A sporadic low‐velocity layer atop the western U.S. mantle transition zone and short‐wavelength variations in transition zone discontinuities
暂无分享,去创建一个
Kenneth G. Dueker | Brandon Schmandt | B. Schmandt | S. Hansen | K. Dueker | S. M. Hansen | John J. Jasbinsek | Zhongfei Zhang | J. Jasbinsek | Z. Zhang
[1] B. Wood. The Effect of H2O on the 410-Kilometer Seismic Discontinuity , 1995, Science.
[2] P. Mumby,et al. Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States , 2004 .
[3] K. Hirose,et al. Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications , 2004 .
[4] L. P. Vinnik,et al. Detection of waves converted from P to SV in the mantle , 1977 .
[5] E. Ohtani,et al. Stability of hydrous melt at the base of the Earth's upper mantle , 2006, Nature.
[6] J. A. Tyburczy,et al. Electromagnetic detection of a 410-km-deep melt layer in the southwestern United States , 2007, Nature.
[7] E. Humphreys,et al. Seismically imaged relict slab from the 55 Ma Siletzia accretion to the northwest United States , 2011 .
[8] Shijie Zhong,et al. Constraints on thermochemical convection of the mantle from plume heat flux, plume excess temperature, and upper mantle temperature , 2006 .
[9] Robert Tibshirani,et al. Bootstrap Methods for Standard Errors, Confidence Intervals, and Other Measures of Statistical Accuracy , 1986 .
[10] S. Poli,et al. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation , 1998 .
[11] T. Kikegawa,et al. The Phase Boundary Between α- and β-Mg2SiO4 Determined by in Situ X-ray Observation , 1994, Science.
[12] R. Hilst,et al. High resolution global tomography : a snapshot of convection in the Earth , 1997 .
[13] A. Hofmann,et al. Segregation of subducted oceanic crust in the convecting mantle , 1994 .
[14] M. Kumar,et al. Seismic signatures of detached lithospheric fragments in the mantle beneath eastern Himalaya and southern Tibet , 2009 .
[15] Toru Inoue,et al. Effect of water on melting phase relations and melt composition in the system Mg2SiO4MgSiO3H2O up to 15 GPa , 1994 .
[16] P. Shearer,et al. A global study of transition zone thickness using receiver functions , 2006 .
[17] V. Farra,et al. Subcratonic low‐velocity layer and flood basalts , 2001 .
[18] S. Ono,et al. Post-spinel transition in Mg2SiO4 determined by high P–T in situ X-ray diffractometry , 2003 .
[19] P. Tackley. Strong heterogeneity caused by deep mantle layering , 2002 .
[20] Michael G. Bostock,et al. Green's functions, source signatures, and the normalization of teleseismic wave fields , 2004 .
[21] S. Karato,et al. Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite , 2005, Nature.
[22] Akio Suzuki,et al. MELTING RELATIONS OF PERIDOTITE AND THE DENSITY CROSSOVER IN PLANETARY MANTLES , 1995 .
[23] N. Schmerr,et al. Upper Mantle Discontinuity Topography from Thermal and Chemical Heterogeneity , 2007, Science.
[24] R. Aster,et al. Upper mantle convection beneath the central Rio Grande rift imaged by P and S wave tomography , 2004 .
[25] R. Carlson,et al. Three‐dimensional seismic velocity structure of the northwestern United States , 2008 .
[26] M. Ravi Kumar,et al. Super‐deep low‐velocity layer beneath the Arabian plate , 2003 .
[27] H. Iwamori,et al. Stagnant slab, wet plumes and Cenozoic volcanism in East Asia , 2010 .
[28] S. Sipkin,et al. Seismic evidence for silicate melt atop the 410-km mantle discontinuity , 1994, Nature.
[29] C. J. McGrath,et al. Effect of exchange rate return on volatility spill-over across trading regions , 2012 .
[30] Peter M. Shearer,et al. Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity , 1990, Nature.
[31] Gary L. Pavlis,et al. Model Update December 2008: Upper Mantle Heterogeneity beneath North America from P-wave Travel Time Tomography with Global and USArray Transportable Array Data , 2009 .
[32] Cin-Ty A. Lee,et al. Possible density segregation of subducted oceanic lithosphere along a weak serpentinite layer and implications for compositional stratification of the Earth's mantle , 2007 .
[33] H. Iwamori. Degree of melting and source composition of Cenozoic basalts in southwest Japan: Evidence for mantle upwelling by flux melting , 1992 .
[34] D. Helmberger,et al. Fine structure of the 410‐km discontinuity , 1998 .
[35] S. Hansen,et al. P- and S-Wave Receiver Function Images of Crustal Imbrication beneath the Cheyenne Belt in Southeast Wyoming , 2009 .
