Data for: Petrogenesis and tectonic implications of two types of gneissic granitoids in the Jiao-Liao-Ji belt, North China Craton
Published: 24 June 2019| Version 1 | DOI: 10.17632/mmp4nhm6db.1
Contributors:
Zhenghong Liu, Kai Zhu, Zhongyuan Xu, Weilong CuiDescription
Whole-rock major and trace element analyses were performed at ALS Chemex Labs in Guangzhou, China. Major element compositions were determined by X-ray fluorescence using a PANalytical Axios Advanced PW4400 XRF spectrometer. Trace element compositions were determined by inductively coupled plasma mass spectrometry (ICP–MS; X-series). Zircon U–Pb dating by laser ablation (LA)–ICP–MS and in situ zircon Lu–Hf isotope analyseswas were performed at the MRL Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China.
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Geochemistry, Age Dating