Estimate of the Rigidity of Eclogite in the Lower Mantle From Waveform Modeling of Broadband S‐to‐P Wave Conversions
dc.contributor.author | Haugland, Samuel M. | |
dc.contributor.author | Ritsema, Jeroen | |
dc.contributor.author | Kaneshima, Satoshi | |
dc.contributor.author | Thorne, Michael S. | |
dc.date.accessioned | 2018-02-05T16:27:35Z | |
dc.date.available | 2019-01-07T18:34:39Z | en |
dc.date.issued | 2017-12-16 | |
dc.identifier.citation | Haugland, Samuel M.; Ritsema, Jeroen; Kaneshima, Satoshi; Thorne, Michael S. (2017). "Estimate of the Rigidity of Eclogite in the Lower Mantle From Waveform Modeling of Broadband S‐to‐P Wave Conversions." Geophysical Research Letters 44(23): 11,778-11,784. | |
dc.identifier.issn | 0094-8276 | |
dc.identifier.issn | 1944-8007 | |
dc.identifier.uri | https://hdl.handle.net/2027.42/141104 | |
dc.description.abstract | Broadband USArray recordings of the 21 July 2007 western Brazil earthquake (Mw=6.0; depth = 633 km) include high‐amplitude signals about 40 s, 75 s, and 100 s after the P wave arrival. They are consistent with S wave to P wave conversions in the mantle beneath northwestern South America. The signal at 100 s, denoted as S1750P, has the highest amplitude and is formed at 1,750 km depth based on slant‐stacking and semblance analysis. Waveform modeling using axisymmetric, finite difference synthetics indicates that S1750P is generated by a 10 km thick heterogeneity, presumably a fragment of subducted mid‐ocean ridge basalt in the lower mantle. The negative polarity of S1750P is a robust observation and constrains the shear velocity anomaly δVS of the heterogeneity to be negative. The amplitude of S1750P indicates that δVS is in the range from −1.6% to −12.4%. The large uncertainty in δVS is due to the large variability in the recorded S1750P amplitude and simplifications in the modeling of S1750P waveforms. The lower end of our estimate for δVS is consistent with ab initio calculations by Tsuchiya (2011), who estimated that δVS of eclogite at lower mantle pressure is between 0 and −2% due to shear softening from the poststishovite phase transition.Key PointsBroadband recordings of S‐P conversions allow for constraining compositional properties of deep Earth materialsStishovite is present in subducted eclogite and contributes to shear velocity softeningFragments of subducted oceanic crust are entrained in mantle flow and can be preserved at depths approaching 2,000 km | |
dc.publisher | Elsevier | |
dc.publisher | Wiley Periodicals, Inc. | |
dc.subject.other | oceanic crust | |
dc.subject.other | seismology | |
dc.subject.other | eclogite | |
dc.subject.other | stishovite | |
dc.subject.other | subduction | |
dc.subject.other | S‐P conversion | |
dc.title | Estimate of the Rigidity of Eclogite in the Lower Mantle From Waveform Modeling of Broadband S‐to‐P Wave Conversions | |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | |
dc.subject.hlbsecondlevel | Geological Sciences | |
dc.subject.hlbtoplevel | Science | |
dc.description.peerreviewed | Peer Reviewed | |
dc.description.bitstreamurl | https://deepblue.lib.umich.edu/bitstream/2027.42/141104/1/grl56669_am.pdf | |
dc.description.bitstreamurl | https://deepblue.lib.umich.edu/bitstream/2027.42/141104/2/grl56642-sup-0002-supplementary.pdf | |
dc.description.bitstreamurl | https://deepblue.lib.umich.edu/bitstream/2027.42/141104/3/grl56642-sup-0001-supplementary.pdf | |
dc.description.bitstreamurl | https://deepblue.lib.umich.edu/bitstream/2027.42/141104/4/grl56669.pdf | |
