Reviews of geochronology, geochemistry, and geodynamic processes of Ordovician-Devonian granitic rocks in southeast China

Granite is the most important magmatic product during continental accretion and reworking, and is widely distributed at convergent margins. However, the formation of intracontinental granitic rocks remains unclear. The Early Paleozoic Wuyi-Yunkai orogen in southeast China is widely accepted as an intracontinental collision belt and has attracted significant attention in recent decades. Nevertheless, the tectonic driving mechanism for the...