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O. Sigmarsson, M. Condomines, J. Morris, R. Harmon (1990)
Uranium and 10Be enrichments by fluids in Andean arc magmasNature, 346
S. Sorensen, J. Grossman (1989)
Enrichment of trace elements in garnet amphibolites from a paleo-subduction zone: Catalina Schist, southern CaliforniaGeochimica et Cosmochimica Acta, 53
G. Wörner, R. Harmon, J. Davidson, S. Moorbath, D. Turner, N. McMillan, C. Nyes, L. Lopez-escobar, H. Moreno (1988)
The Nevados de Payachata volcanic region (18°S/69°W, N. Chile)Bulletin of Volcanology, 50
F. McDermott, Marc Defant, C. Hawkesworth, R. Maury, J. Joron (1993)
Isotope and trace element evidence for three component mixing in the genesis of the North Luzon arc lavas (Philippines)Contributions to Mineralogy and Petrology, 113
Y. Tatsumi, M. Murasakia, S. Nohda (1992)
Across-arc variation of lava chemistry in the Izu-Bonin Arc: identification of subduction componentsJournal of Volcanology and Geothermal Research, 49
F. Tera, L. Brown, J. Morris, I. Sacks, J. Klein, R. Middleton (1986)
Sediment incorporation in island-arc magmas: Inferences from 10BeGeochimica et Cosmochimica Acta, 50
J. Woodhead, R. Johnson (1993)
Isotopic and trace-element profiles across the New Britain island arc, Papua New GuineaContributions to Mineralogy and Petrology, 113
J. Davies, D. Stevenson (1992)
Physical model of source region of subduction zone volcanicsJournal of Geophysical Research, 97
J. Davidson (1987)
Crustal contamination versus subduction zone enrichment: Examples from the Lesser Antilles and implications for mantle source compositions of island arc volcanic rocksGeochimica et Cosmochimica Acta, 51
J. Woodhead, S. Eggins, J. Gamble (1993)
High field strength and transition element systematics in island arc and back-arc basin basalts: Evidence for multi-phase melt extraction and a depleted mantle wedgeEarth and Planetary Science Letters, 114
L. Briqueu, J. Lancelot (1983)
Sr isotopes and K, Rb, Sr balance in sediments and igneous rocks from the subducted plate of the Vanuatu (New Hebrides) active marginGeochimica et Cosmochimica Acta, 47
J. Davies, M. Bickle (1991)
A physical model for the volume and composition of melt produced by hydrous fluxing above subduction zonesPhilosophical Transactions of the Royal Society of London. Series A: Physical and Engineering Sciences, 335
Y. Tatsumi, M. Sakuyama, H. Fukuyama, I. Kushiro (1983)
Generation of arc basalt magmas and thermal structure of the mantle wedge in subduction zonesJournal of Geophysical Research, 88
J. Gill, J. Morris, R. Johnson (1993)
Timescale for producing the geochemical signature of island arc magmas: U-Th-Po and Be-B systematics in recent Papua New Guinea lavasGeochimica et Cosmochimica Acta, 57
L. Brown, J. Klein, R. Middleton, I. Sacks, F. Tera (1982)
10Be in island-arc volcanoes and implications for subductionNature, 299
P. Lin, R. Stern, J. Morris, S. Bloomer (1990)
Nd- and Sr-isotopic compositions of lavas from the northern Mariana and southern Volcano arcs: implications for the origin of island arc meltsContributions to Mineralogy and Petrology, 105
D. Othman, W. White, J. Patchett (1989)
The geochemistry of marine sediments, island arc magma genesis, and crust-mantle recyclingEarth and Planetary Science Letters, 94
R. Kay (1978)
Aleutian magnesian andesites: Melts from subducted Pacific ocean crustJournal of Volcanology and Geothermal Research, 4
O. Navon, E. Stolper (1987)
Geochemical Consequences of Melt Percolation: The Upper Mantle as a Chromatographic ColumnThe Journal of Geology, 95
G. Rogers, C. Hawkesworth (1985)
A geochemical traverse across the North Chilean Andes: evidence for crust generation from the mantle wedgeEarth and Planetary Science Letters, 91
J. Brenan, E. Watson (1991)
Partitioning of trace elements between olivine and aqueous fluids at highP-T conditions: implications for the effect of fluid composition on trace-element transportEarth and Planetary Science Letters, 107
I. Parkinson, J. Pearce, M. Thirlwall, K. Johnson, G. Ingram (1992)
Trace element geochemistry of peridotites from the Izu-Bonin-Mariana Forearc, Leg 125
S. Newman, S. Laan (1992)
8. VOLATILE CONTENTS OF IZU-BONIN FOREARC VOLCANIC GLASSES1
