Structure and growth of the Izu‐Bonin‐Mariana arc crust: 1. Seismic constraint on crust and mantle structure of the Mariana arc–back‐arc system
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- Type
- article
- Published
- 2008-01-01
- Cited by
- 125
- References
- 59
- Access
- Open access
- OpenAlex
- https://openalex.org/W2012021462
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129911681
Keywords
Geology, Crust, Mantle (geology), Mantle wedge, Transition zone
References
- A New Scenario of the Parece Vela Basin Genesis
- The deep structure of non–volcanic rifted continental margins
- Evolution of magma-poor continental margins from rifting to seafloor spreading
- Relationship between seismic P‐wave velocity and the composition of anhydrous igneous and meta‐igneous rocks
- Composition and structure of the central Aleutian island arc from arc‐parallel wide‐angle seismic data
- Tectono-magmatic evolution of the West Philippine-Mariana region and the origin of boninites
- Rifting history of the northern Mariana Trough: SeaMARC II and seismic reflection surveys
- New seismological constraints on growth of continental crust in the Izu-Bonin intra-oceanic arc
- Nature and composition of the continental crust: A lower crustal perspective
- Gravity evidence for an Alpine buckling of the crust beneath the Paris Basin
- Evolution of the Shikoku Basin
- Crustal structure of the Mariana Trough
- Generation of arc basalt magmas and thermal structure of the mantle wedge in subduction zones
- Crustal structure and evolution of the Mariana intra-oceanic island arc
- Three‐dimensional seismic refraction tomography: A comparison of two methods applied to data from the Faeroe Basin
- Possible Miocene rifting of the Izu–Ogasawara (Bonin) arc deduced from magnetic anomalies
- Nature and growth rate of the Northern Izu–Bonin (Ogasawara) arc crust and their implications for continental crust formation
- Crustal construction of a volcanic arc, wide‐angle seismic results from the western Alaska Peninsula
- Crustal structure of the Goban Spur rifted continental margin, NE Atlantic
- Continental Crust, Crustal Underplating, and Low-Q Upper Mantle Beneath an Oceanic Island Arc
Cited by
- Structural, petrological and geochemical constraints on transfer and evolution of arc magmas in the mafic-ultramafic Sapat Complex (Kohistan; Northern Pakistan)
- Petrogenesis and structure of oceanic crust in the Lau back-arc basin
- Crustal shear wave tomography of the Taupo Volcanic Zone, New Zealand, via ambient noise correlation between multiple three‐component networks
- A Geochemical Study of Crustal Plutonic Rocks from the Southern Mariana Trench Forearc: Relationship to Volcanic Rocks Erupted during Subduction Initiation
- Evolution of the Earth as an andesite planet: water, plate tectonics, and delamination of anti-continent
- Seismic imaging of a possible paleoarc in the Izu‐Bonin intraoceanic arc and its implications for arc evolution processes
- Structural variations of arc crusts and rifted margins in the southern Izu‐Ogasawara arc–back arc system
- Crustal structure of the Izu collision zone in central Japan from seismic refraction data
- Along‐arc variation in seismic velocity structure related to variable growth of arc crust in northern Izu‐Bonin intraoceanic arc
- Sedimentary, volcanic, and tectonic processes of the central Mariana Arc: Mariana Trough back‐arc basin formation and the West Mariana Ridge
- Amplitude modeling of the seismic reflectors in the crust‐mantle transition layer beneath the volcanic front along the northern Izu‐Bonin island arc
- Crustal structure across the Costa Rican Volcanic Arc
- Electromagnetic constraints on a melt region beneath the central Mariana back‐arc spreading ridge
- Magma Transfer and Evolution in Channels within the Arc Crust: the Pyroxenitic Feeder Pipes of Sapat (Kohistan, Pakistan)
- Seismic properties of the Kohistan oceanic arc root: Insights from laboratory measurements and thermodynamic modeling
- Optimal nonlinear excitation of decadal variability of the North Atlantic thermohaline circulation
- Geodynamic regimes of intra-oceanic subduction: Implications for arc extension vs. shortening processes
- The composition of the foundered complement to the continental crust and a re-evaluation of fluxes in arcs
- Contrasting subduction structures within the Philippine Sea plate: Hydrous oceanic crust and anhydrous volcanic arc crust
- Foundering of lower island-arc crust as an explanation for the origin of the continental Moho
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