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izu-bonin arc (68) 68
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Physics of the Earth and Planetary Interiors, ISSN 0031-9201, 05/2012, Volume 198-199, pp. 51 - 60
► There are three interfaces at 670, 710 and 730 km beneath Izu-Bonin area. ► The interfaces were depressed approximately 20–30 km in the northern region. ► No... 
N-th root slant stack | 660-km Discontinuity | Izu-Bonin area | Multiplicity | 660-KILOMETER DISCONTINUITY | WAVE-FORMS | TOPOGRAPHY | GEOCHEMISTRY & GEOPHYSICS | TONGA SUBDUCTION ZONE | SCATTERERS | MANTLE DISCONTINUITIES | SEISMIC DISCONTINUITIES | COMPUTATION | NORTHEAST CHINA | STAGNANT SLABS
Journal Article
Geochemical Journal, ISSN 0016-7002, 2016, Volume 50, Issue 6, pp. 461 - 475
The Bayonnaise knoll, an active submarine volcano belonging to an actively rifted part of the Izu-Bonin volcanic arc, exhibits hydrothermal ore deposits on its... 
Sbp | Auv | Hydrothermal deposits | High-resolution acoustic observation | Sub-seafloor | sub-seafloor | SBP | SYSTEM | AUV | RIFT | high-resolution acoustic observation | VOLCANISM | UNDERWATER | GEOCHEMISTRY & GEOPHYSICS | IZU-BONIN ARC | MID-ATLANTIC RIDGE | EVOLUTION | IMAGES | JAPAN | BASIN | hydrothermal deposits
Journal Article
by Cui, QH and Gao, YJ and Zhou, YZ
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, ISSN 0001-5733, 07/2017, Volume 60, Issue 7, pp. 2589 - 2598
The lithosphere-asthenosphere boundary (LAB) is the seismic discontinuity with a negative velocity contrast in the upper mantle. Seismic detections on the LAB... 
Lithosphere-asthenosphere boundary | SUBDUCTION ZONES | KM DISCONTINUITY BENEATH | TOPOGRAPHY | WAVE-FORM DATA | Central South America area | IZU-BONIN | sP precursors | GEOCHEMISTRY & GEOPHYSICS | UPPER-MANTLE | CHEMICAL HETEROGENEITY | TRAVEL-TIMES | Subduction zone | SEISMIC DISCONTINUITIES | STAGNANT SLABS | Slant stack
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 10/2006, Volume 33, Issue 20, p. L20312
[1] We study the discontinuities beneath Tonga subduction zone using the deep earthquakes recorded by the Pacific Northwest Seismic Network (PNSN). The... 
Geographic Location | Subduction zones | Seismology | Continental crust | Tectonophysics | composition and state | Pacific Ocean | Mantle | Earth's interior | GEOSCIENCES, MULTIDISCIPLINARY | SUBDUCTING SLABS | SHARPNESS | TRANSITION ZONE | TRAVEL-TIMES | MANTLE DISCONTINUITIES | TOPOGRAPHY | SEISMIC DISCONTINUITIES | COMPUTATION | IZU-BONIN
Journal Article
Canadian Journal of Earth Sciences, ISSN 0008-4077, 04/2011, Volume 48, Issue 4, pp. 757 - 777
In the Archean Blake River Group, mafic to intermediate fragmental units have controversially been proposed to have formed during the collapse of a giant... 
ROUYN-NORANDA AREA | IZU-BONIN ARC | GEOSCIENCES, MULTIDISCIPLINARY | CANADA | SUPERIOR PROVINCE | ERUPTION | VOLCANO | QUEBEC | SILICIC CALDERA | MASSIVE SULFIDE DEPOSIT | ZIRCON AGES | Volcanic ash, tuff, etc | Research
Journal Article
by Xing, J and Hao, TY and Hu, LT and Suh, MC and Kim, KH
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, ISSN 0001-5733, 01/2016, Volume 59, Issue 1, pp. 116 - 140
The Japan and the IBM subduction zone are located in the place where the Pacific plate, the Philippine Sea plate and the Eurasian plate meet. Both the... 
OCEANIC LITHOSPHERE | DEEP-STRUCTURE | BONIN-MARIANA ARC | Japan | IZU-BONIN | NORTHWESTERN PACIFIC | GEOCHEMISTRY & GEOPHYSICS | SEISMIC CRUSTAL STRUCTURE | Earthquakes | IBM | ADJACENT AREAS | ISLAND ARCS | Subduction zone | Western Pacific | Gravity | LOWER MANTLE BENEATH
Journal Article
Island Arc, ISSN 1038-4871, 06/2005, Volume 14, Issue 2, pp. 178 - 198
Abstract  The structure, paleomagnetism and biostratigraphy of the Nishizaki and Kagamigaura formations on the southern Boso Peninsula, central Japan, were... 
Izu–Bonin island arc | accretionary prism | Boso Peninsula | Tanzawa block | arc collision | Izu-Bonin island arc | Arc collision | Accretionary prism | ROTATION | HONSHU | ZONE | CENTRAL JAPAN | MIDDLE MIOCENE | GEOSCIENCES, MULTIDISCIPLINARY | EVOLUTION | AREA | TRIPLE JUNCTION | TROUGH | PALEOMAGNETISM
Journal Article
Journal of Asian Earth Sciences, ISSN 1367-9120, 09/2017, Volume 146, pp. 265 - 278
The geological processes in the northernmost Philippine Sea plate, which is bounded by the Suruga and Sagami troughs, are a typical example of an active... 
Focal mechanisms | Northernmost Philippine Sea plate | Strike-slip tectonics | Geodesy | PERMANENT DEFORMATION | ZONE | SUBDUCTION | CRUSTAL DEFORMATION | CENTRAL JAPAN | INVERSION | IZU-BONIN ARC | GEOSCIENCES, MULTIDISCIPLINARY | EVOLUTION | EARTHQUAKE | TRANSIENT | Tectonics (Geology) | Strike-slip faults (Geology) | Analysis | Strikes
Journal Article
Earth and Planetary Science Letters, ISSN 0012-821X, 02/2019, Volume 508, pp. 30 - 40
The development of ideas leading to a greater understanding of subduction initiation is limited by the scarcity of present-day examples. Furthermore, the few... 
boninites | subduction initiation | adakites | forearc | ophiolites | subduction zone | FIJI | ISLAND-ARC | SOUTHERN | GEOCHEMISTRY & GEOPHYSICS | ORIGIN | EVOLUTION | FORE-ARC CRUST | TERMINATION | IZU-BONIN-MARIANA | INSIGHTS
Journal Article
地質学雑誌, ISSN 0016-7630, 2010, Volume 116, Issue 3, pp. 134 - 150
Journal Article
Journal of Asian Earth Sciences, ISSN 1367-9120, 2002, Volume 20, Issue 4, pp. 353 - 431
A plate tectonic model for the Cenozoic development of the region of SE Asia and the SW Pacific is presented and its implications are discussed. The model is... 
Continent | Arc | Boundary | continent | boundary | SUMBA ISLAND INDONESIA | WEST PHILIPPINE BASIN | SEISMIC VELOCITY STRUCTURE | ARC-CONTINENT COLLISION | INDIA-EURASIA COLLISION | PAPUA-NEW-GUINEA | STRIKE-SLIP FAULTS | GEOSCIENCES, MULTIDISCIPLINARY | are | EAST SULAWESI OPHIOLITE | SOUTH-CHINA SEA | IZU-BONIN-MARIANA
Journal Article