邓新根,华杰雄.浙江治岭头矿区Ⅰ号铅锌矿体地质特征及成因初探[J].矿产勘查,2010,1(5):458-462 |
浙江治岭头矿区Ⅰ号铅锌矿体地质特征及成因初探 |
Research on the characters and the genesis of the Pb-Zn orebody I in Zhilingtou mining zone, Zhejiang |
投稿时间:2010-05-17 |
DOI: |
中文关键词: 铅锌矿体 隐爆角砾岩 浙江 治岭头 |
英文关键词: Pb-Zn ore-body hidden-explosive rocks Zhejiang Zhilingtou |
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中文摘要: |
浙江省遂昌县治岭头矿区在中矿段金银矿勘探过程中发现Ⅰ号铅锌矿体,1997—2007年完成矿床详查工作。矿体产于燕山晚期火山通道隐爆形成的岩石中,赋存岩石为隐爆岩、爆裂角砾岩和爆破角砾岩,矿体呈筒状,平面上矿体呈不规则状,长度29.5~130 m,厚度11~58 m,矿体垂向延伸大于481 m,平均品位Pb+Zn 6.07%,伴生Ag、S、In、Cd等有用组分,属火山期后中低温隐爆岩型矿床,类型独特,对今后找矿有一定示范指导意义。 |
英文摘要: |
The Pb-Zn orebody I was discovered during exploration of the middle block of gold-silver deposit of Yetouling mine area, Suichang, Zhejiang provice. And its general exploration is done during 1997-2007. The orebody, in tube form, hosted by crytoexplosive, crtoexplosive breccia and explosive breccia formed in the volcanic conduit. It has an irregular shape in horizontal plane with its length of 29.5~130m, thickness of 11~58m. It extends for more than 481m in the perpendicular direction. the average grade of the Pb+Zn is 6.07% and with associated elements of Ag, S, In and Cd. It belongs to middle-temperature crytoexplosive type ore deposit and is meanfule for future exploration. |
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