中文摘要：

江西省相山火山盆地是我国第一大、世界第三大火山岩型铀矿田，其西部牛头山一带铀矿勘探中发现深部有大垂幅的Pb—Zn-Ag矿化．60多年来，以该矿田为对象开展的研究取得了一系列丰硕成果，但对火山机构的认识仍不确定．我们采集了涵盖该火山盆地主要地质体的1386块钻孔岩芯标本和243块地表岩石标本，开展了电阻率、磁化率、密度等物性参数测量，并在火山盆地中施测了19条MT剖面（2条骨干剖面和17条精细剖面），对3000m以浅主要地层、岩体和断裂带等目标地质体的三维展布特征进行了解译和三维建模．研究结果表明：（1）相山火山盆地具有变质岩-花岗岩双基底．基底变质岩系顶界面表现为南北分带（三隆间两凹）和东西分块（两垒夹一堑）的三维地质格局；南西部有加里东期花岗岩侵入，具有似层状的空间展布特征；盆地基底变质岩系与上覆火山-沉积岩盖层之间呈连续的水平低阻异常带，不整合界面清晰．（2）打鼓顶组火山岩呈似层状产出，主要分布于盆地西部；在河元背-船坑-杏树下-带识别出近东西走向厚层的流纹英安岩凹槽，相山铀矿田西部探明的主要铀矿床分布在该凹槽内或其边缘．鹅湖岭组火山岩总体形态呈蘑菇状，在盆地中部厚度较大．在相山主峰半径约2km的范围内，发现自下而上贯通式的低阻异常，推测是鹅湖岭组碎斑熔岩喷发的通道相（火山颈相），其火山颈呈陡立管状，深部向南东倾伏，浅部向南东撒开．后期花岗斑岩呈岩墙-岩床组合状，总体构成一个向西开口的环形岩体．打鼓顶期主要岩浆通道位于相山顶-巴山之间，次岩浆通道位于河元背；鹅湖岭期火山活动主岩浆通道也位于相山顶-巴山之间，次岩浆通道位于河元背、阳家山（芙蓉山）、严坑和柏昌．（3）火山盆地中断裂构造发育，MT测量结

英文摘要：

Xiangshan volcanic basin, the third largest volcanic-type uranium ore field in the world, attracts great research interests and a large amount of industry investment all the time. There is a broad consensus of opinion amongst the scientists about the basin which should be a Pb-Zn and Ag bearing ＂three-storeyed type＂ model, known as ＂under the uranium mineralized volcanic rocks＂. However, over the past 60 years and more, the geological structure of volcanic calderas is still not confirmed because of the uncertain pathways of U-Pb-Zn-Ag-bearing fluid. Based on 1386 samples of physical property measurement and 19 profiles of Magnetotelluric （MT） detection, MT sounding and GOCAD modeling were adopted to study the geological structure of volcanic calderas. The results indicate that. （1） it has double bases of Metamorphic base and Caledonian granite base in the volcanic basin. Between the basement metamorphic rocks and the overlying volcanic-sedimentary rocks there is a clear unconformity interface of low resistivity anomaly zone. （2） Daguding Formation mainly shows a stratified distribution in the west, Ehuling Formation displays a mushroom shape of low resistivity anomaly in Xiangshan Peak with a radius of almost 2 km. （3） According to the results of MT inversion, and the large scale of arc volcanic collapsed structure with low resistivity in the northern basin, seven North- East-strike, four North-West-strike and one North-South-strike faults are interpreted in the basin.