铀矿地质
鈾礦地質
유광지질
URANIUM GEOLOGY
2015年
5期
517-523,535
,共8页
佟术敏%蔡建芳%杨文达%宁君%丁翠玲
佟術敏%蔡建芳%楊文達%寧君%丁翠玲
동술민%채건방%양문체%저군%정취령
宝龙山%局部补给区%局部排泄区%地下水类型%矿化度
寶龍山%跼部補給區%跼部排洩區%地下水類型%礦化度
보룡산%국부보급구%국부배설구%지하수류형%광화도
Baolongshan%local recharge and discharge area%groundwater type%TSD
宝龙山铀矿床水文地质条件比较复杂，文章概括了该区含水层及隔水层的基本情况，着重分析了含矿含水层及其隔水顶板的特征，简述了其与铀成矿的关系。依据该区的水文地球化学特征，尤其是矿化度、水化学类型及铀含量分布规律，说明了区内地下水整体流向由西南向东北方向；西辽河及架玛吐、兴隆协代花岗岩古隆起为地下水局部补给区， F3断裂、宝龙山剥蚀天窗及新开河为局部排泄区。
寶龍山鈾礦床水文地質條件比較複雜，文章概括瞭該區含水層及隔水層的基本情況，著重分析瞭含礦含水層及其隔水頂闆的特徵，簡述瞭其與鈾成礦的關繫。依據該區的水文地毬化學特徵，尤其是礦化度、水化學類型及鈾含量分佈規律，說明瞭區內地下水整體流嚮由西南嚮東北方嚮；西遼河及架瑪吐、興隆協代花崗巖古隆起為地下水跼部補給區， F3斷裂、寶龍山剝蝕天窗及新開河為跼部排洩區。
보룡산유광상수문지질조건비교복잡，문장개괄료해구함수층급격수층적기본정황，착중분석료함광함수층급기격수정판적특정，간술료기여유성광적관계。의거해구적수문지구화학특정，우기시광화도、수화학류형급유함량분포규률，설명료구내지하수정체류향유서남향동북방향；서료하급가마토、흥륭협대화강암고륭기위지하수국부보급구， F3단렬、보룡산박식천창급신개하위국부배설구。
Hydrogeological condition of Baolongshan uranium deposit is quite complex , by sumarrizing the condition of aquifer and inpermiable layer with the focus on their roof feature ,this article describes its relationship with uranium mineralization.Based on the study result of hydrogeochemical characteristics of this area such as of salinity , hydochemical type and the distribution of uranium content , the ground water was found flows from southwest to north east , and the uplift granite in Westliaohe and Jiamatu , Xinglong xiedai are regarded as local recharge area , while F3 fracture ,Baolongshan fenster and Xin‐kaiuhe are regarded as local discharge area.
