The Southwest Ryukyu Arc is a migrating microplate (forearc sliver)
- 1 June 1989
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 163 (1-2) , 75-91
- https://doi.org/10.1016/0040-1951(89)90119-4
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Tectonics of the hellenic trench: A synthesis of sea-beam and submersible observationsPublished by Elsevier ,2003
- Active collision in eastern Taiwan: The Coastal RangeTectonophysics, 1986
- A synthesis of the geologic evolution of TaiwanTectonophysics, 1986
- Oblique subduction and collision: Forearc tectonics of the Kuril arcGeology, 1986
- Terrane motion by strike-slip faulting of forearc sliversGeology, 1986
- Sunda Strait and Central Sumatra faultGeology, 1984
- TECTONICS OF THE RYUKYU ISLAND ARCJournal of Physics of the Earth, 1978
- Discontinuities in the Deep Seismic Zones Under the Japanese ArcsGSA Bulletin, 1973
- Structure and tectonic evolution of TaiwanAmerican Journal of Science, 1972
- Geotectonic Framework of the Ryukyu Islands (Nansei-shoto)The Journal of the Geological Society of Japan, 1965