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Find link is a tool written by Edward Betts.searching for Mantle wedge 54 found (97 total)
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Forearc
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the mantle wedge closer to the trench is dominated by the denser and colder subducting slab, resulting in a cold, stagnant portion of the mantle wedge. InitialSubcontinental lithospheric mantle (737 words) [view diff] exact match in snippet view article find links to article
the mantle wedge above. Continued subduction of the slab leads to further hydration of the mantle which causes partial melting in the mantle wedge. ItSanukitoid (936 words) [view diff] exact match in snippet view article find links to article
melting of thick crustal roots of island arcs, but these cannot assimilate mantle wedge components so sanukitoids will not form in this setting. SanukitoidsMendocino Triple Junction (1,320 words) [view diff] exact match in snippet view article find links to article
or from the mantle wedge to the east. It turns out that the chemistry of erupted basalts associated with the MTJ are typical of mantle wedge–derived meltsBoninite (941 words) [view diff] exact match in snippet view article find links to article
melting in forearcs via hydration of previously depleted mantle within the mantle wedge above a subducted slab, causing further melting of the already depletedSimberi Island (924 words) [view diff] exact match in snippet view article find links to article
"Carbonated, alkaline hybridizing melts from a sub-arc environment: Mantle wedge samples from the Tabar-Lihir-Tanga-Feni arc, Papua New Guinea". EarthSlab window (866 words) [view diff] exact match in snippet view article find links to article
production in subduction zones generally results from hydration of the mantle wedge due to de-watering of the subducting slab. Slab-window magmatism mayBack-arc region (766 words) [view diff] exact match in snippet view article find links to article
the direction of motion. In addition, mantle convection in the upper mantle wedge caused by the downward movement of the subducted slab causes stress in1987 Chiba earthquake (654 words) [view diff] exact match in snippet view article find links to article
boundary between the serpentinized and unmetamorphosed parts of the mantle wedge is interpreted to be vertical and NNW–SSE trending. The earthquake hadMota Lava (808 words) [view diff] case mismatch in snippet view article find links to article
in Vanuatu Arc Lavas: the Role of Subducted Material and a Variable Mantle Wedge Composition". Journal of Petrology. 38 (10): 1331–1358. doi:10.1093/petrology/38Koryaksky (496 words) [view diff] case mismatch in snippet view article find links to article
Gordeev E., Droznin D. (2002), Complex Anisotropic Structure of the Mantle Wedge Beneath Kamchatka Volcanoes, American Geophysical Union, Fall MeetingBeijing Anomaly (566 words) [view diff] exact match in snippet view article find links to article
deep-seated oceanic lithosphere and “flooding” the overlying lower mantle wedge at depth, giving rise to zones of high elasticity (and potentially fluid-rich)Avachinsky (722 words) [view diff] case mismatch in snippet view article find links to article
Gordeev, E.; Droznin, D. (2002), "Complex Anisotropic Structure of the Mantle Wedge Beneath Kamchatka Volcanoes", American Geophysical Union, Fall MeetingChlorite group (1,250 words) [view diff] exact match in snippet view article find links to article
TL, Chatterjee N, Parman SW, et al. (2006). "The influence of H2O on mantle wedge melting". Earth Planet. Sci. Lett. 249 (1–2): 74–89. Bibcode:2006E&PSLAntigorite (1,126 words) [view diff] case mismatch in snippet view article find links to article
"Serpentinization, Deformation, and Seismic Anisotropy in the Subduction Mantle Wedge". Geochemistry, Geophysics, Geosystems. 21 (4). Bibcode:2020GGG....2108950HMount Tangkoko (246 words) [view diff] exact match in snippet view article find links to article
Quaternary lavas from NE Sulawesi: transfer of subduction components into the mantle wedge". Contr Mineral Petr. 107: 137–149. Media related to Mount Tongkoko atChile Ridge (4,011 words) [view diff] exact match in snippet view article find links to article
eroded rock from the overlying South American Plate, and the sub-arc mantle wedge as well as the chemical composition of the magma, that melts from theConvergent boundary (2,381 words) [view diff] exact match in snippet view article find links to article
