矿床地质:2025,Vol.>>Issue(6):1209-1223

赣南新安钼矿床花岗闪长岩岩石地球化学、锆石U-Pb测年、Hf同位素研究及其意义
江西省地质局第七地质大队, 江西 赣州 341000;江西省地质局第七地质大队, 江西 赣州 341000;成都理工大学地球与行星科学学院, 四川 成都 610059;关键矿产资源勘查与开发江西省重点实验室, 江西 南昌 330000;江西省地质局, 江西 南昌 330000
Geochemical characteristics, U-Pb age and Hf isotope of zircons from granodiorite in Xin’an Mo deposit, southern Jiangxi Province and its significance
XIE Gang,LI Wei,CHEN BinFeng,PENG LinLin,LIAN DunMei
(The Seventh Geological Brigade of Jiangxi Bureau of Geology, Ganzhou 341000, Jiangxi, China;The Seventh Geological Brigade of Jiangxi Bureau of Geology, Ganzhou 341000, Jiangxi, China;College of Earth and Planetary Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China;Jiangxi Province Key Laboratory of Exploration and Development of Critical Mineral Resources, Nanchang 330000, Jiangxi, China;Jiangxi Bureau of Geology, Nanchang 330000, Jiangxi, China)
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投稿时间:2025-07-09   修订日期:2025-10-17      网络发布日期:2026-01-04
中文摘要:赣南新安钼矿床位于南岭成矿带与武夷成矿带交汇部位,是新探明的中型钼矿床。钼矿体主要产于花岗闪长岩与围岩侵入接触界线附近,以浸染型和细脉-浸染型钼矿化为主,具有斑岩型钼矿床矿化特征。花岗闪长岩地球化学分析显示,岩石具有高碱、富Al及贫Ti、Mg、P特征,属弱过铝质钙碱性岩类;轻重稀土分馏明显,Eu无异常,稀土配分曲线为右倾型。文章利用LA-ICP-MS锆石U-Pb定年方法测得花岗闪长岩年龄为162.5~170.9 Ma,谐和年龄为(165.4±0.3)Ma(MSDW=0.6),成岩时代属中侏罗世。锆石n(176Lu)/n(177Hf)=0.000 916~0.001 572,εHf(t)=−10.9~−5.5,二阶段模式年龄(TDM2)为1.56~1.90 Ga,显示其岩浆起源于古元古代地壳部分熔融,可能混有不同程度的幔源岩浆物质。综合分析认为,新安钼矿床成岩与成矿作用均发生于中侏罗世,是赣南新厘定的Mo成矿作用期,为区内钼矿找矿工作提出新方向。
Abstract:The Xin’an Mo deposit is a newly identified medium-sized Mo deposit in southern Jiangxi Province, which is located at the junction of the Nanling and Wuyi metallogenic belts. The disseminated and disseminated-veinlet Mo ore bodies are mainly distributed near the intrusive contact boundary between granodiorite and the surrounding rock, which has the mineralization characteristics of porphyry Mo deposit. The whole-rock geochemical analyses show that granodiorite has the features of week peraluminous, calc-alkali series, high Al2O3 and LREE contents, along with low TiO2, MgO, and P2O5 Values. The REE distribution curve shows a typical right-skewed distribution pattern. LA-ICP-MS Zircon U-Pb dating of granodiorite yields emplacement age of 162.5~170.9 Ma, with a concordia age of (165.4±0.3)Ma (MSWD=0.6), indicating the magmatic intrusion diagenesis occurred in the Middle Jurassic. The n(176Lu)/n(177Hf) and εHf(t) values are 0.000 916~0.001 572 and −10.9~−5.5, respectively, and TDM2 are 1.59 Ga~1.90 Ga, indicating primary reworking of the Paleoproterozoic crust with different degrees of mantle-derived magma material. The comprehensive analysis shows that the diagenesis and Mo mineralization in Xin’an Mo deposit both occurred during the Middle Jurassic, representing a newly defined Mo mineralization phase in southern Jiangxi Province. This provides a new direction for Mo prospecting work in this region.
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基金项目:本文得到江西省地质局青年科技带头人培养项目(编号:2024JXDZKJRC01)和国家重点研发计划项目(编号:2021YFC2901702)联合资助
引用文本:
谢刚,李伟,陈斌锋,彭琳琳,连敦梅.2025.赣南新安钼矿床花岗闪长岩岩石地球化学、锆石U-Pb测年、Hf同位素研究及其意义[J].矿床地质,44(6):1209~1223
XIE Gang,LI Wei,CHEN BinFeng,PENG LinLin,LIAN DunMei.2025.Geochemical characteristics, U-Pb age and Hf isotope of zircons from granodiorite in Xin’an Mo deposit, southern Jiangxi Province and its significance[J].Mineral Deposits44(6):1209~1223
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