U-Pb ages, Hf-O isotopes and trace elements of zircons from the ore-bearing and ore-barren adakitic rocks in the Handan-Xingtai district: Implications for petrogenesis and iron mineralization

• Published in: Ore geology reviews Vol. 104; pp. 14 - 25
• Main Authors: Sun, Yi, Wu, Tao, Xiao, Long, Bai, Ming, Zhang, Yanhai
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.01.2019
• Subjects: Adakitic rock; Handan-Xingtai district; Iron mineralization; Oxygen fugacity; Zircon Hf-O isotopes; Adakitic rock; Oxygen fugacity; Zircon Hf-O isotopes; Handan-Xingtai district; Iron mineralization
• ISSN: 0169-1368; 1872-7360
• DOI: 10.1016/j.oregeorev.2018.10.010

[Display omitted] •The ore-bearing complexes have low Ti-in-zircon temperatures but high oxygen fugacity.•The ore-bearing complexes have a mixed source, whereas the ore-barren one was derived from the SCLM.•The lower crustal materials may have played key roles in iron mineralization. The petrogenesis of the Early Cretaceous adakitic intrusions in the Handan-Xingtai district, central North China Craton (NCC), and their genetic association with iron mineralization still remain controversial. Here, we present an integrated study of zircon U-Pb ages and Hf-O isotopes, as well as their trace elements for the ore-bearing and ore-barren complexes in the Handan-Xingtai district. Both of the ore-bearing and ore-barren complexes were emplaced contemporaneously (Early Cretaceous). Zircon εHf(t) and δ18O values of ore-barren complex range from −16.0 to −13.3 and from 6.3‰ to 7.1‰, respectively, whereas those of ore-bearing complexes have variable δ18O (5.7‰ to 8.3‰) and much lower εHf(t) values (−24.3 to −18.3). Furthermore, the ore-bearing complexes also have lower Ti-in-zircon temperatures but higher water contents and oxygen fugacity than those of ore-barren complexes. The zircon Hf-O isotopes, as well as their trace element data, indicate that the parental magma of ore-bearing complexes was a mixture of melts that derived from the enriched lithospheric mantle and ancient lower continental crust, whereas the ore-barren complex was most likely generated by partial melting of the enriched lithospheric mantle. We proposed that the high oxidation states and high water contents of magma, as well as the lower crustal materials may have played key roles in iron mineralization of Handan-Xingtai district.