Hf-Nd isotope decoupling in S-type granitoids caused by disequilibrium melting of metasedimentary rocks: Evidence from the North Qinling Terrane, Central China-Reference-Cited by-同舟云学术

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Hf-Nd isotope decoupling in S-type granitoids caused by disequilibrium melting of metasedimentary rocks: Evidence from the North Qinling Terrane, Central China

Published:2024-06 Issue: Volume:474-475 Page:107598
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Sun Fang-Yuan,Zhang Shao-Bing,Zheng Yong-Fei,Li Zhen-Xin,Liang Ting

Funder

Chinese Academy of Medical Sciences & Peking Union Medical College

Chinese Academy of Sciences

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference82 articles.

1. The control of weathering processes on riverine and seawater hafnium isotope ratios;Bayon;Geology,2006

2. Hf and Nd isotopes in marine sediments: Constraints on global silicate weathering;Bayon;Earth Planet. Sci. Lett.,2009

3. Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation-ICP-MS study);Bea;Chem. Geol.,1994

4. Lu-Hf ratios of crustal rocks and their bearing on zircon Hf isotope model ages: the effects of accessories;Bea;Chem. Geol.,2018

5. Hf isotopic measurements on Barberton komatiites: effects of incomplete sample dissolution and importance for primary and secondary magmatic signatures;Blichert-Toft;Chem. Geol.,2004

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