[36] J. Revenaugh,et al. A Water‐Rich Transition Zone Beneath the Eastern United States and Gulf of Mexico from Multiple ScS Reverberations , 2013 .
[37] S. Karato,et al. Water distribution across the mantle transition zone and its implications for global material circulation , 2011 .
[38] E. Matzel,et al. Upper mantle seismic structure beneath eastern Mexico determined from P and S waveform inversion and its implications , 2006 .
[39] J. V. Smith,et al. Reduced sapphirine granulite xenoliths from the Lace Kimberlite, South Africa; implications for the deep structure of the Kaapvaal Craton , 1987 .
[40] D. Frost,et al. The effect of water on the 410‐km discontinuity: An experimental study , 2002 .
[41] D. Bercovici,et al. Stability of a compressible hydrous melt layer above the transition zone , 2009 .
[42] H. Keppler,et al. Water partitioning at 660 km depth and evidence for very low water solubility in magnesium silicate perovskite , 2003 .
[43] M. Bostock. Mantle stratigraphy and evolution of the Slave province , 1998 .
[44] F. Marone,et al. Seismic Evidence for Water Deep in Earth's Upper Mantle , 2003, Science.
[45] P. Shearer,et al. Constraining seismic velocity and density for the mantle transition zone with reflected and transmitted waveforms , 2006 .
[46] M. Bostock. Seismic waves converted from velocity gradient anomalies in the Earth’s upper mantle , 1999 .
[47] A. Deuss. Seismic observations of transition-zone discontinuities beneath hotspot locations , 2007 .
[48] Guust Nolet,et al. Tomographic imaging of subducted lithosphere below northwest Pacific island arcs , 1991, Nature.
[49] Yu Jeffrey Gu,et al. Global variability of transition zone thickness , 2002 .
[50] Matthias Hort,et al. Serpentine and the subduction zone water cycle , 2004 .
[51] H. Keppler,et al. Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 , 1996 .
[52] M. Richards,et al. The dynamics of Cenozoic and Mesozoic plate motions , 1998 .
[53] M. Hirschmann,et al. Melting in the Earth's deep upper mantle caused by carbon dioxide , 2006, Nature.
[54] Mei Xue,et al. Slab‐plume interaction beneath the Pacific Northwest , 2010 .
[55] F. Niu,et al. A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China , 2009 .
[56] T. Kondo,et al. Water transport into the deep mantle and formation of a hydrous transition zone , 2004 .
[57] Brandon Schmandt,et al. Complex subduction and small-scale convection revealed by body-wave tomography of the western United States upper mantle , 2010 .
[58] Deep seismic structure of the Kaapvaal craton , 1996 .
[59] McSween Hy,et al. Evidence for Life in a Martian Meteorite , 1997 .
[60] M. Hirschmann,et al. Storage capacity of H2O in nominally anhydrous minerals in the upper mantle , 2005 .
[61] K. Dueker,et al. Ubiquitous low‐velocity layer atop the 410‐km discontinuity in the northern Rocky Mountains , 2007 .
[62] 井上 徹. Effect of water on melting phase relations and melt composition in the system Mg[2]SiO[4]-MgSiO[3]-H[2]O up to 15 GPa , 1994 .
[63] Allan Cox,et al. Relative Motions Between Oceanic and Continental Plates in the Pacific Basin , 1986 .
[64] A. Sano,et al. Influence of Water on Major Phase Transitions in the Earth's Mantle , 2013 .
[65] Don L. Anderson,et al. Chemical stratification of the mantle , 1979 .
[66] Tianyu Zheng,et al. A complex 660 km discontinuity beneath northeast China , 2003 .
[67] P. Molnar,et al. Receiver functions in the western United States, with implications for upper mantle structure and dynamics , 2003 .
[68] K. Chambers,et al. The Nature of the 660-Kilometer Discontinuity in Earth's Mantle from Global Seismic Observations of PP Precursors , 2006, Science.
[69] M. Bostock,et al. A low‐velocity zone atop the transition zone in northwestern Canada , 2010 .
[70] D. Bercovici,et al. The Transition‐Zone Water Filter Model for Global Material Circulation: Where Do We Stand? , 2013 .
[71] V. Farra,et al. Low S velocity atop the 410-km discontinuity and mantle plumes , 2007 .
[72] D. Weidner,et al. Chemical‐ and Clapeyron‐induced buoyancy at the 660 km discontinuity , 1998 .
[73] A. Levander,et al. High‐resolution transition zone structures of the Gorda Slab beneath the western United States: Implication for deep water subduction , 2010 .
[74] D. Bercovici,et al. Whole-mantle convection and the transition-zone water filter , 2002, Nature.
