中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Core-Mantle Boundary Dynamic Topography: Influence of Postperovskite Viscosity

文献类型:期刊论文

作者Deschamps, Frederic2; Li, Yang1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2019-08-01
卷号124期号:8页码:9247-9264
关键词convection mantle dynamics core-mantle boundary topography postperovskite
ISSN号2169-9313
DOI10.1029/2019JB017859
英文摘要Core-mantle boundary (CMB) topography may provide useful hints on the deep mantle thermochemical structure, as clusters of thermal plumes and piles of chemically differentiated material, which are usually proposed as end-member explanations for the large low shear-wave velocity regions observed in the deep mantle, have different actions on this topography. CMB topography is further sensitive to several parameters, including mantle viscosity and its variations with thermal and compositional changes. Here we assess the influence of the postperovskite (pPv) phase viscosity on deep mantle dynamics and on CMB topography. We perform numerical simulations of thermal and thermochemical convection in spherical geometry, varying the ratio between pPv and bridgmanite viscosities, Delta eta(pPv), between 1 (regular pPv) and 10(-3) (weak pPv). Thermochemical structures are dominated by smaller-scale wavelengths (spherical harmonic degrees 3 to 6) and are more stable in weak than in regular pPv models. The amplitude of CMB topography is reduced by about a factor of 2 as Delta eta(pPv) changes from 1 to 10(-3), mostly due to a sharp drop in the depressions induced by downwellings reaching the CMB. By contrast, the topographies induced by plumes clusters and thermochemical piles are mostly unaffected. For all the values of Delta eta(pPv) we tested, long-wavelength CMB topography and reconstructed shear-wave tomography are anticorrelated in purely thermal models, and correlated in thermochemical models with strong chemical density contrast (Delta rho(C) = 140 kg/m(3)). In models with smaller density contrast (Delta rho(C) = 90 kg/m(3)), topography and tomography are anticorrelated at Delta eta(pPv) = 1, but correlated at Delta eta(pPv) = 10(-3).
WOS关键词POST-PEROVSKITE PHASE ; FREE-OSCILLATION SPECTRA ; PRIMORDIAL RESERVOIRS ; NORMAL-MODE ; THERMOCHEMICAL CONVECTION ; TRAVEL-TIMES ; CONSTRAINTS ; DENSITY ; VELOCITY ; STABILITY
资助项目Academia Sinica Investigator Award[AS-IA-108-M03] ; Ministry of Science and Technology (MoST) of Taiwan[107-2116-M-001-010] ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000491283500088
出版者AMER GEOPHYSICAL UNION
资助机构Academia Sinica Investigator Award ; Academia Sinica Investigator Award ; Ministry of Science and Technology (MoST) of Taiwan ; Ministry of Science and Technology (MoST) of Taiwan ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Academia Sinica Investigator Award ; Academia Sinica Investigator Award ; Ministry of Science and Technology (MoST) of Taiwan ; Ministry of Science and Technology (MoST) of Taiwan ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Academia Sinica Investigator Award ; Academia Sinica Investigator Award ; Ministry of Science and Technology (MoST) of Taiwan ; Ministry of Science and Technology (MoST) of Taiwan ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Academia Sinica Investigator Award ; Academia Sinica Investigator Award ; Ministry of Science and Technology (MoST) of Taiwan ; Ministry of Science and Technology (MoST) of Taiwan ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program ; Chinese Academy of Sciences (CAS) Pioneer Hundred Talent Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/95758]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Deschamps, Frederic
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
2.Acad Sin, Inst Earth Sci, Taipei, Taiwan
推荐引用方式
GB/T 7714
Deschamps, Frederic,Li, Yang. Core-Mantle Boundary Dynamic Topography: Influence of Postperovskite Viscosity[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2019,124(8):9247-9264.
APA Deschamps, Frederic,&Li, Yang.(2019).Core-Mantle Boundary Dynamic Topography: Influence of Postperovskite Viscosity.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,124(8),9247-9264.
MLA Deschamps, Frederic,et al."Core-Mantle Boundary Dynamic Topography: Influence of Postperovskite Viscosity".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 124.8(2019):9247-9264.

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来源:地质与地球物理研究所

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