Establishing the occurrence of late Neoarchaean - earliest Palaeoproterozoic magmatism in the Daqingshan area, northwestern North China Craton: SIMS U-Pb zircon dating, Lu-Hf and Sm-Nd isotopes and whole-rock geochemistry

Daqingshan is located in the northwestern North China Craton where late Neoarchaean supracrustal rocks occur widely, but where magmatic zircon ages have rarely been reported for plutonic rocks. In this study, we report SIMS U-Pb zircon ages and Hf isotope, whole-rock element and Nd isotope compositions for 12 magmatic samples, including TTG, quartz monzonitic and monzogranitic gneisses, and meta-gabbroic and dioritic rocks. They have magmatic zircon ages of 2530-2469 Ma; some samples have ages of <2.48 Ga likely influenced by late Palaeoproterozoic tectonothermal events, making their ages less reliable. TTG gneisses have low Sr/Y and La/Yb ratios, with whole-rock epsilon(Nd)(t) and in situ magmatic zircon epsilon(Hf)(t) values of +1.2 to +2.4 and -1.1 to +6.2, respectively. Quartz monzonite and monzogranite gneisses and gabbroic to dioritic rocks have similar Nd-Hf isotope compositions to the TTG gneisses. The absence of zircon >2.6 Ga in the early Precambrian rocks suggests that the Sanggan Group may have formed in an oceanic environment, whereas the TTG rocks formed as a result of partial melting of the basaltic rocks of the Sanggan Group under relatively low-pressure conditions. Combined with previous studies, the main conclusions are that in the Daqingshan area, late Neoarchaean magmatism was widespread, the late Mesoarchaean - early Neoarchaean was an important period of juvenile continental crustal growth, and the late Neoarchaean supracrustal and plutonic rocks most likely formed in an arc environment. These are common signatures for Neoarchaean crustal evolution throughout much of the North China Craton, and also globally.

Automated summary

This study reports the geochronological and petrographic characteristics of 12 magmatic samples from the Daqingshan area. The samples have magmatic zircon ages of 2530-2469 Ma, with some samples showing ages influenced by late Palaeoproterozoic tectonothermal events. Combined with previous studies, the findings suggest that the late Mesoarchaean-early Neoarchaean was a period of significant continental crustal growth, and the late Neoarchaean supracrustal and plutonic rocks likely formed in an arc environment.