中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Influence of the miscibility of bridgmanite and davemaoite on the long-term evolution of large low shear velocity provinces : insights from 2-D numerical models

文献类型:期刊论文

作者Li Yang1,3; Niu XiaoGuang2,3; Liu ShaoHui1,3; Shi ZhiDong1,3; Zhang ZhiGang2,3; Li Juan2,3; Zhao Liang1,3
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2023-10-01
卷号66期号:10页码:4241-4252
ISSN号0001-5733
关键词Mantle convection Large low shear velocity provinces Bridgmanite Davemaoite Miscibility Numerical modeling
DOI10.6038/cjg2023R0228
英文摘要Bridgmanite and davemaoite are the primary minerals in the deep mantle and are important building blocks of the lower mantle. Recent studies in mineral physics have found that the miscibility of these two minerals will be increased and even become a single perovskite-structured mineral under high-temperature and high-pressure conditions, which would potentially change the physical and chemical state of the lower mantle. In this study, we counted the miscibility of bridgmanite and davemaoite in two-dimensional mantle convection numerical simulations and discussed its long-term dynamic effects on the thermal-chemical structure of the mantle, particularly on the stability of the large low-shear-wave-velocity provinces (LLSVP) in the lower mantle. Our simulation results show that the miscibility of bridgmanite and davemaoite has a positive influence on the long-term preservation of the LLSVPs in the lower mantle, and this stabilizing effect increases as the density difference between the LLSVP and the surrounding mantle decreases, while the Clapeyron slope of the phase transition plays a minor role in the long-term evolution.
WOS关键词POST-PEROVSKITE PHASE ; SPIN TRANSITION ; PRIMORDIAL RESERVOIRS ; MANTLE CONVECTION ; IRON ; STABILITY ; DISCOVERY ; PACIFIC ; LLSVPS ; MGSIO3
WOS研究方向Geochemistry & Geophysics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:001086914800016
源URL[http://ir.iggcas.ac.cn/handle/132A11/110731]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Li Yang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, CAS Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Li Yang,Niu XiaoGuang,Liu ShaoHui,et al. Influence of the miscibility of bridgmanite and davemaoite on the long-term evolution of large low shear velocity provinces : insights from 2-D numerical models[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2023,66(10):4241-4252.
APA Li Yang.,Niu XiaoGuang.,Liu ShaoHui.,Shi ZhiDong.,Zhang ZhiGang.,...&Zhao Liang.(2023).Influence of the miscibility of bridgmanite and davemaoite on the long-term evolution of large low shear velocity provinces : insights from 2-D numerical models.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,66(10),4241-4252.
MLA Li Yang,et al."Influence of the miscibility of bridgmanite and davemaoite on the long-term evolution of large low shear velocity provinces : insights from 2-D numerical models".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 66.10(2023):4241-4252.

入库方式: OAI收割

来源:地质与地球物理研究所

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