Trace element and S-Pb isotopic compositions of pyrite from the Precambrian metamorphic rocks and their derivative pegmatites in the Xiaoqinling district, southern North China Craton: Implications for possible gold source of the Early Cretaceous gold deposits

• Published in: Precambrian research 2022-08, Vol.377, p.106739, Article 106739
• Main Authors: Zhao, Shao-Rui, Li, Zhan-Ke, Li, Jian-Wei, Zhao, Xin-Fu, Jiang, Shao-Yong, Lin, Hai-Tao, Jie, Ya-Qi, Tao, Huan, Du, Shi-Guang
• Format: Article
• Language: English
• Subjects: Gold source; North China Craton; Precambrian metamorphic basement; Pyrite trace elements; S-Pb isotopes
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2022.106739

•Pyrite cogenetic with the Precambrian metamorphic rocks and their derivative pegmatites in the Xiaoqinling district contain low Au contents.•Pyrite cogenetic with the Precambrian metamorphic rocks and their derivative pegmatites has S-Pb isotopes distinct from those of regional gold deposits.•The Precambrian metamorphic basement rocks are not a major Au source for the Early Cretaceous gold mineralization in the Xiaoqinling district. The North China Craton is well endowed with numerous Early Cretaceous gold deposits that are mainly hosted in Archean to early Paleoproterozoic metamorphic rocks and late Mesozoic granitoid intrusions intruding the former. Whether or not gold was sourced from those metamorphic rocks remains hotly debated. Here we present trace element and S-Pb isotope data of pyrite from the Neoarchean to early Paleoproterozoic metamorphic rocks in the Xiaoqinling district of southern North China Craton and late Paleoproterozoic pegmatites derived from the former rocks, in an attempt to provide new insights into the gold sources for Early Cretaceous gold lodes genesis in this district. Pyrite from the metamorphic rocks typically occurs as inclusions in rock-forming minerals or disseminated grains roughly distributed along the foliation of the rocks, whereas pyrite from the pegmatites usually occurs as disseminations closely associated with quartz and magnetite. The textural data suggest that pyrite in the metamorphic rocks and pegmatites are of metamorphogenic and magmatogenic origins, respectively. LA-ICP-MS spot analyses show that pyrite both from the metamorphic rocks and pegmatites has Au contents mostly below the detection limit, with minor analyses revealing Au marginally higher than the detection limit. Considering that Au is moderately incompatible and highly siderophile, the very low gold contents in pyrite allow us to infer that the metamorphic rocks contain negligible gold. Pyrite grains from the metamorphic rocks and pegmatites have broadly consistent δ34S values ranging from −2.7 to 31.5 (mean = 17.6) per mil and 6.3 to 17.9 (mean = 14.3) per mil, respectively. Similarly, they have comparable, highly radiogenic lead isotopes, which are 16.859–24.889 for 206Pb/204Pb, 15.355–15.694 for 207Pb/204Pb, and 37.480–43.848 for 208Pb/204Pb. The sulfur and lead isotopes of pyrites from the metamorphic rocks and pegmatites are distinct from those of Early Cretaceous gold deposits hosted by these rocks. Taken together, the pyrite trace element