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T. Elliott, T. Plank, A. Zindler, W. White, B. Bourdon (1997)
Element transport from slab to volcanic front at the Mariana arcJournal of Geophysical Research, 102
R. Stern (2004)
Subduction initiation: spontaneous and inducedEarth and Planetary Science Letters, 226
R. Hickey‐Vargas, M. Reagan (1987)
Temporal variation of isotope and rare earth element abundances in volcanic rocks from Guam: implications for the evolution of the Mariana ArcContributions to Mineralogy and Petrology, 97
C. Münker, S. Weyer, E. Scherer, K. Mezger (2001)
Separation of high field strength elements (Nb, Ta, Zr, Hf) and Lu from rock samples for MC‐ICPMS measurementsGeochemistry, 2
T. Plank, J. Ludden (1992)
Geochemistry of Sediments in the Argo Abyssal Plain at Site 765: A Continental Margin Reference Section for Sediment Recycling in Subduction Zones
M. Barth, T. Gluhak (2009)
Geochemistry and tectonic setting of mafic rocks from the Othris Ophiolite, GreeceContributions to Mineralogy and Petrology, 157
I. Parkinson, C. Hawkesworth, A. Cohen (1998)
Ancient mantle in a modern arc: osmium isotopes in izu-bonin-mariana forearc peridotitesScience, 281 5385
J. Karner, S. Sutton, J. Papike, C. Shearer, John Jones, M. Newville (2006)
Application of a new vanadium valence oxybarometer to basaltic glasses from the Earth, Moon, and MarsAmerican Mineralogist, 91
J. Pearce, M. Thirlwall, G. Ingram, B. Murton, R. Arculus, S. Laan (1992)
Isotopic evidence for the origin of boninites and related rocks drilled in the Izu-Bonin (Osagawara) Forearc, Leg 125, 125
J. Shervais, D. Kimbrough, P. Renne, B. Hanan, B. Murchey, Cameron Snow, Marchell Schuman, J. Beaman (2004)
Multi-Stage Origin of the Coast Range Ophiolite, California: Implications for the Life Cycle of Supra-Subduction Zone OphiolitesInternational Geology Review, 46
P. Kempton, J. Pearce, T. Barry, J. Fitton, C. Langmuir, D. Christie (2002)
Sr‐Nd‐Pb‐Hf Isotope Results from ODP Leg 187: Evidence for Mantle Dynamics of the Australian‐Antarctic Discordance and Origin of the Indian MORB SourceGeochemistry, 3
S. DeBari, B. Taylor, K. Spencer, K. Fujioka (1999)
A trapped Philippine Sea plate origin for MORB from the inner slope of the Izu^Bonin trenchEarth and Planetary Science Letters, 174
R. Somoza, C. Zaffarana (2008)
Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordilleraEarth and Planetary Science Letters, 271
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. Hickey‐Vargas (1998)
Origin of the Indian Ocean-type isotopic signature in basalts from Philippine Sea plate spreading centers: An assessment of local versus large-scale processesJournal of Geophysical Research, 103
(1975)
Boninite and related rocks of Chichijima
F. Martínez, P. Fryer, N. Becker (2000)
Geophysical characteristics of the southern Mariana Trough, 11°50'N-13°40'NJournal of Geophysical Research, 105
A. Ishiwatari, Y. Yanagida, Yibing Li, T. Ishii, S. Haraguchi, K. Koizumi, Y. Ichiyama, Masaru Umeka (2006)
Dredge petrology of the boninite‐ and adakite‐bearing Hahajima Seamount of the Ogasawara (Bonin) forearc: An ophiolite or a serpentinite seamount? §Island Arc, 15
Martinez Martinez, Fryer Fryer, Becker Becker (2000)
Geophysical characteristics of the southern Mariana TroughJ. Geophys. Res., 105
(1989)
Boninites and tholeiites from DSDP Site 458, Mariana Fore-arc
Y. Ohara, M. Reagan, S. Bloomer, P. Fryer, A. Fuji, R. Hickey‐Vargas, Hiroaki Imoto, T. Ishii, O. Ishizuka, J. Johnson, K. Michibayashi, J. Ribiero, H. Stern, S. Uehara (2008)
Studies of the Southern Izu-Bonin-Mariana (IBM) Forearc using Shinkai 6500: Watery Glimpses of an In Situ Forearc Ophiolite
R. Hickey‐Vargas (1991)
Isotope characteristics of submarine lavas from the Philippine Sea: implications for the origin of arc and basin magmas of the Philippine tectonic plateEarth and Planetary Science Letters, 107
S. Parman, T. Grove (2004)
Harzburgite melting with and without H2O: Experimental data and predictive modelingJournal of Geophysical Research, 109
R. Huene (1971)
Initial reports of the deep sea drilling project: National Science Foundation, Washington, D.C., 1969, 672 pp., U.S. $ 10.25Marine Geology, 10