dc.identifier.doi | 10.1002/2017GL075463 | |
dc.identifier.source | Geophysical Research Letters | |
dc.identifier.citedreference | Ono, S., Hirose, K., Murakami, M., & Isshiki, M. ( 2002 ). Post‐stishovite phase boundary in SiO 2 determined by in situ X‐ray observations. Earth and Planetary Science Letters, 197 ( 3 ), 187 – 192. https://doi.org/10.1016/S0012-821X(02)00479-X | |
dc.identifier.citedreference | Kaneshima, S., & Helffrich, G. ( 1999 ). Dipping low‐velocity layer in the mid‐lower mantle: Evidence for geochemical heterogeneity. Science, 283 ( 5409 ), 1888 – 1892. https://doi.org/10.1126/science.283.5409.1888 | |
dc.identifier.citedreference | Kaneshima, S., & Helffrich, G. ( 2003 ). Subparallel dipping heterogeneities in the mid‐lower mantle. Journal of Geophysical Research, 108 ( B5 ), 2272. https://doi.org/10.1029/2001JB001596 | |
dc.identifier.citedreference | Kaneshima, S., & Helffrich, G. ( 2010 ). Small scale heterogeneity in the mid‐lower mantle beneath the circum‐Pacific area. Physics of the Earth and Planetary Interiors, 183 ( 1 ), 91 – 103. https://doi.org/10.1016/j.pepi.2010.03.011 | |
dc.identifier.citedreference | Karki, B. B., Stixrude, L., & Crain, J. ( 1997 ). Ab initio elasticity of three high‐pressure polymorphs of silica. Geophysical Research Letters, 24 ( 24 ), 3269 – 3272. https://doi.org/10.1029/97GL53196 | |
dc.identifier.citedreference | Kawai, K., & Tsuchiya, T. ( 2012 ). First principles investigations on the elasticity and phase stability of grossular garnet. Journal of Geophysical Research, 117, B02202. https://doi.org/10.1029/2011JB008529 | |
dc.identifier.citedreference | Kawakatsu, H., & Niu, F. ( 1994 ). Seismic evidence for a 920‐km discontinuity in the mantle. Nature, 371 ( 6495 ), 301 – 305. https://doi.org/10.1038/371301a0 | |
dc.identifier.citedreference | Kudo, Y., Hirose, K., Murakami, M., Asahara, Y., Ozawa, H., Ohishi, Y., & Hirao, N. ( 2012 ). Sound velocity measurements of CaSiO 3 perovskite to 133 GPa and implications for lowermost mantle seismic anomalies. Earth and Planetary Science Letters, 349, 1 – 7. https://doi.org/10.1016/j.epsl.2012.06.040 | |
dc.identifier.citedreference | Lakshtanov, D. L., Sinogeikin, S. V., Litasov, K. D., Prakapenka, V. B., Hellwig, H., Wang, J., & Li, J. ( 2007 ). The post‐stishovite phase transition in hydrous alumina‐bearing SiO 2 in the lower mantle of the Earth. Proceedings of the National Academy of Sciences of the United States of America, 104 ( 34 ), 13,588 – 13,590. https://doi.org/10.1073/pnas.0706113104 | |
dc.identifier.citedreference | Li, J., & Yuen, D. A. ( 2014 ). Mid‐mantle heterogeneities associated with Izanagi plate: Implications for regional mantle viscosity. Earth and Planetary Science Letters, 385, 137 – 144. https://doi.org/10.1016/j.epsl.2013.10.042 | |
dc.identifier.citedreference | Litasov, K., Ohtani, E., Suzuki, A., Kawazoe, T., & Funakoshi, K. ( 2004 ). Absence of density crossover between basalt and peridotite in the cold slabs passing through 660 km discontinuity. Geophysical Research Letters, 31, L24607. https://doi.org/10.1029/2004GL021306 | |
dc.identifier.citedreference | Niu, F. ( 2014 ). Distinct compositional thin layers at mid‐mantle depths beneath northeast China revealed by the USArray. Earth and Planetary Science Letters, 402, 305 – 312. https://doi.org/10.1016/j.epsl.2013.02.015 | |
dc.identifier.citedreference | Niu, F., & Kawakatsu, H. ( 1997 ). Depth variation of the mid‐mantle seismic discontinuity. Geophysical Research Letters, 24 ( 4 ), 429 – 432. https://doi.org/10.1029/97GL00216 | |
