New High‐Pressure Phase of CaCO 3 at the Topmost Lower Mantle: Implication for the Deep‐Mantle Carbon Transportation-Reference-Cited by-同舟云学术

New High‐Pressure Phase of CaCO 3 at the Topmost Lower Mantle: Implication for the Deep‐Mantle Carbon Transportation

Published:2018-02-12 Issue:3 Volume:45 Page:1355-1360
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Li Xinyang¹^ORCID,Zhang Zhigang²³,Lin Jung‐Fu⁴^ORCID,Ni Huaiwei¹^ORCID,Prakapenka Vitali B.⁵^ORCID,Mao Zhu¹^ORCID

Affiliation:

1. Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Planetary SciencesUniversity of Science and Technology of China Hefei China

2. Key Laboratory of Earth and Planetary PhysicsInstitute of Geology and Geophysics, Chinese Academy of Sciences Beijing China

3. College of Earth ScienceUniversity of Chinese Academy of Sciences Beijing China

4. Department of Geological Sciences, Jackson School of GeosciencesThe University of Texas at Austin Austin TX USA

5. Center for Advanced Radiation SourcesUniversity of Chicago Chicago IL USA

Funder

Alfred P. Sloan Foundation

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL076536

Reference39 articles.

1. Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application

2. The uptake of carbon during alteration of ocean crust

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4. Carbonates from the lower part of transition zone or even the lower mantle

5. Diamonds from the Machado River alluvial deposit, Rondônia, Brazil, derived from both lithospheric and sublithospheric mantle

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