广宁-罗定金矿带金矿成矿条件及预测

    MINEROGENETIC CONDITIONS AND PROSPECT OF GUANGNING-LUODING GOLD-ORE BELT IN GUANGDONG PROVINCE

    • 摘要: 广宁-罗定断裂带隶属于粤西地区云开加里东褶皱系云开隆起,是广宁-罗定金矿带的控矿断裂带,前人曾把它称为断裂带、断褶带、断裂变质带、推覆构造带.目前,该矿带内已发现金矿床(点)120余处.自1983年以来,发现了河台等一系列大中型金矿,引起了对此矿带基础地质和成矿条件研究工作的重视.从目前的研究看,广宁-罗定金矿带内的一系列金矿床(点)均赋存于广宁-罗定韧性剪切带内,严格受剪切带内强变形糜棱岩-初糜棱岩带控制.河台金矿床、塔岗金矿点均为河台型金矿床,产于含炭细碎屑岩系中的韧性剪切带内.金矿床形成于韧性剪切构造活动的晚期构造扩容阶段,与印支期伍村单元花岗质岩石的侵入有明显的成因联系.通过对金矿带内金矿成矿条件研究及河台金矿典型矿床研究,成功地圈定出塔岗地区为广宁-罗定金矿带内的又一个最具找矿远景的预测靶区.进一步的工程验证,求得F级金矿储量8234kg.

       

      Abstract: Guangning-Luoding fault belt in Yunkai uplift,Yunkai folding belt of Ca ledonian is a gold deposit-controlling fault belt,where more than 120 gold deposits have been found.The basic geology and minerogenetic conditions of gold deposits have been paid attention since 1983 when a series of large gold deposits,such as Hetai gold depositetc.were discovered.The gold deposits are all located in Guangning-Luoding ductile shear zone and distributed strictly in its mylonite-ultramylonite zones.Hetai and Tagang gold deposits are both the Hetai-type,of which the gold deposits formed in the dilatancy period of the ductile shear zone,genetically related to Wucun ultra-unit granitic intrusive rocks.With studying on the minerogenetic conditions and model deposit,some favorable areas are delineated.One of them is Tagang target,from which an F-degree reserves of 8234 kg gold is gained.

       

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