Inferring Earth’s discontinuous chemical layering from the 660-kilometer boundary topography

Inferring blocked mantle convection The boundaries between rocks with different physical properties in Earth's interior come from either a change in crystal structure or a change in chemical composition. Wu et al. examined the roughness of the boundary between Earth's upper and lower mantle, thought to form from a change in mineral structure (see the Perspective by Houser). To their surprise, in some locations, the boundary has small-scale roughness that requires some chemical difference above and below the boundary. This observation provides evidence of partially blocked mantle circulation that leads to some chemical differences between the upper and lower mantle. Science, this issue p. 736; see also p. 696 A rough boundary between Earth’s upper and lower mantle suggests partially blocked mantle circulation. Topography, or depth variation, of certain interfaces in the solid Earth can provide important insights into the dynamics of our planet interior. Although the intermediate- and long-range topographic variation of the 660-kilometer boundary between Earth’s upper and lower mantle is well studied, small-scale measurements are far more challenging. We found a surprising amount of topography at short length scale along the 660-kilometer boundary in certain regions using scattered P'P' seismic waves. Our observations required chemical layering in regions with high short-scale roughness. By contrast, we did not see such small-scale topography along the 410-kilometer boundary in the upper mantle. Our findings support the concept of partially blocked or imperfect circulation between the upper and lower mantle.

[1]  K. Sigloch,et al.  SubMachine: Web‐Based Tools for Exploring Seismic Tomography and Other Models of Earth's Deep Interior , 2018, Geochemistry, geophysics, geosystems : G(3).

[2]  E. Garnero,et al.  Dynamical links between small- and large-scale mantle heterogeneity: Seismological evidence , 2018 .

[3]  K. Hirose,et al.  Persistence of strong silica-enriched domains in the Earth’s lower mantle , 2016, 1803.08026.

[4]  C. Houser Global seismic data reveal little water in the mantle transition zone , 2016 .

[5]  N. Schmerr,et al.  Compositional mantle layering revealed by slab stagnation at ~1000-km depth , 2015, Science Advances.

[6]  T. Irifune,et al.  Phase Transitions and Mineralogy of the Lower Mantle , 2015 .

[7]  J. Irving,et al.  Using PKiKP coda to study heterogeneity in the top layer of the inner core's western hemisphere , 2014 .

[8]  S. Ni,et al.  Constraining the short scale core–mantle boundary topography beneath Kenai Peninsula (Alaska) with amplitudes of core-reflected PcP wave , 2014 .

[9]  H. Kanamori,et al.  Rupture complexity of the 1994 Bolivia and 2013 Sea of Okhotsk deep earthquakes , 2014 .

[10]  A. Deuss,et al.  Reconciling PP and P′P′ precursor observations of a complex 660 km seismic discontinuity , 2013 .

[11]  Y. Fukao,et al.  Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity , 2012 .

[12]  M. Kinoshita,et al.  Stress state estimation by geophysical logs in NanTroSEIZE Expedition 319‐Site C0009, Kumano Basin, southwest Japan , 2012 .

[13]  Michael Fehler,et al.  Seismic Wave Propagation and Scattering in the Heterogeneous Earth , 2012 .

[14]  Y. Ohishi,et al.  A perovskitic lower mantle inferred from high-pressure, high-temperature sound velocity data , 2012, Nature.

[15]  Takuto Maeda,et al.  Seismic Wave Propagation and Scattering in the Heterogeneous Earth : Second Edition , 2012 .

[16]  P. Shearer,et al.  Scattered P′P′ Waves Observed at Short Distances , 2011 .

[17]  Lapo Boschi,et al.  GyPSuM: A joint tomographic model of mantle density and seismic wave speeds , 2010 .

[18]  Q. Williams,et al.  Reconciling Pacific 410 and 660 km discontinuity topography, transition zone shear velocity patterns, and mantle phase transitions , 2010 .

[19]  C. Thomas,et al.  Improving Seismic Resolution Through Array Processing Techniques , 2009 .

[20]  D. Turcotte Fractals in geology and geophysics , 2009, Encyclopedia of Complexity and Systems Science.

[21]  P. Shearer,et al.  Shear and compressional velocity models of the mantle from cluster analysis of long‐period waveforms , 2008 .

[22]  B. Romanowicz,et al.  Deep Earth Structure: Q of the Earth from Crust to Core , 2007 .

[23]  P. Shearer Deep Earth Structure: Seismic Scattering in the Deep Earth , 2007 .

[24]  K. Chambers,et al.  The Nature of the 660-Kilometer Discontinuity in Earth's Mantle from Global Seismic Observations of PP Precursors , 2006, Science.

