Topography of the 410-km discontinuity from PP and SS precursors

Topography of the 410-km discontinuity from PP and SS precursors

A number of previous studies have confirmed the global existence of a transition zone discontinuity at 410-km depth by aligning large numbers of long-period seismograms on a surface reflection phase before stacking. Discussion of SS and PP precursors from the 410-km discontinuity (termed P410P and S...

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Manylion Llyfryddiaeth
Prif Awduron:	Chambers, K, Woodhouse, J, Deuss, A
Fformat:	Journal article
Cyhoeddwyd:	2005

Eitemau Tebyg

Reflectivity of the 410-km discontinuity from PP and SS precursors
gan: Chambers, K, et al.
Cyhoeddwyd: (2005)

A systematic search for mantle discontinuities using SS-precursors
gan: Deuss, A, et al.
Cyhoeddwyd: (2002)

The nature of the 660-kilometer discontinuity in Earth's mantle from global seismic observations of PP precursors.
gan: Deuss, A, et al.
Cyhoeddwyd: (2006)

Ultra-low-velocity anomaly inside the Pacific Slab near the 410-km discontinuity
gan: Jiaqi Li, et al.
Cyhoeddwyd: (2023-05-01)

The nature of the Lehmann discontinuity from its seismological Clapeyron slopes
gan: Deuss, A, et al.
Cyhoeddwyd: (2004)

410 km discontinuity sharpness and the form of the olivine alpha-beta phase diagram: Resolution of apparent seismic contradictions
gan: Helffrich, G, et al.
Cyhoeddwyd: (1996)

Seismic observations of splitting of the mid-transition zone discontinuity in Earth's mantle.
gan: Deuss, A, et al.
Cyhoeddwyd: (2001)

Comparison of 304 SS, 2205 SS, and 410 SS Corrosion by Sulfate-Reducing Desulfovibrio ferrophilus
gan: Junlei Wang, et al.
Cyhoeddwyd: (2021-01-01)

Typhoon Quantitative Precipitation Forecasts by the 2.5 km CReSS Model in Taiwan: Examples and Role of Topography
gan: Chung-Chieh Wang, et al.
Cyhoeddwyd: (2022-04-01)

Transient D '' discontinuity revealed by seismic migration
gan: Chambers, K, et al.
Cyhoeddwyd: (2006)

The Effect of H2O on the 410-Kilometer Seismic Discontinuity.
gan: Wood, B
Cyhoeddwyd: (1995)

Topography of the 660-km discontinuity within the Izu-Bonin subduction zone and evidence of slab penetration near the Bonin Super Deep Earthquake (∼680 km)[Key points]
gan: Gang Hao
Cyhoeddwyd: (2023-12-01)

Mineralogical phase change at the 670-km discontinuity
gan: Wood, B
Cyhoeddwyd: (1989)

Comparison of erosion performance of uncladded and WC-based laser cladded SS304 and SS410 steels
gan: Sarpreet Singh, et al.
Cyhoeddwyd: (2022-08-01)

Measuring the seismic velocity in the top 15 km of Earth’s inner core
gan: Godwin, H, et al.
Cyhoeddwyd: (2017)

MANTLE GEOPHYSICS - MINERALOGICAL PHASE-CHANGE AT THE 670-KM DISCONTINUITY
gan: Wood, B
Cyhoeddwyd: (1989)

Global Variability of Density Contrast Across the 660‐km Discontinuity
gan: Jingchuan Wang, et al.
Cyhoeddwyd: (2023-02-01)

Constraints on core-mantle boundary topography from normal mode splitting
gan: Soldati, G, et al.
Cyhoeddwyd: (2013)

Seismic evidence for a 1000 km mantle discontinuity under the Pacific
gan: Zhendong Zhang, et al.
Cyhoeddwyd: (2023-03-01)

Seismic evidence for a 1000 km mantle discontinuity under the Pacific
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THE 400-KM SEISMIC DISCONTINUITY AND THE PROPORTION OF OLIVINE IN THE EARTHS UPPER MANTLE
gan: Bina, C, et al.
Cyhoeddwyd: (1986)

Sharpness of the paired 660-km discontinuity beneath the Izu-Bonin area
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Cyhoeddwyd: (2020-11-01)

Investigation of Mechanical Properties in Brazing of Ti-6Al-4V and SS410 in Vacuum
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Cyhoeddwyd: (2015-03-01)

The use of surface topography for the identification of discontinuous displacements due to cracks
gan: Uzun, F, et al.
Cyhoeddwyd: (2020)

The Use of Surface Topography for the Identification of Discontinuous Displacements Due to Cracks
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Cyhoeddwyd: (2020-08-01)

After 410
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Iteration method to determine the eigenvalues and eigenvectors of a target multiplet including full mode coupling
gan: Deuss, A, et al.
Cyhoeddwyd: (2004)

Theory and Observations - Earth's Free Oscillations
gan: Woodhouse, J, et al.
Cyhoeddwyd: (2007)

Theoretical free-oscillation spectra: the importance of wide band coupling
gan: Deuss, A, et al.
Cyhoeddwyd: (2001)

Substantial Global Radial Variations of Basalt Content Near the 660‐km Discontinuity
gan: Shangqin Hao, et al.
Cyhoeddwyd: (2024-12-01)

No basalt accumulation and segregation atop the 660-km discontinuity beneath the Sea of Okhotsk
gan: BingXin Zhou, et al.
Cyhoeddwyd: (2024-07-01)

Regional variation of inner core anisotropy from seismic normal mode observations.
gan: Deuss, A, et al.
Cyhoeddwyd: (2010)

Parameter Impacts of Martensitic Structure on Tensile Strength and Hardness of TIG Welded SS410 with characterized SEM Consequences
gan: G. Mahesh, et al.
Cyhoeddwyd: (2023-01-01)

Normal mode sensitivity to Earth's D″ layer and topography on the core-mantle boundary: What we can and cannot see
gan: Koelemeijer, P, et al.
Cyhoeddwyd: (2012)

PP 4.10 – 00119 Multiomic dynamics of the cellular HIV reservoir after rebound during ATI
gan: V. Wu, et al.
Cyhoeddwyd: (2022-12-01)

Statistical Design of Biocarbon Reinforced Sustainable Composites from Blends of Polyphthalamide (PPA) and Polyamide 4,10 (PA410)
gan: Mateo Gonzalez de Gortari, et al.
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OLIVINE-SPINEL TRANSITIONS - EXPERIMENTAL AND THERMODYNAMIC CONSTRAINTS AND IMPLICATIONS FOR THE NATURE OF THE 400-KM SEISMIC DISCONTINUITY
gan: Bina, C, et al.
Cyhoeddwyd: (1987)

Normal mode coupling due to hemispherical anisotropic structure in Earth's inner core
gan: Irving, J, et al.
Cyhoeddwyd: (2009)

Coupled normal-mode sensitivity to inner-core shear velocity and attenuation
gan: Andrews, J, et al.
Cyhoeddwyd: (2006)

Ultratoughening of Biobased Polyamide 410
gan: Saroj Kumar Samantaray, et al.
Cyhoeddwyd: (2020-03-01)