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Titolo: Models of the mantle shear velocity and discontinuities in the pattern of lateral heterogeneities
Autore: Gu, YJ; Dziewonski, AM; Su, WJ; Ekstrom, G;
 Indirizzi:
 Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA Harvard Univ Cambridge MA USA 02138 lanetary Sci, Cambridge, MA 02138 USA
 Titolo Testata:
 JOURNAL OF GEOPHYSICAL RESEARCHSOLID EARTH
fascicolo: B6,
volume: 106,
anno: 2001,
pagine: 11169  11199
 SICI:
 01480227(20010610)106:B6<11169:MOTMSV>2.0.ZU;2Z
 Fonte:
 ISI
 Lingua:
 ENG
 Soggetto:
 TRANSITION ZONE; 3DIMENSIONAL STRUCTURE; NORTHWEST PACIFIC; SEISMIC EVIDENCE; WESTERN PACIFIC; EARTH STRUCTURE; ISLAND ARCS; CONVECTION; TOMOGRAPHY; INVERSION;
 Tipo documento:
 Article
 Natura:
 Periodico
 Settore Disciplinare:
 Physical, Chemical & Earth Sciences
 Citazioni:
 81
 Recensione:
 Indirizzi per estratti:
 Indirizzo: Gu, YJ Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA Harvard Univ Cambridge MA USA 02138 y Sci, Cambridge, MA 02138 USA



 Citazione:
 Y.J. Gu et al., "Models of the mantle shear velocity and discontinuities in the pattern of lateral heterogeneities", J GEO RSOL, 106(B6), 2001, pp. 1116911199
Abstract
Resolution of the pattern of largescale shear velocity variations above and below the known and postulated mantle discontinuities could provide constraints on the nature of mineral phase transitions, changes in composition,and the scale of mantle convection. To achieve good resolution across a full range of depths, we use a diversified data set consisting of body and mantle wave waveforms, travel times, and surface wave phase velocities. Our main focus is on the 670km discontinuity, long presumed to be an important barrier, or impediment, to whole mantle convection. Our data set has a relatively high radial resolution throughout the mantle; in the transition zoneand some 200 km below it, the long period waveforms, dominated by multiplesurface reflections, make a particularly important contribution. We use a local spline support to parameterize the model; this allows us to obtain a smooth model (twice differentiable) and simplifies calculation of the modeland its derivatives in applications such as threedimensional ray tracing. In one inversion we use a continuous radial representation throughout the mantle; in the other, a discontinuity is allowed across the 670km boundary. Both models suggest that the longwavelength anomalies of the transition zone and the mantle below 750 km are significantly different. Near 670 km these two models display notable differences in the peak amplitudes and lateral scales of major anomalies. The degree 2 spherical harmonic, which dominates the largescale shear velocities in the transition zone, is strongly attenuated at the top of the lower mantle where the power spectrum is essentially white. Resolution tests show that these results are robust, which suggests a possible reorganization of the flow between the upper and lower mantle. At other depths the power spectra of our models as a function of depthindicate a modest change near 400 km, where the dominating effect of degree 5 (shields) is replaced by degree: 2 (slabs). The power of the heterogeneity in at midmantle depths is low and nearly flat as a function of spherical harmonic degree up to l = 12, with no detectable change near 1000 km. The increase of the power in the lowermost mantle is rather gradual, not characteristic of a discontinuous change. Cross sections of our models at majorsubduction zones indicate that major downwelling of cold slab material mayoccur at some locations. On the other hand, there are numerous examples ofan abrupt change of the sign of the velocity anomalies across the 670km discontinuity.
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Documento generato il 10/07/20 alle ore 19:11:53