I. Savov, R. Hickey‐Vargas, M. D’Antonio, J. Ryan, P. Spadea (2006)
Petrology and Geochemistry of West Philippine Basin Basalts and Early Palau–Kyushu Arc Volcanic Clasts from ODP Leg 195, Site 1201D: Implications for the Early History of the Izu–Bonin–Mariana ArcJournal of Petrology, 47
Y. Dilek, H. Furnes, M. Shallo (2007)
Suprasubduction zone ophiolite formation along the periphery of Mesozoic GondwanaGondwana Research, 11
C. Chauvel, J. Blichert‐Toft (2001)
A hafnium isotope and trace element perspective on melting of the depleted mantleEarth and Planetary Science Letters, 190
M. Reagan, B. Hanan, M. Heizler, B. Hartman, R. Hickey‐Vargas (2008)
Petrogenesis of Volcanic Rocks from Saipan and Rota, Mariana Islands, and Implications for the Evolution of Nascent Island ArcsJournal of Petrology, 49
Zohar Gvirtzman, R. Stern (2004)
Bathymetry of Mariana trench‐arc system and formation of the Challenger Deep as a consequence of weak plate couplingTectonics, 23
J. Gill (1981)
Orogenic Andesites and Plate Tectonics
C. Yuan, M. Sun, Mei‐Fu Zhou, W. Xiao, Hui Zhou (2005)
Geochemistry and petrogenesis of the Yishak Volcanic Sequence, Kudi ophiolite, West Kunlun (NW China): implications for the magmatic evolution in a subduction zone environmentContributions to Mineralogy and Petrology, 150
P. Fryer, N. Becker, B. Appelgate, F. Martínez, M. Edwards, G. Fryer (2003)
Why is the Challenger Deep so deepEarth and Planetary Science Letters, 211
D. Green (1973)
Experimental melting studies on a model upper mantle composition at high pressure under water-saturated and water-undersaturated conditionsEarth and Planetary Science Letters, 19
J. Shervais (2001)
Birth, death, and resurrection: The life cycle of suprasubduction zone ophiolitesGeochemistry, 2
J. Blichert‐Toft, F. Frey, F. Albarède (1999)
Hf isotope evidence for pelagic sediments in the source of hawaiian basaltsScience, 285 5429
Hanan Hanan, Blichert‐Toft Blichert‐Toft, Pyle Pyle, Christie Christie (2004)
Contrasting origins of the upper mantle MORB source revealed by Hf and Pb isotopes from the Australian‐Antarctic DiscordanceNature, 432
(2008)
Earliest Izu‐Bonin arc volcanism found on the submarine
(1982)
Petrology of the fore ‐ arc sites , Initial Rep
M. Rowe, A. Kent, R. Nielsen (2007)
Determination of sulfur speciation and oxidation state of olivine hosted melt inclusionsChemical Geology, 236
T. Falloon, L. Danyushevsky (2000)
Melting of Refractory Mantle at 1·5, 2 and 2·5 GPa under Anhydrous and H2O-undersaturated Conditions: Implications for the Petrogenesis of High-Ca Boninites and the Influence of Subduction Components on Mantle MeltingJournal of Petrology, 41
V. Bortolotti, G. Principi (2005)
Tethyan ophiolites and Pangea break‐upIsland Arc, 14
B. Hanan, J. Schilling (1989)
Easter microplate evolution: Pb isotope evidenceJournal of Geophysical Research, 94
Yinghuai Lu, A. Makishima, Eizo Nakamura (2007)
Purification of Hf in silicate materials using extraction chromatographic resin, and its application to precise determination of 176Hf/177Hf by MC-ICP-MS with 179Hf spikeJournal of Analytical Atomic Spectrometry, 22
Y. Dilek, H. Furnes, M. Shallo (2008)
Geochemistry of the Jurassic Mirdita Ophiolite (Albania) and the MORB to SSZ evolution of a marginal basin oceanic crustLithos, 100
D. Graham, J. Blichert‐Toft, C. Russo, Kenneth Rubin, F. Albarède (2006)
Cryptic striations in the upper mantle revealed by hafnium isotopes in southeast Indian ridge basaltsNature, 440
R. Taylor, R. Nesbitt, Phillipe Vidal, R. Harmon, B. Auvray, I. Croudace (1994)
Mineralogy, Chemistry, and Genesis of the Boninite Series Volcanics, Chichijima, Bonin Islands, JapanJournal of Petrology, 35
(1989)
Petrogenesis of boninitic lavas from the Limassol Forrest Complex, in Boninites and Related Rocks, edited by A
C. Warren, R. Parrish, D. Waters, M. Searle (2005)
Dating the geologic history of Oman’s Semail ophiolite: insights from U-Pb geochronologyContributions to Mineralogy and Petrology, 150
R. Hickey, F. Frey (1982)
