中文摘要：

龙源坝复式岩体是南岭花岗岩带的重要组成部分，曾被作为其东侧燕山期陂头岩体的组成部分。最新研究表明，岩体的主体形成于印支期，在时代和成因上明显不同于陂头岩体。该印支期花岗岩与燕山期花岗岩和燕山期正长岩在主要氧化物成分上存在显著差别，暗示它们可能不存在结晶分异的演化关系。在微量元素特征上，印支期花岗岩稀土元素总量较高，富集轻稀土元素；燕山期花岗岩的稀土元素含量低，亏损中稀土，Th／U、Nb／Ta和Zr／Hf比值小，分馏明显，暗示岩浆作用过程中流体作用比较强烈；燕山期正长岩以富集高场强元素和稀土元素为特征，类似于A型花岗岩。锶、钕同位素地球化学特征表明，龙源坝复式岩体属于壳源S型花岗岩，起源于早元古代壳-幔分异产生的地壳。

英文摘要：

The Longyuanba composite pluton, located in the eastern part of the Nanling Range, is an important part of the Nanling granites belt, which was regarded as a portion of Yanshanian epoch Pitou pluton to the east of it, and was lowly studied. The newest research shows that, the main body of Longyuanba pluton formed in Indosinian, different from Pitou pluton, which is Yanshanian. From main elements geochemical characteristics, there is obvious gap between Indosinian granites, Yanshanian granites and Yanshanian syenites in major oxides composition, which implies that there is possibly no fractional crystallization relationship between them. Form trace element geochemical characteristics, Indosinian granites are enriched in LREE and high in EREE. Yanshanian granites are depleted in MREE and low in EREE and ratios of Th/U, Nb/Ta, Zr/Hf, and obvious in fraction. The above characteristics show that, liquid action was rather strong in Yanshanian magmatism. Yanshanian syenites are enriched in high field elements and REE, are similar with A-type granite. St, Nd isotopic geochemicial characteristics show that, Longyuanba composite pluton belongs to crust-original Stype granite, and its original resource is early-Proterozoic crust from crust-mantle fraction.