2023 Vol. 46, No. 4
Article Contents

HAN Mingyang, CAO Binhua, ZHANG Lechong, MA Wei, LI Yachao. 2023. Zirconage and geochemistry of granodioritic gneissin in Huai'an, Hebei province. North China Geology, 46(4): 1-9. doi: 10.19948/j.12-1471/P.2023.04.01
Citation: HAN Mingyang, CAO Binhua, ZHANG Lechong, MA Wei, LI Yachao. 2023. Zirconage and geochemistry of granodioritic gneissin in Huai'an, Hebei province. North China Geology, 46(4): 1-9. doi: 10.19948/j.12-1471/P.2023.04.01

Zirconage and geochemistry of granodioritic gneissin in Huai'an, Hebei province

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  • Corresponding author: CAO Binhua  
  • The northern and southern margin of the north China continent are widely distributed in the early Cambrian TTG system,which is the oldest known in the world.The geochemical characteristics of the early Cambrian rocks are quite different from the origins and Genesis.Therefore,it is of great significance to study the geochemical analysis Geochemical analysis and geochronology of granodioritic gneiss in Huai'an area,Hebei Province,and evolution,hyperplasia as well as reforger in the north China.The results show the LA-ICP-MS zircon U-Pb isotope concordia diagram age is 2 551 Ma,indicated granodiorite rock body was formed in Early Paleoproterozoic Era.Granite.The intrusion is dominated by medium grained hypersthenes Granodioritic gneiss.Their SiO2 and total alkaline contents are in the ranges of 67.30%~74.94%(average 70.94%)and 5.57%~8.01%(average 6.37%),respectively.Most of rocks belong to peraluminous(average A/CNK=1.53)granite and generated in syncollisional setting.This intrusion is formed in a magmatic arc tectonic environment.
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