[75] M. Hirschmann,et al. Petrologic Structure of a Hydrous 410 Km Discontinuity , 2013 .
[76] S. Hansen,et al. Characterizing the 410 km discontinuity low‐velocity layer beneath the LA RISTRA array in the North American Southwest , 2010 .
[77] É. Stutzmann,et al. Observations of S410p and S350p phases at seismograph stations in California , 2010 .
[78] A. Sano,et al. Wet subduction versus cold subduction , 2005 .
[79] Daniel E. McNamara,et al. Ambient Noise Levels in the Continental United States , 2004 .
[80] Guust Nolet,et al. Two-stage subduction history under North America inferred from multiple-frequency tomography , 2008 .
[81] Michael G. Bostock,et al. Spectral reconstruction of teleseismic P Green's functions , 2005 .
[82] G. Helffrich. Topography of the transition zone seismic discontinuities , 2000 .
[83] D. Bercovici,et al. Slab dehydration in the Earth's mantle transition zone , 2006 .
[84] B. Hacker. H 2 O subduction beyond arcs , 2008 .
[85] D. Helmberger,et al. P and S waveform modeling of continental sub-lithospheric detachment at the eastern edge of the Rio Grande Rift , 2007 .
[86] D. James,et al. Receiver function imaging of upper mantle complexity beneath the Pacific Northwest, United States , 2010 .
[87] N. Simmons,et al. Multiple seismic discontinuities near the base of the transition zone in the Earth's mantle , 2000, Nature.
[88] K. Hirose. Phase transitions in pyrolitic mantle around 670‐km depth: Implications for upwelling of plumes from the lower mantle , 2002 .
[89] T. Yoshino,et al. Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite , 2008, Nature.
[90] Guust Nolet,et al. Structure of North American mantle constrained by simultaneous inversion of multiple‐frequency SH, SS, and Love waves , 2011 .
[91] Bradford H. Hager,et al. Melt segregation from partially molten source regions: The importance of melt density and source region size , 1981 .
[92] D. Rubie. Solubility of water in the a , b and g phases of ( Mg , Fe ) 2 SiO 4 , 2022 .
[93] L. Elkins‐Tanton,et al. Vertical mantle flow associated with a lithospheric drip beneath the Great Basin , 2009 .
[94] F. Niu,et al. Complex Structure of Mantle Discontinuities at the Tip of the Subducting Slab beneath Northeast China -A Preliminary Investigation of Broadband Receiver Functions- , 1996 .
[95] J. Revenaugh,et al. Deep upper-mantle melting beneath the Tasman and Coral Seas detected with multiple ScS reverberations , 2007 .
[96] R. Aster,et al. Mantle structure beneath the western edge of the Colorado Plateau , 2008 .
[97] D. Fee,et al. Mantle transition zone topography and structure beneath the Yellowstone hotspot , 2004 .
[98] E. R. Engdahl,et al. Constraints on seismic velocities in the Earth from traveltimes , 1995 .
[99] J. Lawrence,et al. Correlation of seismic and petrologic thermometers suggests deep thermal anomalies beneath hotspots , 2007 .
[100] G. MacDonald. Composition and petrology of the earth's mantle , 1977 .
[101] Improved Green’s functions for passive-source structural studies , 2006 .
[102] Ramesh Desikan,et al. Response of mantle transition zone thickness to plume buoyancy flux , 2010 .
[103] D. Helmberger,et al. Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States , 2004, Nature.
[104] D. Bercovici,et al. On the dynamics of a hydrous melt layer above the transition zone , 2007 .
[105] S. Maruyama,et al. Petrogenetic grid in the system MgO-SiO2-H2O up to 30 GPa, 1600°C: Applications to hydrous peridotite subducting into the Earth's deep interior , 2004 .
[106] A. Ringwood. Composition and petrology of the earth's mantle , 1975 .
[107] B. Hacker. H2O subduction beyond arcs , 2008 .
[108] Thomas H. Jordan,et al. Mantle layering from ScS reverberations: 2. The transition zone , 1991 .
[109] B. Tauzin,et al. The mantle transition zone as seen by global Pds phases: No clear evidence for a thin transition zone beneath hotspots , 2008 .
[110] B. Tauzin,et al. Seismic evidence for a global low-velocity layer within the Earth/'s upper mantle , 2010 .
[111] C. Faccenna,et al. Subduction-triggered magmatic pulses: A new class of plumes? , 2010 .
[112] M. Brudzinski,et al. Seismic evidence of negligible water carried below 400-km depth in subducting lithosphere , 2010, Nature.
[113] T. Yoshino,et al. Olivine‐wadsleyite transition in the system (Mg,Fe)2SiO4 , 2004 .