Geochemistry and zircon <scp>U–Pb</scp> dating of <scp>Early Jurassic</scp> syenogranite in the <scp>Kaoshan</scp> area, southern part of the <scp>Zhangguangcai Range</scp>, <scp>NE China</scp>, and tectonic implications

Abstract

Early Jurassic Kaoshan medium‐ and fine‐grained syenogranites emplaced along the Yitong–Shulan Fault Zone in the southern part the Zhangguangcai Range, central Jilin Province, intruded Middle Triassic granitoids and Carboniferous‐Devonian intrusive rocks. They have medium‐ and fine‐grained textures and contain K‐feldspar, quartz, plagioclase, and biotite. They are peraluminous (A/CNK = 1.13–1.20) and have high values of SiO 2 (74.60–75.82 wt%), total alkalis (Na 2 O + K 2 O = 8.28–9.18 wt%), light rare earth elements (20.89–56.14 ppm), large‐ion lithophile elements, and FeO/MgO = 2.78–5.93. In contrast, they feature low values of CaO (0.40–0.49 wt%), TiO 2 (0.05–0.14 wt%), P 2 O 5 (0.02–0.04 wt%), Sr (24.20–62.59 ppm), heavy rare earth elements (5.14–11.80 ppm), high‐field‐strength elements, and δEu (0.41–0.76), and the calculated zircon saturation temperatures (T zr ) range from 804 to 870°C, all of which are similar to the geochemical signatures of anorogenic A 1 ‐type granites. Zircon U–Pb geochronology analyses from the medium‐ and fine‐grained syenogranites yield concordia ages of 193.18 ± 0.95 Ma (MSWD = 6.7, n = 18) and 190.29 ± 0.92 Ma (MSWD = 8.7, n = 17), respectively, and belong to the Early Jurassic Sinemurian stage. In situ Hf isotope analyses of dated zircons yield ε Hf (t) values ranging from +17.0 to +9.7 and Hf model ages (T DM C ) of 225–614 Ma. Their whole‐rock ( 87 Sr/ 86 Sr) i (0.704740–0.704133) and ε Nd (t) values (+2.8 to +0.2) are similar to those of many coeval A 2 ‐type granites in this region, and they form an A‐type granite assemblage. Consequently, the Kaoshan medium‐ and fine‐grained syenogranites were probably derived from partial melting of juvenile lower crust and might be related to the subduction of the Palaeo‐Pacific Plate.