The major tectonic zone that passes through the border regions of the Anhui,Zhejiang,and Jiangxi Provinces in southeast China has been commonly referred to as the Wan-Zhe-Gan fault zone. Geologically,this zone consists of several regional fault belts of various ages and orientations.We have categorized the faults into four age groups based on field investigations.The Neoproterozoic faults are northeast striking.They start from the northeast Jiangxi Province and extend northeastward to Fuchuan in Anhui Province,the same location of the northeast Jiangxi-Fuchuan ophiolite belt.The faults probably acted during the Neoproterozoic as a boundary fault zone of a plate or a block suture with melange along the faults.The nearly east-west- or east-northeast-striking faults are of Silurian ages(~(40)Ar/~(39)Ar age 429 Ma).This group includes the Qimen-Shexian fault and the Jiangwang-Jiekou ductile shear belt.They represent a major tectonic boundary in the basement because the two sides of the fault have clear dissimilarities.The third group of faults is north-northeast striking,having formed since the early-middle Triassic with ~(40)Ar/~(39)Ar ages of 230-254 Ma.They form a fault belt starting from Yiyang in northern Jiangxi and connect with the Wucheng as well as the Ningguo-Jixi faults.This fault belt is a key fault-magmatic belt controlling the formation of Jurassic-Cretaceous red basins,ore distribution,magmatic activity,and mineralization.When it reactivated during the late Cretaceous,the belt behaved as a series of reverse faults from southeast to northwest and composed the fourth fault group.Therefore,classifying the Wan-Zhe-Gan fault zone into four fault groups will help in the analysis of the tectonic evolution of the eastern segment of the Jiangnan orogen since the Neoproterozoic era. The major tectonic zone that passes through the border regions of the Anhui, Zhejiang, and Jiangxi Provinces in southeast China has been commonly referred to as the Wan-Zhe-Gan fault zone. Geologically, this zone consists of several regional fault belts of various ages and orientations. We have categorized the faults into four age groups based on field investigations. Neoproterozoic faults are northeast striking. The start from the northeast Jiangxi Province and extend northeastward to Fuchuan in Anhui Province, the same location of the northeast Jiangxi-Fuchuan ophiolite belt.The faults probably acted during the Neoproterozoic as a boundary fault zone of a plate or a block suture with melange along the faults.The nearly east-west- or east-northeast-striking faults are of Silurian ages (~ (40) Ar / ~ (39) Ar age 429 Ma). This group includes the Qimen-Shexian fault and the Jiangwang-Jiekou ductile shear belt. They represent a major tectonic boundary in the basement because the two sides of the fau lt has a clear dissimilarity. The third group of faults is north-northeast striking, having formed since the early-middle Triassic with ~ (40) Ar / ~ (39) Ar ages of 230-254 Ma. The form of a fault belt starting from Yiyang in northern Jiangxi and connect with the Wucheng as well as the Ningguo-Jixi faults. This fault belt is a key fault-magmatic belt controlling the formation of Jurassic-Cretaceous red basins, ore distribution, magmatic activity, and mineralization. during the late Cretaceous, the belt behaved as a series of reverse faults from southeast to northwest and composed the fourth fault group. agofore, classifying the Wan-Zhe-Gan fault zone into four fault groups will help in the analysis of the tectonic evolution of the eastern segment of the Jiangnan orogen since the Neoproterozoic era.