Geochemical characteristics of boninite series volcanics: implications for their sourceGeochimica et Cosmochimica Acta, 46
Meijer Meijer, Anthony Anthony, Reagan Reagan (1982)
Petrology of the fore‐arc sitesInitial Rep. Deep Sea Drill. Proj., 60
R. Stern, S. Bloomer (1992)
Subduction zone infancy: Examples from the Eocene Izu-Bonin-Mariana and Jurassic California arcsGeological Society of America Bulletin, 104
(1980)
Primitive arc volcanism and a boninite series ; example from western Pacific Island arcs , in The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands , Geophys
W. Sharp, D. Clague (2006)
50-Ma Initiation of Hawaiian-Emperor Bend Records Major Change in Pacific Plate MotionScience, 313
J. Shervais (1982)
Ti-V plots and the petrogenesis of modern and ophiolitic lavasEarth and Planetary Science Letters, 59
D. Hussong, S. Uyeda (1982)
Initial Reports of the Deep Sea Drilling Project, 60
S. Umino (1985)
VOLCANIC GEOLOGY OF CHICHIJIMA, THE BONIN ISLANDS (OGASAWARA ISLANDS)Journal of the Geological Society of Japan, 91
D. Johnson, P. Hooper, R. Conrey (1999)
XRF Analysis of Rocks and Minerals for Major and Trace Elements on a Single Low Dilution Li-tetraborate Fused Bead
J. Woodhead, J. Hergt, J. Davidson, S. Eggins (2001)
Hafnium isotope evidence for ‘conservative’ element mobility during subduction zone processesEarth and Planetary Science Letters, 192
J. Pearce, P. Kempton, G. Nowell, S. Noble (1999)
Hf-Nd Element and Isotope Perspective on the Nature and Provenance of Mantle and Subduction Components in Western Pacific Arc-Basin SystemsJournal of Petrology, 40
MICHAELA. Cosca, R. Arculus, J. Pearce, John Mitchell (1998)
40Ar/ 39Ar and K–Ar geochronological age constraints for the inception and early evolution of the Izu–Bonin – Mariana arc systemIsland Arc, 7
D. Ulfbeck, J. Baker, T. Waight, E. Krogstad (2003)
Rapid sample digestion by fusion and chemical separation of Hf for isotopic analysis by MC-ICPMS.Talanta, 59 2
T. Ishikawa, K. Nagaishi, S. Umino (2002)
Boninitic volcanism in the Oman ophiolite: Implications for thermal condition during transition from spreading ridge to arcGeology, 30
J. Blichert‐Toft, C. Chauvel, F. Albarède (1997)
Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sector-multiple collector ICP-MSContributions to Mineralogy and Petrology, 127
Kuroda Kuroda, Shiraki Shiraki (1975)
Boninite and related rocks of Chichijima, Bonin Islands, JapanRep. Faculty Sci. Shizuoka Univ., 10
Hf/ 177 Hf by MC-ICP-MS with 179 Hf spike
M. Komatsu (1980)
Clinoenstatite in volcanic rocks from the Bonin IslandsContributions to Mineralogy and Petrology, 74
Cin-Ty Lee, W. Leeman, D. Canil, Z. Li (2005)
Similar V/Sc Systematics in MORB and Arc Basalts: Implications for the Oxygen Fugacities of their Mantle Source RegionsJournal of Petrology, 46
H. Staudigel, Kye‐Hun Park, M. Pringle, J. Rubenstone, Walter Smith, A. Zindler (1991)
The longevity of the South Pacific isotopic and thermal anomalyEarth and Planetary Science Letters, 102
C. Hall, M. Gurnis, M. Sdrolias, L. Lavier, R. Müller (2003)
Catastrophic initiation of subduction following forced convergence across fracture zonesEarth and Planetary Science Letters, 212
O. Ishizuka, J. Kimura, Y. Li, R. Stern, M. Reagan, R. Taylor, Y. Ohara, S. Bloomer, T. Ishii, U. Hargrove, S. Haraguchi (2006)
Early stages in the evolution of Izu–Bonin arc volcanism: new age, chemical, and isotopic constraintsEarth and Planetary Science Letters, 250
W. White, F. Albarède, P. Télouk (2000)
High-precision analysis of Pb isotope ratios by multi-collector ICP-MSChemical Geology, 167
M. Portnyagin, L. Danyushevsky, Vadim Kamenetsky (1997)
Coexistence of two distinct mantle sources during formation of ophiolites: a case study of primitive pillow-lavas from the lowest part of the volcanic section of the Troodos Ophiolite, CyprusContributions to Mineralogy and Petrology, 128
A. Meijer (1976)
Pb and Sr isotopic data bearing on the origin of volcanic rocks from the Mariana island-arc systemGeological Society of America Bulletin, 87
R. Taylor, R. Nesbitt (1994)
Arc volcanism in an extensional regime at the initiation of subduction: a geochemical study of Hahajima, Bonin Islands, JapanGeological Society, London, Special Publications, 81