dc.identifier.citedreference | Nomura, R., Hirose, K., Sata, N., & Ohishi, Y. ( 2010 ). Precise determination of post‐stishovite phase transition boundary and implications for seismic heterogeneities in the mid‐lower mantle. Physics of the Earth and Planetary Interiors, 183 ( 1 ), 104 – 109. https://doi.org/10.1016/j.pepi.2010.08.004 | |
dc.identifier.citedreference | Ricolleau, A., Perrillat, J. P., Fiquet, G., Daniel, I., Matas, J., Addad, A., & Guignot, N. ( 2010 ). Phase relations and equation of state of a natural MORB: Implications for the density profile of subducted oceanic crust in the Earth’s lower mantle. Journal of Geophysical Research, 115, B08202. https://doi.org/10.1029/2009JB006709 | |
dc.identifier.citedreference | Ritsema, J., Deuss, A. A., Van Heijst, H. J., & Woodhouse, J. H. ( 2011 ). S40RTS: A degree‐40 shear‐velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal‐mode splitting function measurements. Geophysical Journal International, 184 ( 3 ), 1223 – 1236. https://doi.org/10.1111/j.1365-246X.2010.04884.x | |
dc.identifier.citedreference | Shearer, P. M. ( 2007 ). Deep Earth structure—Seismic scattering in the deep Earth, Treatise on Geophysics (pp. 695–729). Amsterdam: Elsevier. | |
dc.identifier.citedreference | Thorne, M. S., Zhang, Y., & Ritsema, J. ( 2013 ). Evaluation of 1‐D and 3‐D seismic models of the Pacific lower mantle with S, SKS, and SKKS traveltimes and amplitudes. Journal of Geophysical Research: Solid Earth, 118, 985 – 995. https://doi.org/10.1002/jgrb.50054 | |
dc.identifier.citedreference | Tsuchiya, T. ( 2011 ). Elasticity of subducted basaltic crust at the lower mantle pressures: Insights on the nature of deep mantle heterogeneity. Physics of the Earth and Planetary Interiors, 188 ( 3 ), 142 – 149. https://doi.org/10.1016/j.pepi.2011.06.018 | |
dc.identifier.citedreference | Tsuchiya, T., Caracas, R., & Tsuchiya, J. ( 2004 ). First principles determination of the phase boundaries of high‐pressure polymorphs of silica. Geophysical Research Letters, 31, L11610. http://doi.org/10.1029/2004GL019649 | |
dc.identifier.citedreference | Vanacore, E., Niu, F., & Kawakatsu, H. ( 2006 ). Observations of the mid‐mantle discontinuity beneath Indonesia from S to P converted waveforms. Geophysical Research Letters, 33, L04302. https://doi.org/10.1029/2005GL025106 | |
dc.identifier.citedreference | Vinnik, L., Niu, F., & Kawakatsu, H. ( 1998 ). Broadband converted phases from midmantle discontinuities. Earth, Planets and Space, 50 ( 11–12 ), 987 – 997. http://doi.org/10.1186/BF03352193 | |
dc.identifier.citedreference | Xu, W., Lithgow‐Bertelloni, C., Stixrude, L., & Ritsema, J. ( 2008 ). The effect of bulk composition and temperature on mantle seismic structure. Earth and Planetary Science Letters, 275 ( 1 ), 70 – 79. https://doi.org/10.1016/j.epsl.2008.08.012 | |
dc.identifier.citedreference | Yang, Z., & He, X. ( 2015 ). Oceanic crust in the mid‐mantle beneath west‐central Pacific subduction zones: Evidence from S to P converted waveforms. Geophysical Journal International, 203 ( 1 ), 541 – 547. https://doi.org/10.1093/gji/ggv314 | |
dc.identifier.citedreference | Bolfan‐Casanova, N., Andrault, D., Amiguet, E., & Guignot, N. ( 2009 ). Equation of state and post‐stishovite transformation of Al‐bearing silica up to 100 GPa and 3000 K. Physics of the Earth and Planetary Interiors, 174 ( 1 ), 70 – 77. https://doi.org/10.1016/j.pepi.2008.06.024 | |
