CAJ | 학술논문

　　本文研究了河南省登封刘楼重晶石矿床地质特征及控矿地质条件，并对矿床成因进行了分析。认为该区重晶石矿床类型为中、低温热液型脉状矿床，矿体赋存于寒武系中统张夏组碳酸盐地层中，矿体形态、规模及品位变化均受构造断裂带的控制。提出了找矿方向。
　　본문연구료하남성등봉류루중정석광상지질특정급공광지질조건，병대광상성인진행료분석。인위해구중정석광상류형위중、저온열액형맥상광상，광체부존우한무계중통장하조탄산염지층중，광체형태、규모급품위변화균수구조단렬대적공제。제출료조광방향。
Geological?characteristics?of?Liulou?barite?deposits?and?its?ore?controlling?geological?conditions?were?illustrated?and?deposit?genesis?was?initially?analyzed?in?the?paper.?It?is?believed?that?the?type?of?barite?deposit?in?the?area?is?low?to?moderate?temperature?hydrothermroal?vein?type?deposit?and?the?orebodies?occur?in?mid?Cambrian?Zhangxia?Group?carbonate?strata.?Shape?of?the?orebody,?scale?as?well?as?grade?variation?all?are?controlled?by?structure?zone.?Prospecting?direction?was?proposed?at?the?end.