B. Hanan, J. Blichert‐Toft, D. Pyle, D. Christie (2004)
Contrasting origins of the upper mantle revealed by hafnium and lead isotopes from the Southeast Indian RidgeNature, 432
Shen-su Sun, W. McDonough (1989)
Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processesGeological Society, London, Special Publications, 42
M. Reagan, A. Meijer (1984)
Geology and geochemistry of early arc-volcanic rocks from GuamGeological Society of America Bulletin, 95
(2009)
FORE‐ARC BASALTS AND SUBDUCTION INITIATION 10.1029/2009GC002871
A. Volpe, J. Macdougall, G. Lugmair, J. Hawkins, P. Lonsdale (1990)
Fine-scale isotopic variation in Mariana Trough basalts: evidence for heterogeneity and a recycled component in backarc basin mantleEarth and Planetary Science Letters, 100
S. Bloomer, J. Hawkins (1987)
Petrology and geochemistry of boninite series volcanic rocks from the Mariana trenchContributions to Mineralogy and Petrology, 97
J. Whittaker, R. Müller, G. Leitchenkov, H. Stagg, M. Sdrolias, C. Gaina, A. Goncharov (2007)
Major Australian-Antarctic Plate Reorganization at Hawaiian-Emperor Bend TimeScience, 318
B. Storey (1995)
The role of mantle plumes in continental breakup: case histories from GondwanalandNature, 377
O. Ishizuka, M. Yuasa, R. Taylor, I. Sakamoto (2007)
Two contrasting magmatic types coexist after the cessation of back-arc spreadingChemical Geology, 266
M. Flower, R. Russo, K. Tamaki, N. Hoàng (2001)
Mantle contamination and the Izu-Bonin-Mariana (IBM) 'high-tide mark': evidence for mantle extrusion caused by Tethyan closureTectonophysics, 333
Y. Dilek, H. Furnes (2009)
Structure and geochemistry of Tethyan ophiolites and their petrogenesis in subduction rollback systemsLithos, 113
Katherine Kelley, T. Plank, J. Ludden, H. Staudigel (2003)
Composition of altered oceanic crust at ODP Sites 801 and 1149Geochemistry, 4
S. Bloomer (1983)
Distribution and origin of igneous rocks from the landward slopes of the Mariana Trench: Implications for its structure and evolutionJournal of Geophysical Research, 88
Ishizuka Ishizuka, Yuasa Yuasa, Sakamoto Sakamoto, Kanayama Kanayama, Taylor Taylor, Umino Umino, Tani Tani, Ohara Ohara (2008)
Earliest Izu‐Bonin arc volcanism found on the submarine Bonin RidgeEos Trans. AGU, 89
Recent diving with the JAMSTEC Shinkai 6500 manned submersible in the Mariana fore arc southeast of Guam has discovered that MORB‐like tholeiitic basalts crop out over large areas. These “fore‐arc basalts” (FAB) underlie boninites and overlie diabasic and gabbroic rocks. Potential origins include eruption at a spreading center before subduction began or eruption during near‐trench spreading after subduction began. FAB trace element patterns are similar to those of MORB and most Izu‐Bonin‐Mariana (IBM) back‐arc lavas. However, Ti/V and Yb/V ratios are lower in FAB reflecting a stronger prior depletion of their mantle source compared to the source of basalts from mid‐ocean ridges and back‐arc basins. Some FAB also have higher concentrations of fluid‐soluble elements than do spreading center lavas. Thus, the most likely origin of FAB is that they were the first lavas to erupt when the Pacific Plate began sinking beneath the Philippine Plate at about 51 Ma. The magmas were generated by mantle decompression during near‐trench spreading with little or no mass transfer from the subducting plate. Boninites were generated later when the residual, highly depleted mantle melted at shallow levels after fluxing by a water‐rich fluid derived from the sinking Pacific Plate. This magmatic stratigraphy of FAB overlain by transitional lavas and boninites is similar to that found in many ophiolites, suggesting that ophiolitic assemblages might commonly originate from near‐trench volcanism caused by subduction initiation. Indeed, the widely dispersed Jurassic and Cretaceous Tethyan ophiolites could represent two such significant subduction initiation events.
Geochemistry, Geophysics, Geosystems – Wiley
Published: Mar 1, 2010
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