摘要
The Youdong granite, located in the central part of the southern Zhuguang granitic complex, is important uranium-bearing granite. It consists mainly of medium-grained, small porphyritic two-mica granite. SHRIMP U-Pb dating of zircon collected from the granite yields an age of (232±4) Ma (MSWD=3.2), indicating it was the product of granitic magmatic activity in the early Indosinian epoch. Under the tectonic settings, the Youdong granite was formed by partial melting of Paleoproterozoic-Mesoproterozoic argillaceous and arenaceous rocks in the intermediate-lower crust sources under the influence of lithosphere thinning and asthenosphere ascending.