矿产保护与利用
礦產保護與利用
광산보호여이용
CONSERVATION AND UTILIZATION OF MINERAL RESOURCES
2013年
6期
13-18
,共6页
伏彦雄%戈保梁%童雄%李青%张晋禄
伏彥雄%戈保樑%童雄%李青%張晉祿
복언웅%과보량%동웅%리청%장진록
砂岩型铜矿%工艺矿物学%赋存状态
砂巖型銅礦%工藝礦物學%賦存狀態
사암형동광%공예광물학%부존상태
sandstone copper%process mineralogy%occurrence
针对某低品位砂岩型铜矿进行工艺矿物学研究,结果表明,该铜矿石矿物成分复杂,原生硫化铜矿物为黝铜矿、黄铜矿,次生硫化铜矿物为斑铜矿、辉铜矿、蓝铜矿;氧化铜矿物主要为孔雀石;脉石矿物以石英、白云母、高岭土、绢云母为主。原矿含铜0.77%,氧化率为45.45%,为一氧化不彻底的氧化铜矿石。矿石中存在着一部分嵌布粒度较细的铜矿物。由于部分硫化铜矿物常和白云石、黄铁矿共生,部分氧化铜矿物常与褐铁矿互相浸染,因此选择合理的磨矿细度,使细粒嵌布的铜矿物充分单体解离是本矿石获得较好选矿指标的关键。
針對某低品位砂巖型銅礦進行工藝礦物學研究,結果錶明,該銅礦石礦物成分複雜,原生硫化銅礦物為黝銅礦、黃銅礦,次生硫化銅礦物為斑銅礦、輝銅礦、藍銅礦;氧化銅礦物主要為孔雀石;脈石礦物以石英、白雲母、高嶺土、絹雲母為主。原礦含銅0.77%,氧化率為45.45%,為一氧化不徹底的氧化銅礦石。礦石中存在著一部分嵌佈粒度較細的銅礦物。由于部分硫化銅礦物常和白雲石、黃鐵礦共生,部分氧化銅礦物常與褐鐵礦互相浸染,因此選擇閤理的磨礦細度,使細粒嵌佈的銅礦物充分單體解離是本礦石穫得較好選礦指標的關鍵。
침대모저품위사암형동광진행공예광물학연구,결과표명,해동광석광물성분복잡,원생류화동광물위유동광、황동광,차생류화동광물위반동광、휘동광、람동광;양화동광물주요위공작석;맥석광물이석영、백운모、고령토、견운모위주。원광함동0.77%,양화솔위45.45%,위일양화불철저적양화동광석。광석중존재착일부분감포립도교세적동광물。유우부분류화동광물상화백운석、황철광공생,부분양화동광물상여갈철광호상침염,인차선택합리적마광세도,사세립감포적동광물충분단체해리시본광석획득교호선광지표적관건。
In this thesis the object of study is a low grade sandstone copper with complex composi -tion.The results of the process mineralogy research showed that the primary sulfide copper minerals are tetrahedrite and chalcopyrite while the secondary sulfide copper minerals are bornite ,chalcocite and azurite .The main oxide copper mineral is malachite and the main gangue mineral is quartz . The grade of copper is 0 .77%and the oxidation rate is 45 .45%in the run of mine .There is a part of copper mineral particles disseminated relatively fine .As the copper minerals often intergrow with dolomite and pyrite and the oxide copper minerals are often blended with limonite ,the key of obtai-ning the good flotation index is a reasonable grinding fineness to ensure full liberation of the fine -disseminated copper mineral particles .