@article{oai:ir.kagoshima-u.ac.jp:00005219,
 author = {木村, 政昭},
 journal = {南方海域調査研究報告=Occasional Papers},
 month = {2016-10-28},
 note = {Recent studies strongly support the view that the Okinawa Trough is an active
backarc basin that has not yet undergone full spreading. The crust under the trough is
still regarded to be continental. Extremely high heat flow (max. 1600 mW/m^<2>) has been
measured at the deep small basin in the Middle Okinawa Trough.
An assemblage of the active hydrothermal vent system, including hydrothermal
mounds and associated chimneys, was discovered in the Middle Okinawa Trough in
July, 1986. Such a hydrothermal vent system has not to be observed in backarc basins
any where in the world.},
 pages = {7--23},
 title = {南西諸島周辺の地熱系},
 volume = {11},
 year = {}
}