摘要
内蒙古乌拉特后旗阿勒特高勒金多金属矿位于内蒙古中部狼山—白云鄂博铜、铅、金、锌、铁、铂、镍多金属成矿带西段,该矿是在完成1∶5万区域矿产远景调查中通过化探异常查证发现的,金矿赋存于中元古界渣尔泰山群阿古鲁沟组,主要为一套浅变质碎屑岩建造,受NEE断裂构造控制,该金矿主要矿体赋存于地表长约1 km,宽约3~50m的褐铁矿化蚀变带中,蚀变带内石英脉发育。勘查区内圈定金矿体4条,深部钻探验证表明,矿体延深稳定。本文分析了阿勒特高勒金等多金属矿的矿床特征、控矿因素,总结了找矿标志,指出该区成矿潜力较大。
Wulatehouqi Aletegaole gold and other polymetallic ore are located in central Mongolia, western part of Langshan-Baiyun obo polymetallic metallogenic belt. This belt contained copper, lead, gold, zinc, iron,platinum, nickel and formed Huogeqi copper ore and Dongshenmiao lead zinc ore. The discovery of Aletegaole gold polymetallic ore enriched the mineral of Langshan-Baiyun obo polymetallic metallogenic belt. This gold mine hosted in Proterozoic Chaertaishan group Agulu ditch group, mainly builted for a set of shallow metamorphic clastic rocks. Because of controlled by the northeast fracture structure, the diggings encircled 4 ore bodies. It shows that the deepening of ore body is steady by the deeping exploration. The paper analysis the deposit characteristics and ore-controlling factors of Aletegaole gold and other polymetallic ore, summarizes the ore-prospecting marks, points out this diggings has large potential. In conclusion, this paper shows the direction for the prospecting and evaluating work of this diggings.
作者
王强
王若瞩
佘小龙
WANG Qiang WANG Ruo-zhu SHE Xiao-long(The Second Institute of Geology and Mineral Exploration, Gansu Provincial Bureau of Geology and Mineral Exploration and Development, Lanzhou 730000, Chin)
出处
《甘肃地质》
2016年第4期37-43,共7页
Gansu Geology
关键词
金多金属矿
矿体特征
找矿前景
乌拉特后旗
阿勒特高勒
gold polymetallic deposit
prospecting potential
Urad Houqi
Aletegaole
Inner Mongolia
作者简介
王强（1981-），男，助理工程师，主要从事野外地质调查工作。Email：119242324@qq．com
