Petrology, Chronology and Isotope Geochemistry of the Proterozoic Amphibolites from Xiangshan, Central Jiangxi Province, China

On the basis of a comprehensive study on the petrology, trace elements and isotopic geochemistry of the Xiangshan amphibolites, we suggest that the protoliths of the amphibolites were basalts formed in an island\|arc tectonic setting. The basaltic magma was derived from a slightly depleted mantle source with a small amount of crustal contamination. Assemblage of the rock\|forming minerals indicates that these amphibolites underwent a low\|grade metamorphism of amphibolite facies. According to the formation age (1113 Ma) and subsequent metamorphic age (726.6 Ma) of the basalts as well as the geological and geochemical features of these amphibolites, a tectonic model of Proterozoic oceanic island\|arc setting is proposed for central Jiangxi.