ISBN 0-442-20623-2. Taylor, Brian; Martinez, Fernando (March 2002). "Mantle wedge control on back-arc crustal accretion". Nature. 416 (6879): 417–420.Island arc (2,077 words) [view diff] exact match in snippet view article find links to article
melts may result from the up-welling of hot mantle material within the mantle wedge. If hot material rises quickly enough so that little heat is lost, theQiangtang terrane (528 words) [view diff] exact match in snippet view article find links to article
(Central Tibet): evidence for metasomatism by slab-derived melts in the mantle wedge". Contributions to Mineralogy and Petrology. 155 (4): 473–490. Bibcode:2008CoMPLautaro (volcano) (1,885 words) [view diff] exact match in snippet view article
Stern, C. R.; Kilian, Rolf (15 April 1996). "Role of the subducted slab, mantle wedge and continental crust in the generation of adakites from the Andean AustralSubduction (8,277 words) [view diff] exact match in snippet view article find links to article
seismicity and induce melting within the subducted plate and in the overlying mantle wedge. This type of melting selectively concentrates volatiles and transportsPartial melting (1,854 words) [view diff] exact match in snippet view article find links to article
Stephen W.; Médard, Etienne (2006-09-15). "The influence of H2O on mantle wedge melting". Earth and Planetary Science Letters. 249 (1): 74–89. Bibcode:2006E&PSLUltra-high-pressure metamorphism (3,643 words) [view diff] exact match in snippet view article find links to article
that both subducted sediment and crystalline rocks may rise through the mantle wedge diapirically to form UHP terranes. Diapiric rise of a much larger subductedAndean Volcanic Belt (2,748 words) [view diff] exact match in snippet view article find links to article
variations in the Southern Volcanic Zone, Chile (34.5–38.0°S): Constraints on mantle wedge and slab input compositions" (PDF). Geochimica et Cosmochimica Acta.Shatsky Rise (1,688 words) [view diff] exact match in snippet view article find links to article
Coffin, M. F.; Kimura, J. I.; Hirano, N.; Nakanishi, M. (2007). "Depleted mantle wedge and sediment fingerprint in unusual basalts from the Manihiki PlateauPeridotite (3,793 words) [view diff] no match in snippet view article find links to article
Xenoliths from Iraya Volcano, Philippines, and its Implication for Dynamic Mantle-Wedge Processes". Journal of Petrology. 45 (2): 369–389. doi:10.1093/petrology/egg100South Fiji Basin (1,553 words) [view diff] case mismatch in snippet view article find links to article
Mortimer et al. 2007, Table 2 Todd et al. 2011, section:5.2. Havre Ambient Mantle Wedge (AMW) Todd et al. 2011, section:Abstract Mortimer et al. 2007, Fig.1Igneous rock (5,657 words) [view diff] exact match in snippet view article find links to article
Chatterjee, N.; Parman, S. W.; Medard, E. (2006). "The influence of H2O on mantle wedge melting". Earth and Planetary Science Letters. 249 (1–2): 74–89. Bibcode:2006E&PSLLau-Colville Ridge (1,360 words) [view diff] exact match in snippet view article find links to article
"Hf isotopic evidence for small‐scale heterogeneity in the mode of mantle wedge enrichment: Southern Havre Trough and South Fiji Basin back arcs". GeochemistryReclus (volcano) (3,737 words) [view diff] exact match in snippet view article
Stern, C. R.; Kilian, Rolf (1996-04-01). "Role of the subducted slab, mantle wedge and continental crust in the generation of adakites from the Andean AustralTonga-Kermadec Ridge (873 words) [view diff] exact match in snippet view article find links to article
within the Tonga-Kermadec-Lau arc-back-arc systems: the role of varying mantle wedge composition in space and time" (PDF). Journal of Petrology. 39 (3): 331–368Yilgarn Craton (3,249 words) [view diff] exact match in snippet view article find links to article
are found in many large deposits, including melts from metasomatised mantle wedge as well as lamprophyres. Debate continues whether these mantle rocksHavre Trough (1,807 words) [view diff] exact match in snippet view article find links to article
from the Kermadec Ridge arc front. This is consistent with the ambient mantle wedge under the Havre Trough being Pacific during its current rifting stageMonte Burney (4,156 words) [view diff] exact match in snippet view article find links to article
(1999-09-02). "Reaction between slab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8 GPa". Chemical Geology. 160 (4): 335–356Volcano (9,967 words) [view diff] exact match in snippet view article find links to article
the subducting plate lowers the melting temperature of the overlying mantle wedge, thus creating magma. This magma tends to be extremely viscous becauseMagma (7,678 words) [view diff] exact match in snippet view article find links to article
