Element Partitioning and Li‐O Isotope Fractionation Between Silicate Minerals and Crustal‐Derived Carbonatites and Their Implications-Reference-Cited by-同舟云学术

Element Partitioning and Li‐O Isotope Fractionation Between Silicate Minerals and Crustal‐Derived Carbonatites and Their Implications

Author:

Su Ben‐Xun¹²^ORCID,Wang Jing¹,Cui Meng‐Meng¹²,Wu Yong³,Pang Kwan‐Nang⁴^ORCID,Malaviarachchi Sanjeewa P. K.⁵,Dharmapriya P. L.⁵

Affiliation:

1. Key Laboratory of Mineral Resources Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. University of Chinese Academy of Sciences Beijing China

3. Beijing Research Institute of Uranium Geology Beijing China

4. Institute of Earth Sciences Academia Sinica Taipei Taiwan

5. Department of Geology, Faculty of Science University of Peradeniya Peradeniya Sri Lanka

Funder

Youth Innovation Promotion Association

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference52 articles.

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1. Carbonatites and related mineralization: an overview;Geological Society, London, Special Publications;2024-09-10