[25]  K. Koper,et al.  Observations of PKiKP/PcP amplitude ratios and implications for Earth structure at the boundaries of the liquid core , 2004 .

[26]  T. Yoshino,et al.  Olivine‐wadsleyite transition in the system (Mg,Fe)2SiO4 , 2004 .

[27]  P. Bird An updated digital model of plate boundaries , 2003 .

[28]  R. Hilst,et al.  Core mantle boundary topography from short period PcP, PKP, and PKKP data , 2003 .

[29]  M. Weber,et al.  The upper mantle transition zone discontinuities in the Pacific as determined by short-period array data , 2002 .

[30]  Sebastian Rost,et al.  ARRAY SEISMOLOGY: METHODS AND APPLICATIONS , 2002 .

[31]  D. Komatitsch,et al.  Introduction to the spectral element method for three-dimensional seismic wave propagation , 1999 .

[32]  Flanagan,et al.  Seismic Velocity and Density Jumps Across the 410- and 660-Kilometer Discontinuities. , 1999, Science.

[33]  K. Creager,et al.  Topography of the 660-km seismic discontinuity beneath Izu-Bonin : Implications for tectonic history and slab deformation , 1998 .

[34]  D. Komatitsch,et al.  The spectral element method: An efficient tool to simulate the seismic response of 2D and 3D geological structures , 1998, Bulletin of the Seismological Society of America.

[35]  P. Shearer,et al.  Global mapping of topography on transition zone velocity discontinuities by stacking SS precursors , 1998 .

[36]  P. Shearer,et al.  Observations of PKKP Precursors Used to Estimate Small-Scale Topography on the Core-Mantle Boundary , 1997 .

[37]  G. Helffrich,et al.  Topography of the “410” and “660” km seismic discontinuities in the Izu‐Bonin Subduction Zone , 1997 .

[38]  P. Shearer,et al.  Seismic evidence for small-scale heterogeneity throughout the Earth's mantle , 1997, Nature.

[39]  E. R. Engdahl,et al.  Evidence for deep mantle circulation from global tomography , 1997, Nature.

[40]  A. Hofmann,et al.  Mantle geochemistry: the message from oceanic volcanism , 1997, Nature.

[41]  R. Kind,et al.  The Nature of the 660-Kilometer Upper-Mantle Seismic Discontinuity from Precursors to the PP Phase , 1996, Science.

[42]  B. Romanowicz A global tomographic model of shear attenuation in the upper mantle , 1995 .

[43]  S. Myers,et al.  Rupture Characteristics of the Deep Bolivian Earthquake of 9 June 1994 and the Mechanism of Deep-Focus Earthquakes , 1995, Science.

[44]  A. E. Ringwood,et al.  Role of the transition zone and 660 km discontinuity in mantle dynamics , 1994 .

[45]  P. Shearer Global mapping of upper mantle reflectors from long-period SS precursors , 1993 .

[46]  P. Shearer,et al.  Seismic constraints on mantle flow and topography of the 660-km discontinuity: evidence for whole-mantle convection , 1993, Nature.

[47]  J. Vidale,et al.  Sharpness of upper-mantle discontinuities determined from high-frequency reflections , 1993, Nature.

[48]  Xiaodong Song,et al.  Velocity structure near the inner core boundary from waveform modeling , 1992 .

[49]  P. Shearer,et al.  Global mapping of topography on the 660-km discontinuity , 1992, Nature.

[50]  Alexandra Navrotsky,et al.  Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application , 1989 .

[51]  D. L. Anderson,et al.  Seismic velocities in mantle minerals and the mineralogy of the upper mantle , 1989 .

[52]  S. Flatté,et al.  Inhomogeneities near the core‐mantle boundary inferred from short‐period scattered PKP waves recorded at the Global Digital Seismograph Network , 1988 .

[53]  D. J. Doornbos Multiple scattering by topographic relief with application to the core-mantle boundary , 1988 .

[54]  M. Kurz,et al.  Constraints on evolution of Earth's mantle from rare gas systematics , 1983, Nature.

[55]  D. L. Anderson,et al.  Preliminary reference earth model , 1981 .

[56]  Don L. Anderson,et al.  The upper mantle transition region - Eclogite , 1979 .

[57]  R. Sayles,et al.  Surface topography as a nonstationary random process , 1978, Nature.

[58]  G. Buchbinder A velocity structure of the Earth's core , 1971, Bulletin of the Seismological Society of America.

[59]  M N Shaffner THE ELEVENTH ANNUAL FIELD CONFERENCE OF PENNSYLVANIA GEOLOGISTS. , 1941, Science.