapid...
RyukyuArc 1995, Miyakojima). He is buried in Jerusalem on Rechov Emek Refa'im 1981: NHK 女性手帳 (NHK Jyosei Techō) "琉球狐の女たちよ" (≈ "Women of the Ryukyu Arc")...
Plate is in contrast subducting beneath the Eurasian Plate, forming the RyukyuArc. The earthquake had a moment-magnitude of 8.2 according to the International...
volcanic province, constituting the western end of the island chains of the Ryukyuarc. Five separate bodies can be distinguished: Chilungshan (Mount Keelung)...
Plate is in contrast subducting beneath the Eurasian Plate, forming the RyukyuArc. The earthquake formed the largest of a sequence of events that have affected...
languages were originally and traditionally spoken throughout the Ryukyu Islands, an island arc stretching between the southern Japanese island of Kyushu and...
The Ryukyu independence movement (琉球独立運動, Ryūkyū Dokuritsu Undō) or the Republic of the Ryukyus (Japanese: 琉球共和国, Kyūjitai: 琉球共和國, Hepburn: Ryūkyū Kyōwakoku)...
one of the administrative divisions of the Ryukyu Kingdom Shimajiri Group, a geological group of the RyukyuArc This disambiguation page lists articles associated...
abstract) Katanoda, Itsurō (1999). Ryūkyū ko/noyama no hana From Amai: taiyō no okurimono 琉球弧・野山の花 From Amami: 太陽の贈り物 [RyukyuArc/flowers of the fields and mountains;...
Volcanic Arc Aleutian Islands Kuril Islands Northeastern Japan Arc Japanese Archipelago including the Ryukyu Islands Izu–Bonin–Mariana Arc: Izu Islands...
northeastward and made several landfalls and close approaches over the islands of RyukyuArc. It started weakening while in cold waters and brought rains to Southern...
terrestrial ecoregion of the Ryukyu Islands, also known as the Nansei Islands, in Japan. The Nansei Islands are an island arc that stretches southwest from...