Chatterjee, N.; Parman, S. W.; Medard, E. (2006). "The influence of H2O on mantle wedge melting". Earth and Planetary Science Letters. 249 (1–2): 74–89. Bibcode:2006E&PSLMount Rinjani (4,575 words) [view diff] no match in snippet view article find links to article
volcanoes, probably originated by partial melting of the peridotite mantle-wedge overlying the active Benioff Zone beneath Lombok Island. The Pleistocene-RecentSerpentinization (3,139 words) [view diff] exact match in snippet view article find links to article
Huang, Haibo (31 May 2017). "Degree of serpentinization in the forearc mantle wedge of Kyushu subduction zone". International Geophysical Conference, QingdaoSunda Arc (3,696 words) [view diff] exact match in snippet view article find links to article
the Eurasia Plate. Magma originates from the partial melting of the mantle wedge driven by the fluids from the subducting slab. In addition, volcanicWells Gray-Clearwater volcanic field (3,460 words) [view diff] exact match in snippet view article find links to article
the subducted plate asthenosphere may possibly flow upward into the mantle wedge. Similarly, if the displacement had a section of extension, a horizontalSubduction zone metamorphism (2,315 words) [view diff] exact match in snippet view article find links to article
magmas are produced by partial melting of metasomatic domains in the mantle wedge, which have reacted with liquid phases derived from dehydration meltingTaunshits (1,311 words) [view diff] exact match in snippet view article find links to article
January 2008). "Some first-order observations on magma transfer from mantle wedge to upper crust at volcanic arcs". Geological Society, London, SpecialSouth China Craton (7,502 words) [view diff] exact match in snippet view article find links to article
adakitic rock A conventional way to generate magma is by melting in the mantle wedge which is aided by the fluid release from the subducted slab. HoweverLau Basin (3,837 words) [view diff] exact match in snippet view article find links to article
Section:2. Geological Setting Martinez, Fernando; Taylor, Brian (2002). "Mantle wedge control on back-arc crustal accretion". Nature. 416 (6879): 417–420.List of common misconceptions (55,573 words) [view diff] exact match in snippet view article find links to article
(March 31, 2015). "Temperature and melt fraction distributions in a mantle wedge determined from the electrical conductivity structure: Application toIkuo Kushiro (999 words) [view diff] exact match in snippet view article find links to article
J. Geophys. Res. 81, 6347–50. I. Kushiro (1990) Partial melting of mantle wedge and evolution of island arc crust. J. Geophys. Res. 95, 15929–39. I.Geology of New Caledonia (6,217 words) [view diff] exact match in snippet view article find links to article
(December 2015). "Strain localization and fluid infiltration in the mantle wedge during subduction initiation: Evidence from the base of the New CaledoniaGreg Hirth (1,928 words) [view diff] exact match in snippet view article find links to article
Hirth, Greg; Kelemen, Peter B. (2003). "Arc‐parallel flow within the mantle wedge: Evidence from the accreted Talkeetna arc, south central Alaska". JournalWhakatāne Graben (1,670 words) [view diff] exact match in snippet view article find links to article
tectonomagmatic relationship, where magmas supplied by flux melting in the mantle wedge thermally weaken the lithosphere and facilitate rifting. For more detailMount Churchill (8,353 words) [view diff] case mismatch in snippet view article find links to article
Xuran; Zhao, Dapeng; Hua, Yuanyuan; Xu, Yi-Gang (January 2024). "Big Mantle Wedge and Intraplate Volcanism in Alaska: Insight From Anisotropic Tomography"Intraplate volcanism (11,934 words) [view diff] exact match in snippet view article find links to article
trace elements. This enriched fluid rises to metasomatize the overlying mantle wedge and leads to the formation of island arc basalts. The subducting slabAppinite (4,394 words) [view diff] case mismatch in snippet view article find links to article
from the Qinling Orogen (Central China): Hydrous Melting of Depleted Mantle Wedge in Post-Collision Stage". Minerals. 2023 (3): 441. Bibcode:2023Mine.Magmatism along strike-slip faults (5,444 words) [view diff] case mismatch in snippet view article find links to article
Kelemen P. (2002). Thermal Structure due to Solid-State Flow in the Mantle Wedge Beneath Arcs. Hutton, D. H. W.; Reavy, R. J. (1992). "Strike-slip tectonics