dc.identifier.citedreference | Castle, J. C., & van der Hilst, R. D. ( 2003 ). Searching for seismic scattering off mantle interfaces between 800 km and 2000 km depth. Journal of Geophysical Research, 108 ( B2 ), 2095. https://doi.org/10.1029/2001JB000286 | |
dc.identifier.citedreference | Fukao, Y., Widiyantoro, S., & Obayashi, M. ( 2001 ). Stagnant slabs in the upper and lower mantle transition region. Reviews of Geophysics, 39 ( 3 ), 291 – 323. https://doi.org/10.1029/1999RG000068 | |
dc.identifier.citedreference | Grand, S. P., van der Hilst, R. D., & Widiyantoro, S. ( 1997 ). High resolution global tomography: A snapshot of convection in the Earth. Geological Society of America Today, 7 ( 4 ), 1 – 7. | |
dc.identifier.citedreference | Hirose, K., Fei, Y., Ma, Y., & Mao, H. K. ( 1999 ). The fate of subducted basaltic crust in the Earth’s lower mantle. Nature, 397 ( 6714 ), 53 – 56. https://doi.org/10.1038/16225 | |
dc.identifier.citedreference | Irifune, T., & Ringwood, A. E. ( 1987 ). Phase transformations in a harzburgite composition to 26 GPa: Implications for dynamical behaviour of the subducting slab. Earth and Planetary Science Letters, 86 ( 2–4 ), 365 – 376. https://doi.org/10.1016/0012-821X(87)90233-0 | |
dc.identifier.citedreference | Irifune, T., & Ringwood, A. E. ( 1993 ). Phase transformations in subducted oceanic crust and buoyancy relationships at depths of 600–800 km in the mantle. Earth and Planetary Science Letters, 117 ( 1–2 ), 101 – 110. https://doi.org/10.1016/0012-821X(93)90120-X | |
dc.identifier.citedreference | Irifune, T., & Tsuchiya, T. ( 2007 ). Mineralogy of the Earth–Phase transitions and mineralogy of the lower mantle. Treatise on Geophysics, 2, 33 – 62. https://doi.org/10.1029/2012JB009696 | |
dc.identifier.citedreference | Jahnke, G., Thorne, M. S., Cochard, A., & Igel, H. ( 2008 ). Global S H ‐wave propagation using a parallel axisymmetric spherical finite‐difference scheme: Application to whole mantle scattering. Geophysical Journal International, 173 ( 3 ), 815 – 826. https://doi.org/10.1111/j.1365-246X.2008.03744.x | |
dc.identifier.citedreference | Kaneshima, S. ( 2013 ). Lower mantle seismic scatterers below the subducting Tonga slab: Evidence for slab entrainment of transition zone materials. Physics of the Earth and Planetary Interiors, 222, 35 – 46. https://doi.org/10.1016/j.pepi. 2013.07.001 | |
dc.identifier.citedreference | Kaneshima, S. ( 2016 ). Seismic scatterers in the mid‐lower mantle. Physics of the Earth and Planetary Interiors, 257, 105 – 114. https://doi.org/10.1016/j.pepi.2016.05.004 | |
dc.identifier.citedreference | Kaneshima, S., & Helffrich, G. ( 1998 ). Detection of lower mantle scatterers northeast of the Marianna subduction zone using short‐period array data. Journal of Geophysical Research, 103 ( B3 ), 4825 – 4838. https://doi.org/10.1029/97JB02565 | |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
Files in this item
Remediation of Harmful Language
The University of Michigan Library aims to describe library materials in a way that respects the people and communities who create, use, and are represented in our collections. Report harmful or offensive language in catalog records, finding aids, or elsewhere in our collections anonymously through our metadata feedback form. More information at Remediation of Harmful Language.
Accessibility
If you are unable to use this file in its current format, please select the Contact Us link and we can modify it to make it more accessible to you.