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Major trace and rare earth elements of apatite and zircon U-Pb ages of ore-associated and barren granitoids from the Edong ore district South China

机译:中国南方鄂东矿区伴生及贫瘠花岗岩类的磷灰石和锆石U-Pb年龄的主要痕量和稀土元素

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摘要

The data in this article contains major, trace and rare earth element concentrations of apatite, and statistic analysis of apatite morphology in the granitoid rocks from the Edong ore district, South China, together with zircon U-Pb dating results for these rocks. Both the ore-associated and barren granitoids yield similar ages, including quartz diorite in the Fuzishan Cu-Au skarn deposit (138.6 ± 2.9 Ma), quartz monzodiorite in the Niutoushan Cu skarn deposit (137.8 ± 1.8 Ma), quartz diorite in the Ouyangshan Cu skarn deposit (138.4 ± 1.2 Ma), Liujiawan quartz monzodiorite (135.0 ± 2.4 Ma), and Bengqiaodi quartz monzodiorite porphyry (138.7 ± 1.1 Ma). Apatite occurs in all the minerals for each rock sample, and a detailed petrographic analysis shows the majority of them are early formed mineral phase. The F, Cl, SO3 contents in apatite are different, those in ore-associated rocks show higher values than barren ones. Li, Ni, Co, V contents are also higher in apatites from the ore-associated rocks than in barren rocks. Apatite (La/Sm)N and (Yb/Sm)N ratio show a positive correlation for ore-associated rocks but a negative correlation for barren rocks.
机译:本文中的数据包含了磷灰石的主要,痕量和稀土元素浓度,并对来自中国南方鄂东矿区的花岗岩岩石中的磷灰石形态进行了统计分析,以及这些岩石的锆石U-Pb测年结果​​。与矿石相关的和贫瘠的花岗岩类都具有相似的年龄,包括伏子山铜金矽卡岩矿床中的石英闪长岩(138.6±2.9 Ma),牛头山铜矽卡岩矿床中的石英闪长岩(137.8±1.8 Ma),欧阳山的石英闪长岩。铜矽卡岩矿床(138.4±1.2 Ma),刘家湾石英独生石(135.0±2.4 Ma)和本桥底石英独生石斑岩(138.7±1.1 Ma)。每个岩石样品的所有矿物中都存在磷灰石,详细的岩石学分析表明,其中大多数是早期形成的矿物相。磷灰石中的F,Cl,SO3含量不同,与矿石相关的岩石中的F,Cl,SO3含量高于贫瘠的岩石。与矿石相关的岩石中的磷灰石中的Li,Ni,Co,V含量也比贫瘠的岩石中的高。磷灰石的(La / Sm)N和(Yb / Sm)N比率与矿石相关的岩石呈正相关,而与贫瘠的岩石呈负相关。

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