期刊文献+

浅析湖南九嶷山矿田锡矿类型及找矿方向 被引量:6

THE SHALLOW ANALYSIS OF TIN MINE AND LOOK FOR THE MINE DIRECTIONOF JIUYISHAN MINE AREA IN HUNAN
下载PDF
导出
摘要 湖南九嶷山矿田是南岭地区重要的锡矿成矿远景区之一,具有优越的成矿地质条件。锡矿类型较多,主要以云英岩体型、蚀变花岗岩型为主,具有矿体厚度大,蚀变强,品位中等,矿石利用性能好的特点。为了日后在本区找矿有更大的突破,通过研究区内控矿地质条件、主要矿床类型及时其特征,初步分析了区内矿床的找矿方向。认为燕山早期第一阶段晚期次及燕山早期第二阶段早期次侵入体与近南北向或北东向断裂带接触的部位,是寻找钨锡多属矿床的最有利的区段。 The Hunan jiuyishan mine area are one of important tin ore one-tenth mine distant view areas of Nan Ling district , and possess the superior one-tenth mine geology condition . The tin ore type is many , and it is major with Yun Yingyan' s type of figure and losing to become the ganite mould to give first place to , possessing mineral thickness greatly , losing becoming strong , the grade is medium , the good characteristic of ore utilization capability . Looking for the mine to have the bigger breakthrough in this area for , by way of accuse mine geology condition inside studying the area and major mineral deposit type his characteristic promptly , the mine direction is looked for in the initial analysis mineral deposit inside the area in the future . Thinking that Yanshan early stage stage 1 late period degree reaches Yanshan early stage stage in early stage more inferior incursion body easternly with closely northern and southern direction or east and north direction faces splitting taking the position of contact is seeks the tungsten tin much the most advantageous area of category mineral deposits section.
作者 龚述清
出处 《中国矿业》 北大核心 2007年第1期90-93,共4页 China Mining Magazine
基金 中国地质调查局大调查项目<湖南省九嶷山-姑婆山地区锡多金属矿评价>(项目编号:200310200070)
关键词 九嶷山矿田 锡矿 矿床类型 找矿方向 Jiuyishan mine area ,Tin mine ,The mineral deposit type ,Look for the mine direction
  • 相关文献

参考文献11

二级参考文献41

  • 1刘义茂,许继峰,戴橦模,李献华,邓希光,王强.骑田岭花岗岩^(40)Ar/^(39)Ar同位素年龄及其地质意义[J].中国科学(D辑),2002,32(z1):41-48. 被引量:163
  • 2庄锦良 刘钟伟 等.湘南地区小岩体与成矿关系及隐伏矿床预测[J].湖南地质,1988,(4):31-72.
  • 3赵日鉴.中国原生锡矿主要类型[A]..锡矿地质讲座会论文集[C].北京:地质出版社,1987.17~20.
  • 4朱金初.硅铝质熔浆体系中的水质流体[J].南京大学学报,1997,33:11-20.
  • 5姚金炎 吴明超.滇东南—桂东地区锡矿区域分布特点和找矿评价准则[J].矿产与地质,1988,:32-39.
  • 6Wood S A.The aqueous geochemistry of the rare-earth elements and yttrium:1.Review of the available low-temperature data for inorganic complexes and inorganic REE speciation in natural waters[J].Chem.Geol,1990,82,159-186.
  • 7Bau M.Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: Evidence from Y/Ho,Zr/Hf,and lanthanide tetrad effect[J].Contrib.Mineral.Petrol.,1996,123:323-333.
  • 8Irber W,Frster H J,Hecht L,et al.Experimental,geochemical,mineralogical and O-isotope constraints on the late-magmatic history of the Fichtelgebirge granites (Germany)[J].Geol.Rdsch,1997,86(Suppl.):110-124.
  • 9Bau M.The lanthanide tetrad effect in highly evolved felsic igneous rocks-a reply to a comment by Y Pan[J].Contrib. Mineral. Petrol.,1997,128:409-412.
  • 10Masau M,Cerny P,Chapman R.Dysprosian xenotime-(Y) from the Annie Claim #3 the granitic pegmatite,southern Manitoba, Canada:The evidence of the tetrad effect?[J].Canadian Mineralogist,2000,38:899-905.

共引文献136

同被引文献104

引证文献6

二级引证文献14

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部