Jie Li

TL;DR: In this article, the authors showed that basaltic lavas from Hainan Island near the northern edge of the South China Sea have an age range between late Miocene (about 13 Ma) and Holocene, with a peak age of late Pliocene to middle Pleistocene.

TL;DR: In this article, the authors investigated the Hatu tholeiitic basalts and basaltic andesites of the western Junggar region, Central Asian Orogenic Belt (CAOB) LA-ICPMS zircon U-Pb analyses indicate that the huts were generated in the Late Carboniferous (~315 ǫ Ma) and the studied rock samples are characterized by flat rare earth elements pattern on chondrite-normalized plot, and negligible Nb, Ta and Ti anomalies on mid-ocean-ridge basalt normalized

TL;DR: In this paper, the authors presented new Pb, Sr, Nd, Pb and Os isotope data for the Hainan flood basalts, which have primitive Pb isotopic compositions that lie on, or very close to, 4.5- to 4.4-Ga geochrons on 207Pb/204Pb versus 206Pb /204PB diagram, suggesting a mantle source developed early in Earthʼs history (4.5−4.4 Ga).

TL;DR: In this paper, the authors presented new zircon LA-ICPMS U-Pb age, whole-rock major and trace element, Sr-Nd and Zircon Hf isotopic data for Late Mesozoic intermediate-felsic intrusive rocks in the Rena Co area in southern Qiangtang, central Tibet.

TL;DR: In this article, the authors reported the first Re-Os isotope data for the Late Permian Emeishan large igneous province (LIP) in Southwest China.