期刊文献+

缅甸太公当地区那田塘镍铬多金属矿化探异常特征与找矿潜力

The geochemical anomaly characteristics and prospecting potential of the Na ta lin Taung nickel-chromium polymetallic mineral in Taguang Taung,Myanmar
下载PDF
导出
摘要 那田塘镍铬多金属矿位于太公当-密支那成矿带最南端。中国有色桂林矿产地质研究院有限公司在该矿区开展地物化遥等地质工作。通过系统工作发现该区超基性岩发育,化探异常规模大、分带性好、浓集中心较明显,并且地表矿化较好,通过异常查证工作认为化探异常为矿致异常,该区有很大的找矿潜力。 The Na ta lin Taung nickel-chromium polymetallic deposit is located at the southernmost tip of the Taguang Taung-Myitkyina metallogenic belt.Geological Geophysical Geophysical and Remote Sensing work work was carried out in this mining area by China Nonferrous Metals(Guilin)Geology and Mining Co.Ltd.Through systematic work,it was discovered that the ultramafic rocks in the area developed,the geochemical exploration anomalies is large and zonation is very good,concentration center is very obvious,and the surface mineralization is good.The abnormality of the geochemical exploration was considered to be abnormal due to anomalies.The area has great prospecting potential.
作者 潘瀚 周守余 李学彪 宁庚陈 Pan Han;Zhou Shou-yu;Li Xue-biao;Ning Geng-chen(China Nonferrous Metals(Guilin)Geology and Mining Co.Ltd,Guilin 541004,China)
出处 《世界有色金属》 2018年第8期118-120,共3页 World Nonferrous Metals
关键词 镍铬多金属矿 化探异常 找矿潜力 缅甸 Ni Cr polymetallic ore geochemical anomaly prospecting potential Burma
  • 相关文献

参考文献2

二级参考文献27

  • 1付伟,牛虎杰,黄小荣.东南亚典型红土型镍矿床的成矿特征与找矿思路[J].矿物学报,2011,31(S1):774-775. 被引量:4
  • 2叶培盛,江万,吴珍汉,胡道功,刘琦胜.西藏泽当—罗布莎蛇绿岩的地球化学特征及其构造意义[J].现代地质,2006,20(3):370-377. 被引量:25
  • 3DESCHAMPS F,GODARD M,GUILLOT S,et al. Geochemis- try of subduction zone serpentinites : a review[-J]. Lithos, 2013, 178:96-127.
  • 4PRINZHOFER A,ALLEGRE C J. Residual peridotites and the mechanisms of partial melting[J]. Earth and Planetary Science Letters. 1985,74(2/ 3) :251-265.
  • 5PEARCE J, ROBINSON P T. The Troodo ophiolite complex probably formed in a subduction initiation, slab edge setting[J]. Gondwana Research, 2010,18(1) ;60-81.
  • 6MITCHELL A H G,HTAY M T,HTUN K M,et al. Rock re lationships in the Mogok metamorphic beh,Tatkon to Manda lay, central Myanmar[J]. Journal of Asian Earth Sciences 2004,23:321-341.
  • 7MITCHELL A H G,HTAY M T,HTUN K M,et al. Rock re lationships in the Mogok metamorphic belt,Tatkon to Manda lay,central Myanmar[J]. Journal of Asian Earth Sciences2007,29:891-910.
  • 8NIU Y L. Bulk-rock major and trace element compositions of abysal peridotites: Implications for mantle melting, melt extrac- tion and post-melting processes beneath mid-ocean ridges[J]. Journal of Petrology, 2004,45 (12) : 2423-2458.
  • 9PEARCE J A, LIPPARD S J, Roberts S. Characteristics and tec- tonic significance of supra-subduction zone ophiolites[J]//KOKE- LAAR B P, HOWELLS M F. Marginal basin geology. London: Geological Society of Special Publication, 1984,16 : 77-94.
  • 10PARKINSON I, PEARCE J. Peridotites from the Izu-Bonin- Mariana forearc ( ODP Leg125) : evidence for mantle melting and melt-mantle interaction in a supra-subduction zone setting [J]. Journal of Petrology,1998,39(9) :1577-1618.

共引文献1

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