globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2020.116685
论文题名:
Constraints on the composition and temperature of LLSVPs from seismic properties of lower mantle minerals
作者: Vilella K.; Bodin T.; Boukaré C.-E.; Deschamps F.; Badro J.; Ballmer M.D.; Li Y.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2021
卷: 554
语种: 英语
中文关键词: composition ; equation of state ; LLSVP ; seismic properties
英文关键词: Alumina ; Aluminum oxide ; Iron ; Iron oxides ; Minerals ; Seismology ; Shear flow ; Solidification ; Temperature ; Formation mechanism ; Large Low Shear Velocity Provinces (LLSVPs) ; Low temperatures ; Lowermost mantle ; Oxidation state ; Seismic observation ; Seismic properties ; Temperature contrast ; Calcium compounds ; air temperature ; equation of state ; lower mantle ; magma ; mineralogy ; oxidation ; principal component analysis ; seismic property
英文摘要: Seismic observations have suggested the presence of two Large Low Shear Velocity Provinces (LLSVPs) in the lowermost mantle whose nature and origin are still debated. Several studies have tried to infer their potential composition using seismic observations with the hope to identify their formation mechanism. In particular, compositions enriched in iron (∼12–14 wt%) and bridgmanite (∼90 vol%) have been identified as promising candidates. Interestingly, these characteristics are somewhat consistent with the cumulates produced by the solidification of a primitive magma ocean, except that the iron enrichment should be much larger (>20 wt%). Here, we provide a reappraisal of potential LLSVPs compositions based on an improved mineralogical model including, in particular, the effects of alumina. We systematically investigate the effects of six parameters: FeO and Al2O3 content, proportion of CaSiO3 and bridgmanite (so that the proportion of ferropericlase is implicitly investigated), Fe3+/∑Fe and temperature contrast between far-field mantle and LLSVPs. From the 81 millions cases studied, only 79000 cases explain the seismic observations. Nevertheless, these successful cases involve a large range of parameters with, for instance, FeO content between 12–25 wt% and Al2O3 content between 3–17 wt%. We then apply a principal component analysis (PCA) to these cases and find two robust results: (i) the proportion of ferropericlase should be low (<6 vol%); (ii) the formation of Fe3+-bearing bridgmanite is much more favored compared to other iron-bearing components. Following these results, we identify two end-member compositions: a Bm-rich and a CaPv-rich one. For each end-member composition, a large range of parameters is possible. We note, however, that a low temperature contrast (<500 K) is favored, and that a certain proportion between FeO content, Al2O3 and oxidation state should be maintained. Finally, we discuss different scenarios for the formation of LLSVPs and propose that investigating the mineral proportion produced by each scenario is the best way to evaluate their relevance. For instance, the solidification of a primitive magma ocean may produce FeO and Al2O3 contents similar to those suggested by our analysis. However, the mineral proportion of such reservoirs is not well-constrained and may contain a larger proportion of ferropericlase than what is allowed by our results. © 2020 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165699
Appears in Collections:气候变化与战略

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作者单位: JSPS International Research Fellow, Hokkaido University, Japan; Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan; Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, Villeurbanne, F-69622, France; Earth and Planetary Science Laboratory, École Polytechnique Fédérale de Lausanne, Lausanne, Switzerland; Institut de Physique du Globe, Univ. Paris Diderot, Sorbonne Paris Cité, CNRS, Paris, France; Institute of Geophysics, Department of Earth Sciences, ETH Zurich, Zurich, Switzerland; University College London, Department of Earth Sciences, London, United Kingdom; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, China

Recommended Citation:
Vilella K.,Bodin T.,Boukaré C.-E.,et al. Constraints on the composition and temperature of LLSVPs from seismic properties of lower mantle minerals[J]. Earth and Planetary Science Letters,2021-01-01,554
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