Geochronology and geochemistry of Beilou granitic pluton: Identification of early Palaeozoic arc magmatic rock in the Dabie Orogen, central China

Abstract

The Dabie Orogen constitutes the eastern part of the Qinling‐Tongbai‐Hong'an‐Dabie orogenic belt, however, whether it has involved into the early Palaeozoic subduction–related event as well‐recorded in the western part is still in debate. This study provides new petrological, geochronological and geochemical data for the Beilou and Mafan plutons in the Dabie‐Hong'an orogens. The Beilou pluton is dominated by granite, some of which have been strongly deformed to form mylonites. The Beilou pluton was emplaced at ca. 490 and ca. 450 Ma, whereas the Mafan pluton was emplaced at 450–430 Ma. The whole‐rock major‐ and trace‐element analyses results indicate that both plutons are depleted in high‐field‐strength elements and heavy rare earth elements. The Beilou pluton also has positive whole‐rock εNd(t) values and generally positive zircon εHf(t) values, whereas all but one of the Mafan pluton samples yield positive whole‐rock εNd(t) and consistently positive zircon εHf(t) values. All of the samples have low (87Sr/86Sr)i ratios. These data indicate that these plutons are formed from magmas generated by the partial melting of metasomatized mantle wedge material with minor additions of crustal materials, representing arc magmatic rocks associated with subduction. Detailed detrital zircon dating of flysch sequences of the Foziling Group within the Dabie Orogen indicates that the early Palaeozoic magmatic rocks had once been distributed in the whole Orogen, although only the Beilou pluton now is exposed in the western Dabie Orogen.

Sedimentological Evidence for Pre‐Early Permian Continental Subduction in the Dabie Orogen, Central‐East China

“…Detrital zircon U‐Pb age spectra from the Foziling Group schists exhibit two substantial age peaks at c. 450 Ma and c. 785–978 Ma ( n = 913, see the compilation in Y. Wang et al. (2022)); (c) Carboniferous coal‐bearing coastal‐facies of the Yangshan Group (Figure 1c) which is the only unmetamorphosed unit in the Beihuaiyang belt and which also exhibits a main detrital zircon U‐Pb peak at c. 450 Ma ( n = 555, C. Cheng et al., 2021).…”