Methods for U-Pb, major, and trace element data of garnet, biotite, and plagioclase from the Bengbu uplift area, Northern China

The Bengbu uplift area is located at the southeast margin of the NCB, bounded to the east by the Tan-Lu fault zone and to the south by the Dabie orogenic belt. The Jingshan intrusion, situated in the western part of the Bengbu uplift, is considered a representative product of crustal anatexis during the Late Jurassic. This method contains LA-ICPMS, EPMA, SEM.