Two‐phase opening model for the Okinawa Trough inferred from paleomagnetic study of the Ryukyu arc
- 10 May 1995
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 100 (B5) , 8169-8184
- https://doi.org/10.1029/95jb00034
Abstract
No abstract availableThis publication has 36 references indexed in Scilit:
- Paleogeographic reconstruction and origin of the Philippine SeaPublished by Elsevier ,2003
- Active hydrothermal mounds in the Okinawa Trough backarc basin, JapanPublished by Elsevier ,2003
- Opening mode of the Okinawa Trough: paleomagnetic evidence from the South Ryukyu ArcTectonophysics, 1990
- The Southwest Ryukyu Arc is a migrating microplate (forearc sliver)Tectonophysics, 1989
- Heat flow anomaly in the middle Okinawa TroughTectonophysics, 1989
- Radio-metric ages of some Cenozoic volcanic rocks from Ryukyu Islands.The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 1987
- The Okinawa Trough: Genesis of a back-arc basin developing along a continental marginTectonophysics, 1986
- Geology and tectonics of the Ryukyu IslandsTectonophysics, 1986
- Fission track ages of some Cenozoic acidic intrusive rocks from Ryukyu Islands.The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 1986
- The instantaneous rotation vector of the Philippine sea plate relative to the Eurasian plateTectonophysics, 1977