Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons. / Koelemeijer, P.; Schuberth, B. S.A.; Davies, D. R.; Deuss, A.; Ritsema, J.

In: Earth and Planetary Science Letters, Vol. 494, 15.07.2018, p. 226-238.

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Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons. / Koelemeijer, P.; Schuberth, B. S.A.; Davies, D. R.; Deuss, A.; Ritsema, J.

In: Earth and Planetary Science Letters, Vol. 494, 15.07.2018, p. 226-238.

Research output: Contribution to journalArticle

Harvard

Koelemeijer, P, Schuberth, BSA, Davies, DR, Deuss, A & Ritsema, J 2018, 'Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons', Earth and Planetary Science Letters, vol. 494, pp. 226-238. https://doi.org/10.1016/j.epsl.2018.04.056

APA

Koelemeijer, P., Schuberth, B. S. A., Davies, D. R., Deuss, A., & Ritsema, J. (2018). Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons. Earth and Planetary Science Letters, 494, 226-238. https://doi.org/10.1016/j.epsl.2018.04.056

Vancouver

Author

Koelemeijer, P. ; Schuberth, B. S.A. ; Davies, D. R. ; Deuss, A. ; Ritsema, J. / Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons. In: Earth and Planetary Science Letters. 2018 ; Vol. 494. pp. 226-238.

BibTeX

@article{2912a44419ab4cde8e1cea750b7aa002,
title = "Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons",
abstract = "Lower mantle tomography models consistently feature an increase in the ratio of shear-wave velocity (VS) to compressional-wave velocity (VP) variations and a negative correlation between shear-wave and bulk-sound velocity (VC) variations. These seismic characteristics, also observed in the recent SP12RTS model, have been interpreted to be indicative of large-scale chemical variations. Other explanations, such as the lower mantle post-perovskite (pPv) phase, which would not require chemical heterogeneity, have been explored less. Constraining the origin of these seismic features is important, as geodynamic simulations predict a fundamentally different style of mantle convection under both scenarios. Here, we investigate to what extent the presence of pPv explains the observed high VS/VP ratios and negative VS–VC correlation globally. We compare the statistical properties of SP12RTS with the statistics of synthetic tomography models, derived from both thermal and thermochemical models of 3-D global mantle convection. We convert the temperature fields of these models into seismic velocity structures using mineral physics lookup tables with and without pPv. We account for the limited tomographic resolution of SP12RTS using its resolution operator for both VS and VP structures. This allows for direct comparisons of the resulting velocity ratios and correlations. Although the tomographic filtering significantly affects the synthetic tomography images, we demonstrate that the effect of pPv remains evident in the ratios and correlations of seismic velocities. We find that lateral variations in the presence of pPv have a dominant influence on the VS/VP ratio and VS–VC correlation, which are thus unsuitable measures to constrain the presence of large-scale chemical variations in the lowermost mantle. To explain the decrease in the VS/VP ratio of SP12RTS close to the CMB, our results favour a pPv-bearing CMB region, which has implications for the stability field of pPv in the Earth's mantle.",
keywords = "composition of the mantle, geodynamic modelling, mineral physics, seismic tomography, tomographic filtering",
author = "P. Koelemeijer and Schuberth, {B. S.A.} and Davies, {D. R.} and A. Deuss and J. Ritsema",
year = "2018",
month = "7",
day = "15",
doi = "10.1016/j.epsl.2018.04.056",
language = "English",
volume = "494",
pages = "226--238",
journal = "Earth and Planetary Science Letters",
issn = "0012-821X",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Constraints on the presence of post-perovskite in Earth's lowermost mantle from tomographic-geodynamic model comparisons

AU - Koelemeijer, P.

AU - Schuberth, B. S.A.

AU - Davies, D. R.

AU - Deuss, A.

AU - Ritsema, J.

PY - 2018/7/15

Y1 - 2018/7/15

N2 - Lower mantle tomography models consistently feature an increase in the ratio of shear-wave velocity (VS) to compressional-wave velocity (VP) variations and a negative correlation between shear-wave and bulk-sound velocity (VC) variations. These seismic characteristics, also observed in the recent SP12RTS model, have been interpreted to be indicative of large-scale chemical variations. Other explanations, such as the lower mantle post-perovskite (pPv) phase, which would not require chemical heterogeneity, have been explored less. Constraining the origin of these seismic features is important, as geodynamic simulations predict a fundamentally different style of mantle convection under both scenarios. Here, we investigate to what extent the presence of pPv explains the observed high VS/VP ratios and negative VS–VC correlation globally. We compare the statistical properties of SP12RTS with the statistics of synthetic tomography models, derived from both thermal and thermochemical models of 3-D global mantle convection. We convert the temperature fields of these models into seismic velocity structures using mineral physics lookup tables with and without pPv. We account for the limited tomographic resolution of SP12RTS using its resolution operator for both VS and VP structures. This allows for direct comparisons of the resulting velocity ratios and correlations. Although the tomographic filtering significantly affects the synthetic tomography images, we demonstrate that the effect of pPv remains evident in the ratios and correlations of seismic velocities. We find that lateral variations in the presence of pPv have a dominant influence on the VS/VP ratio and VS–VC correlation, which are thus unsuitable measures to constrain the presence of large-scale chemical variations in the lowermost mantle. To explain the decrease in the VS/VP ratio of SP12RTS close to the CMB, our results favour a pPv-bearing CMB region, which has implications for the stability field of pPv in the Earth's mantle.

AB - Lower mantle tomography models consistently feature an increase in the ratio of shear-wave velocity (VS) to compressional-wave velocity (VP) variations and a negative correlation between shear-wave and bulk-sound velocity (VC) variations. These seismic characteristics, also observed in the recent SP12RTS model, have been interpreted to be indicative of large-scale chemical variations. Other explanations, such as the lower mantle post-perovskite (pPv) phase, which would not require chemical heterogeneity, have been explored less. Constraining the origin of these seismic features is important, as geodynamic simulations predict a fundamentally different style of mantle convection under both scenarios. Here, we investigate to what extent the presence of pPv explains the observed high VS/VP ratios and negative VS–VC correlation globally. We compare the statistical properties of SP12RTS with the statistics of synthetic tomography models, derived from both thermal and thermochemical models of 3-D global mantle convection. We convert the temperature fields of these models into seismic velocity structures using mineral physics lookup tables with and without pPv. We account for the limited tomographic resolution of SP12RTS using its resolution operator for both VS and VP structures. This allows for direct comparisons of the resulting velocity ratios and correlations. Although the tomographic filtering significantly affects the synthetic tomography images, we demonstrate that the effect of pPv remains evident in the ratios and correlations of seismic velocities. We find that lateral variations in the presence of pPv have a dominant influence on the VS/VP ratio and VS–VC correlation, which are thus unsuitable measures to constrain the presence of large-scale chemical variations in the lowermost mantle. To explain the decrease in the VS/VP ratio of SP12RTS close to the CMB, our results favour a pPv-bearing CMB region, which has implications for the stability field of pPv in the Earth's mantle.

KW - composition of the mantle

KW - geodynamic modelling

KW - mineral physics

KW - seismic tomography

KW - tomographic filtering

UR - http://www.scopus.com/inward/record.url?scp=85046870274&partnerID=8YFLogxK

U2 - 10.1016/j.epsl.2018.04.056

DO - 10.1016/j.epsl.2018.04.056

M3 - Article

AN - SCOPUS:85046870274

VL - 494

SP - 226

EP - 238

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

SN - 0012-821X

ER -