Neotectonics in Southern Ryukyu arc by means of paleostress analysis
Paleostress estimation is essential in understanding the tectonics of the Southern Ryukyu arc. We have used Multiple inverse method (Yamaji, 2000) and Ginkgo method (Yamaji, 2003) to detect paleostress from the fault-slip data collected in the Southern Ryukyu arc where 23 groups of stress (stresses A-W) are devided. We suggest that stress transition in
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Upper Mantle Velocity Structure beneath the Ryukyu-Taiwan Arc
Hideki INATANI, Kei KURITA
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6 Heat flow around the Ryukyu Arc
Yamano, Makoto +2 more
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Divergence With Gene Flow and Contrasting Population Size Blur the Species Boundary in Cycas Sect. Asiorientales, as Inferred From Morphology and RAD-Seq Data. [PDF]
Chang JT +5 more
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Interchanges and movements of humpback whales in Japanese waters: Okinawa, Ogasawara, Amami, and Hokkaido, using an automated matching system. [PDF]
Kobayashi N +13 more
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Intermediate Earthquakes in a Northern Part of the Kyushu-Ryukyu Arc
Toshiki KAKUTA +2 more
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Phylotranscriptomics and genome-size evidence clarify the Taiwanese Cirsium japonicum complex and delimit C. brevicaule and allied East Asian thistles. [PDF]
Chang CY +5 more
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Sources of dehydration fluids underneath the Kamchatka arc. [PDF]
Shu Y +5 more
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Evidence of megathrust earthquakes and seismic supercycles in subtropical Japan from millennia-old coral microatolls. [PDF]
Debaecker S +12 more
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Phylogeography of Ryukyu insular cicadas: Extensive vicariance by island isolation vs accidental dispersal by super typhoon. [PDF]
Osozawa S +3 more
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