Recycling carbonated hydrous sediments into the mantle source of carbonatite-associated rare-earth-element deposits-Reference-Cited by-同舟云学术

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Recycling carbonated hydrous sediments into the mantle source of carbonatite-associated rare-earth-element deposits

Published:2024-09 Issue: Volume:133 Page:1-13
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Geng Xianlei^ORCID,Tian Shihong,Chen Lu,Liang Zhengwei,Xu Wei,Lu Na,Hu Wenjie,Xiang Mi

Publisher

Elsevier BV

Reference151 articles.

1. Geochemistry, Sr–Nd–Pb isotopes and geochronology of amphibole- and mica-bearing lamprophyres in northwestern Iran: implications for mantle wedge heterogeneity in a palaeo-subduction zone;Aghazadeh;Lithos,2015

2. Carbon dioxide released from subduction zones by fluid-mediated reactions;Ague;Nat. Geosci.,2014

3. Calcium isotopic evidence for the mantle sources of carbonatites;Amsellem;Sci. Adv.,2020

4. Lithospheric thickness of the Chinese Continent;An;Phys. Earth Planet.,2006

5. Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica;Anenburg;Sci. Adv.,2020

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