Author:
Lan Zhongwu,Kamo Sandra L.,Roberts Nick M.W.,Sano Yuji,Li Xian-Hua
Funder
Chinese Academy of Sciences
China University of Geosciences, Wuhan
State Key Laboratory of Palaeobiology and Stratigraphy
State Key Laboratory of Geological Processes and Mineral Resources
National Natural Science Foundation of China
Subject
Geochemistry and Petrology,Geology
Reference61 articles.
1. Pre-3750 Ma supracrustal rocks from the Nuvvuagittuq supracrustal belt, northern Québec;Cates;Earth Planet. Sci. Lett.,2007
2. Metamorphic zircon, trace elements and Neoarchean metamorphism in the ca. 3.75 Ga Nuvvuagittuq supracrustal belt, Québec (Canada);Cates;Chem. Geol.,2009
3. Reduced, reused and recycled: Detrital zircons define a maximum age for the Eoarchean (ca. 3750–3780 Ma) Nuvvuagittuq supracrustal belt, Québec (Canada);Cates;Earth Planet. Sci. Lett.,2013
4. Cellular remains in a ∼3.42-billion-year-old sub-seafloor hydrothermal environment.;Cavalazzi;Sci. Adv.,2021
5. A multistage origin for Neoarchean layered hematite-magnetite iron formation from the Weld Range, Yilgarn Craton, Western Australia;Czaja;Chem. Geol.,2018
Cited by
6 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献