Arc-continent collision between the Bainaimiao intra-oceanic arc and North China Craton facilitated the Late Ordovician climatic cooling and glaciation

Sample descriptions, analytical methods, LA-ICP-MS zircon U-Pb results, Hf isotopic, major-trace elemental compositions, detailed petrogenesis of the Early Paleozoic igneous rocks in the Bainiamiao arc system, and associated references.