首页|粤东隆文矽卡岩型铁锡多金属矿床成岩成矿时代及地球化学特征

粤东隆文矽卡岩型铁锡多金属矿床成岩成矿时代及地球化学特征

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隆文铁锡多金属矿床是东南沿海地区一处小型矽卡岩型铁锡矿床,位于粤东锡成矿带西北端,其成矿时代及成矿岩体岩浆演化过程尚不清楚.文章选择早阶段粗粒花岗岩、晚阶段细粒花岗岩及锡多金属矿石为研究对象,开展年代学与地球化学研究.结果显示,两阶段花岗岩锆石U-Pb年龄分别为(140.8±1.2)Ma、(140.7±1.4)Ma,锡石U-Pb年龄为(139.8±1.3)Ma、(140.8±1.8)Ma,成岩成矿时代为早白垩世;成矿岩体具有高硅、钙碱性及过铝质特征,呈现轻稀土元素微富集、重稀土元素平坦的配分模式,属于高分异Ⅰ型花岗岩;两阶段花岗岩具有负的全岩εNd(t)值和锆石εHf(t)值,Nd二阶段、Hf地壳模式年龄分别为1557-1621 Ma、1341~1811 Ma.结合粗粒花岗岩内暗色微粒包体,推断隆文花岗质岩浆主要来自早中元古代地壳物质的部分熔融,有少量地幔物质加入;与早阶段粗粒花岗岩相比,晚阶段花岗岩贫TFeO、MgO和TiO2,具有较高的Rb/Sr比值,较低的Nb/Ta和Zr/Hf比值.这表明晚阶段细粒花岗岩是早阶段粗粒花岗岩岩浆进一步分异演化的产物,是岩浆晶粥经过熔体-晶体的分离作用形成的,与锡成矿关系密切.
Geochronology and geochemistry of Longwen skarn-type iron-tin deposit in eastern Guangdong
The Longwen tin-iron polymetallic deposit is a small skarn-type tin-iron deposit located in the northwestern end of the eastern Guangdong tin metallogenic belt.The exact mineralization age and magmatic evolution process of ore-forming intrusion are still unclear.To shed light on this,we focused on the early-stage coarse-grained gra-nite,late-stage fine-grained granite,and skarn ore containing cassiterite for geochronological and geochemical studies.The results show that the zircon U-Pb ages of the two stages of granite are(140.8±1.2)Ma and(140.7±1.4)Ma,respectively.Similarly,the cassiterite U-Pb ages are(139.8±1.3)Ma and(140.8±1.8)Ma.These ages sug-gest that both the magmatic crystallization and tin polymetallic mineralization occurred during the Early Creta-ceous period.The ore-forming granites exhibit characteristics of high silica,calc-alkaline,and peraluminous com-position.They also show slight enrichment in light rare earth element(REE)and flat heavy REE distribution pat-terns,indicating that they belong to highly fractionated I-type granites.Both stages of granite exhibit negative whole-rock εNd(t)values and zircon εHf(t)values.The Nd two-stage and Hf crustal model ages range from 1557 to 1621 Ma and 1341 to 1811 Ma,respectively.Combined with the presence of dark microgranular enclaves in the coarse-grained granite,it is inferred that the Longwen granitic magma primarily originated from partial melting of Paleo-to Meso-Proterozoic crust with minor mantle and juvenile crust involvement.In comparison to the early-stage coarse-grained granite,the late-stage fine-grained granite is depleted in TFeO,MgO,and TiO2,and has high-er Rb/Sr ratio and lower Nb/Ta and Zr/Hf ratios.These differences suggest that the late-stage granite resulted from further differentiation of the early-stage granitic magma,through the extraction of melt from a crystal mush system.The fiine-grained granite is closely related to tin mineralization in the Longwen deposit.

skarncassiterite U-Pb ageI-type graniteLongwen iron-tin depositeastern Guangdong

张朋、马收先、陈懋弘、翟德高、柯昌辉、朱德全

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中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室 北京 100037

中国地质大学(北京),北京 100083

中冶武勘工程技术有限公司,湖北武汉 430080

山东省核工业二四八地质大队,山东青岛 266041

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矽卡岩 锡石U-Pb年龄 Ⅰ型花岗岩 隆文铁锡矿床 粤东

中国地质调查局地质调查项目中国地质调查局地质调查项目中国地质调查局地质调查项目

DD20201173DD20221684DD20240117

2024

矿床地质
中国地质学会矿床地质专业委员会 中国地质科学院矿床地质研究所

矿床地质

CSTPCD北大核心
影响因子:2.163
ISSN:0258-7106
年,卷(期):2024.43(5)
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