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

Abstract

Abstract 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\u202f±\u202f2.0\u202fMa for gabbro-diorites, 800.3\u202f±\u202f2.1\u202fMa for biotite granites, and 749.1\u202f±\u202f2.0\u202fMa for K-feldspar granites. The gabbro-diorites are sodic and calc-alkaline rocks with low SiO2 (52.62–53.87\u202fwt%), medium MgO (2.67–3.41\u202fwt%), high Fe2O3T (7.18–7.49\u202fwt%) and CaO (5.68–7.50\u202fwt%) contents. They display high Th/Zr and Rb/Y ratios but low Nb/Zr and Nb/Y ratios. Together with their positive whole-rock eNd(t) (+1.0 to +1.5) and zircon eHf(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\u202fppm), Sr/Y ratios (38.9–54.3), low Y (7.04–9.71\u202fppm) and Yb contents (0.78–1.08\u202fppm), resembling the adakitic granites. Their low Mg# (36–41) values, Cr (2.94–3.59\u202fppm) and Ni (1.32–1.55\u202fppm) contents as well as positive eNd(t) (+0.5 to +0.6) and eHf(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\u202fwt%) and alkalis (Na2O\u202f+\u202fK2O\u202f=\u202f8.55–9.69\u202fwt%) contents, high 10,000\u202f*\u202fGa/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 propose that the gabbro-diorites, adakitic granites and A-type granites in this study were formed in persistent subduction process during the Neoproterozoic.