The Neoproterozoic tectonic evolution of the Jiangnan Orogen is controversial, with one of the issues being whether the ca. 850–820-Ma granitoids were generated by mantle plumes or the collision betwe
Zircon U–Pb ages and geochemical and isotopic data for Late Ordovician granites in the Baoshan Block reveal the early Palaeozoic tectonic evolution of the margin of East Gondwana. The granites are hig
Table S1 Zircon LA-ICP-MS analytical data for the studied sandstones of the Langxian Fm and Langjiexue Group in Jiacha-Jindong area, the eastern YZSZ.Table S2 Trace element concentrations of marble sa
Gases dissolved in molten rock (“magma”) leave the magma as it crystallizes to form solid, igneous rocks underground. Near Cloncurry in western Queensland, Australia, there is evidence in ancient rock
Major and trace element, zircon U–Pb and Hf-isotope data are reported for mafic intrusions and host granite from the Kachang pluton (North Yingjiang of SW Yunnan) in the Tengchong Terrane, in order to