Age of the Zhongtiaoshan dyke swarm: Constraints on the nature of the 1.8 Ga large igneous province event in North China
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Publisher
Science China Press., Co. Ltd.
Subject
Multidisciplinary
Link
https://engine.scichina.com/doi/pdf/854C8419F3FF48E6869A3404B43A1BF5
Reference60 articles.
1. Peng P. Precambrian mafic dyke swarms in the North China Craton and their geological implications. Sci China Earth Sci, 2015, 58: 649-675.
2. Wang Y, Fan W, Zhang Y. Geochemical, 40Ar/39Ar geochronological and Sr-Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800 Ma event of the North China Craton. Precambrian Res, 2004, 135: 55-77.
3. Wang X, Zhu W, Luo M. Approximately 1.78 Ga mafic dykes in the Lüliang Complex, North China Craton: Zircon ages and Lu-Hf isotopes, geochemistry, and implications. Geochem Geophys Geosyst, 2014, 15: 3123-3144.
4. Hou G, Li J, Yang M. Geochemical constraints on the tectonic environment of the Late Paleoproterozoic mafic dyke swarms in the North China Craton. Gondwana Res, 2008, 13: 103-116.
5. Peng P. Reconstruction and interpretation of giant mafic dyke swarms: A case study of 1.78 Ga magmatism in the North China Craton. Geol Soc Lond Spec Publ, 2010, 338: 163-178.
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