LAUSR

Abstract One highly disputed topic about the Jurassic igneous rocks in the eastern South China Block (SCB) is whether they were products of the Pacific plate subduction or the intra-continental extension of the SCB. The early Jurassic mafic rocks, which are regarded as important tracers for the mantle nature, geodynamic processes and tectonic setting, are of great importance to solve this controversy. This paper presents the detailed zircon U-Pb geochronological, elemental geochemical and Sr-Nd-Hf isotopic data for the Xialan gabbroic intrusion from the Eastern Nanling Range. SIMS zircon U-Pb dating results for olivine gabbro and hornblende gabbro yield weighted mean 206 Pb/ 238 U ages of 190.6 ± 1.3 Ma and 196.0 ± 2.7 Ma, respectively. Olivine gabbros are high in MgO, Mg-numbers and CaO and low in SiO 2 and depleted in LILEs and LREEs. They have significant Ba, Sr and Eu positive anomalies with e Nd (t) of +0.8 - +2.9, suggestive of their origination from an ancient lithospheric source. Hornblende gabbros have a wide compositional range of SiO 2 , MgO, Cr and Ni and are characterized by enrichment in LILEs and LREEs and insignificantly negative Nb-Ta anomalies, along with positive e Nd (t) values ranging from +1.7 to +6.2 and zircon e Hf (t) values from +9.7 to +12.7, indicative of their origination from the asthenosphere-lithosphere interaction. The estimated mantle potential temperature (1341–1407 °C) of hornblende gabbros is similar to that of the western Basin and Range Province (1350–1450 °C). In combination with the E-W-trending early Jurassic rock-association in the Nanling Range, it is herein proposed that the early Jurassic igneous rocks most likely formed in an intra-continental extension setting in response to the asthenospheric upwelling.