Petrogenesis and geodynamic implications of Neoproterozoic gabbro-diorites, adakitic granites, and A-type granites in the southwestern margin of the Yangtze Block, South China

• Published in: Journal of Asian earth sciences 2019-10, Vol.183, p.103977, Article 103977
• Main Authors: Zhu, Yu, Lai, Shao-cong, Qin, Jiang-feng, Zhu, Ren-zhi, Zhang, Fang-yi, Zhang, Ze-zhong, Gan, Bao-ping
• Format: Article
• Language: English
• Subjects: A-type granite; Adakitic granite; Gabbro-diorite; Geodynamic implication; Neoproterozoic; Petrogenesis
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2019.103977

[Display omitted] •Neoproterozoic gabbro-diorites, adakitic granites, A-type granites in South China.•Ca. 810 Ma gabbro-diorites were derived from metasomatized lithospheric mantle.•Ca. 800 Ma adakitic granites were derived from the juvenile thickened lower crust.•Ca. 750 Ma A-type granites were derived from a felsic crustal source.•These rocks imply a persistent subduction process during the Neoproterozoic. The occurrence of A-type granites following adakitic granites can provide unique insights into the tectonic evolution of subduction zone. This paper presents a comprehensive study of zircon U-Pb-Hf isotopes and whole-rock geochemistry on the Neoproterozoic gabbro-diorites, biotite granites, and K-feldspar granites in the southwestern margin of the Yangtze Block, South China. Zircon U-Pb dating of three distinctive intrusions yield concordant ages of 810.4 ± 2.0 Ma for gabbro-diorites, 800.3 ± 2.1 Ma for biotite granites, and 749.1 ± 2.0 Ma for K-feldspar granites. The gabbro-diorites are sodic and calc-alkaline rocks with low SiO2 (52.62–53.87 wt%), medium MgO (2.67–3.41 wt%), high Fe2O3T (7.18–7.49 wt%) and CaO (5.68–7.50 wt%) contents. They display high Th/Zr and Rb/Y ratios but low Nb/Zr and Nb/Y ratios. Together with their positive whole-rock εNd(t) (+1.0 to +1.5) and zircon εHf(t) values (+3.66 to +8.18), we suggest that these gabbro-diorites were derived from the partial melting of depleted lithospheric mantle modified by subduction-related fluids. The biotite granites display relatively high Sr contents (335–395 ppm), Sr/Y ratios (38.9–54.3), low Y (7.04–9.71 ppm) and Yb contents (0.78–1.08 ppm), resembling the adakitic granites. Their low Mg# (36–41) values, Cr (2.94–3.59 ppm) and Ni (1.32–1.55 ppm) contents as well as positive εNd(t) (+0.5 to +0.6) and εHf(t) values (+1.62 to +8.07) indicate that they were formed by partial melting of thickened juvenile mafic lower crust, probably within the existence of garnet. The K-feldspar granites have high SiO2 (76.61–77.14 wt%) and alkalis (Na2O + K2O = 8.55–9.69 wt%) contents, high 10,000 * Ga/Al (2.56–2.80) ratios and differentiation index (95.3–96.9), indicating the affinity to highly fractionated A-type granites. We suggest that these A-type granites were mainly generated by the partial melting of felsic crustal rocks under low pressure condition and subsequently extensive fractional crystallization is significant. Taking into account previous studies from the western Yangtze Block, South China, we