Re-melting of the Neoproterozoic juvenile mafic lower crust: The origin of adakitic and non-adakitic felsic suites in the southwest margin of Yangtze Craton-Reference-Cited by-同舟云学术

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Re-melting of the Neoproterozoic juvenile mafic lower crust: The origin of adakitic and non-adakitic felsic suites in the southwest margin of Yangtze Craton

Published:2024-06 Issue: Volume:474-475 Page:107601
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Wu Jingkai,Zhao Zhidan,Li Xiaowei,Tu Xuejing,Li Chen,Lei Hangshan,Ma Qian,Miao Zhuang,Yang Yiyun,Liu Dong,Wang Qing,Zhu Di-Cheng,Hou Zengqian,Mo Xuanxue

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

National Key Research and Development Program of China

Higher Education Discipline Innovation Project

Publisher

Elsevier BV

Reference80 articles.

1. Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons;Amelin;Nature,1999

2. Correction of common lead in U-Pb analyses that do not report Pb-204;Andersen;Chem. Geol.,2002

3. Compositions of near-solidus peridotite melts from experiments and thermodynamic calculations;Baker;Nature,1995

4. The Lu-Hf isotope geochemistry of shergottites and the evolution of the Martian mantle-crust system;Blichert-Toft;Earth Planet. Sci. Lett.,1999

5. Neoproterozoic subduction along the Ailaoshan zone, South China: Geochronological and geochemical evidence from amphibolite;Cai;Precambrian Res.,2014

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