J. Pearce, S. Laan, R. Arculus, B. Murton, T. Ishii, D. Peate, I. Parkinson (1992)
Boninite and Harzburgite from Leg 125 (Bonin-Mariana Forearc): A Case Study of Magma Genesis during the Initial Stages of Subduction
M. Thirlwall, T. Smith, A. Graham, N. Theodorou, P. Hollings, J. Davidson, R. Arculus (1994)
High Field Strength Element Anomalies in Arc Lavas: Source or Process?Journal of Petrology, 35
E. Stolper, S. Newman (1994)
The role of water in the petrogenesis of Mariana trough magmasEarth and Planetary Science Letters, 121
Daniel Miller, C. Langmuir, S. Goldstein, Andrew Franks (1992)
The importance of parental magma composition to calc‐alkaline and tholeiitic evolution: Evidence from Umnak Island in the AleutiansJournal of Geophysical Research, 97
S. Peacock, T. Rushmer, A. Thompson (1994)
Partial melting of subducting oceanic crustEarth and Planetary Science Letters, 121
A. Saunders, J. Tarney, S. Weaver (1980)
Transverse geochemical variations across the Antarctic Peninsula: Implications for the genesis of calc-alkaline magmas, 46
Marc Defant, R. Maury, E. Ripley, M. Feigenson, D. Jacques (1991)
An Example of Island-Arc Petrogenesis: Geochemistry and Petrology of the Southern Luzon Arc, PhilippinesJournal of Petrology, 32
M. Spiegelman, D. McKenzie (1987)
Simple 2-D models for melt extraction at mid-ocean ridges and island arcsEarth and Planetary Science Letters, 83
C. Stern, F. Frey, K. Futa, R. Zartman, Zi-cheng Peng, T. Kyser (1990)
Trace-element and Sr, Nd, Pb, and O isotopic composition of Pliocene and Quaternary alkali basalts of the Patagonian Plateau lavas of southernmost South AmericaContributions to Mineralogy and Petrology, 104
P. Wyllie (1983)
Experimental and thermal constraints on the deep-seated parentage of some granitoid magmas in subduction zones
D. Green (1973)
Contrasted melting relations in a pyrolite upper mantle under mid-oceanic ridge, stable crust and island arc environmentsTectonophysics, 17
A. Jaques, David Green (1980)
Anhydrous melting of peridotite at 0–15 Kb pressure and the genesis of tholeiitic basaltsContributions to Mineralogy and Petrology, 73
L. Briqueu, C. Laporte, A. Crawford, T. Hasenaka, P. Baker, M. Coltorti (1994)
20. TEMPORAL MAGMATIC EVOLUTION OF THE AOBA BASIN, CENTRAL NEW HEBRIDES ISLAND ARC: PB, SR, AND ND ISOTOPIC EVIDENCE FOR THE COEXISTENCE OF TWO MANTLE COMPONENTS BENEATH THE ARC1, 134
M. Condomines, O. Sigmarsson (1993)
Why are so many arc magmas close to 238U-230Th radioactive equilibrium?Geochimica et Cosmochimica Acta, 57
Y. Tatsumi, Mitsuhiro Murasaki, E. Arsadi, S. Nonda (1991)
Geochemistry of Quaternary lavas from NE Sulawesi: transfer of subduction components into the mantle wedgeContributions to Mineralogy and Petrology, 107
R. Arculus (1991)
Fuji and Hakone., 7
Volcanic arc magmas can be defined tectonically as magmas erupting from volcanic edifices above subducting oceanic lithosphere. They form a coherent magma type, characterized compositionally by their enrichment in large ion lithophile (LlL) elements relative to high field strength (HFS) elements. In terms of process, the predominant view is that the vast majority of volcanic arc magmas originate by melting of the underlying mantle wedge, which contains a component of aqueous fluid and/or melt derived from the subducting plate. Recently, opinions have converged over the key aspects of the physical model for magma generation above subduction zones (Davies & Stevenson 1992), namely: that the mantle wedge experiences subduction-induced corner flow (e.g. Spiegelman & MacKenzie 1987); 2. that the subduction component reaches the fusible part of the mantle wedge by the three-stage process of (i) metasomatism of mantle lithosphere, fol lowed by (ii) aqueous fluid release due to breakdown of hydrous minerals at depth (e.g. Wyllie 1983, Tatsumi et al 1983) and (iii) aqueous fluid migra tion, followed by hydrous melt migration, to the site of melting; 0084-6597/95/0515-0251$05.00 251 PEARCE & PEATE 3. that slab-induced flow may be locally reversed beneath the arc itself, allowing mantle decompression to contribute
Annual Review of Earth and Planetary Sciences – Annual Reviews
Published: May 1, 1995
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