Abstract
Abstract Obvious differences in mineralization characteristics exist between the southern and northern parts of the eastern part of the Jiangnan Uplift in northern Jiangxi Province and southern Anhui Province. The regional metallogeny is discussed, and the ore‐forming fluid systems are classified in this article. It is proposed that the fluid ore‐forming activities in the Jiangnan Uplift both in northern Jiangxi and southern Anhui have close relationships with the crust‐mantle interaction and magmatic‐tectonic activities. The types and scales of the mineralization on the both sides of the eastern Jiangnan Uplift were determined by fluid ore‐forming systems and geological backgrounds.
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