Adv Search
Volume 16 Issue 2
Apr.  2014
Turn off MathJax
Article Contents
Abstract
References
ZHOU Zhenhua. Brief Introduction of Output Features of Mineral Crystals in the Huanggang Skarn Sn-Fe Deposit,Inner Mongolia[J]. Journal of Gems & Gemmology, 2014, 16(2): 1-9.
Citation: ZHOU Zhenhua. Brief Introduction of Output Features of Mineral Crystals in the Huanggang Skarn Sn-Fe Deposit,Inner Mongolia[J]. Journal of Gems & Gemmology, 2014, 16(2): 1-9.
shu

Brief Introduction of Output Features of Mineral Crystals in the Huanggang Skarn Sn-Fe Deposit,Inner Mongolia

  • Institute of Mineral Resources, Chinese Academy of Geological Sciences;MLR Key Laboratory of Metallogeny and Mineral Assessment, Beijing 100037, China

More Information
  • Received Date: December 13, 2013
    Graphical Abstract
    • Abstract
  • The Huanggang skarn Sn-Fe deposit from Inner Mongolia is an important deposit in the southern section of the Daxing'anling metallogenic belt,where its metal mineral reserves is very large,and also contains fine mineral crystal resources with great value.Although the Huanggang Sn-Fe deposit hasAbstract:The Huanggang skarn Sn-Fe deposit from Inner Mongolia is an important deposit in the southern section of the Daxing'anling metallogenic belt, where its metal mineral reserves is very large, and also contains fine mineral crystal resources with great value. Although the Huanggang Sn-Fe deposit has received great international reputation due to its production of numerous precious mineral crystal specimens, it is rarely known in China. This paper gives a brief introduction of output features of the mineral crystals in the Huanggang deposit, focusing on the briefly description of the varieties and characteristics of the main output areas such as I,II,V districts. Mineral crystal is a new discipline, which has received wide attention in some foreign developed countries. In contrast, mineral crystal in China is still in the initial stage. Many precious mineral crystal specimens are destroyed or sold off due to ignorance of its value, which lead to huge losses. In the future, it needs to arouse public attention in order to make further development of the mineral crystal research, as well as collection land trade.
    • FullText(HTML)
    • References (32)
  • [1]
    Geijer P,Magnusson N H.The iron ores of Sweden[C] //Symposium sur le gisements de fer du monde:Internat.Geol.Congr.19th,Algiers,1952:477-499.
    [2]
    Magnusson N H.Iron and sulfide ores of central Sweden[C] //21th IGC,Copenhagen:Excursion Guides A26and C21,1960:1-48.
    [3]
    Einaudi M T,Meinert L D,Newberry R J.Skarn deposits[J].Economic Geology,75th Anniv.1981,76(2):317-391.
    [4]
    Meinert L D.Skarns and skarn deposits[J].Geoscience Canada,1992,19(4):145-162.
    [5]
    Meinert L D.Igneous petrogenesis and skarn deposits[J].Geol.Assoc.Canada Spec.Pap.,1993,40(2):569-583.
    [6]
    Misra K C.Understanding mineral deposits[M].Dordrecht:Kluwer Academic Publishers,2000:1-513.
    [7]
    Ahmed Z,Hariri M M.Formation and mineral chemistry of a calcic skarn from Al-Madhiq,SW Saudi Arabia[J].Chemie der Erde Geochemistry,2006,66(3-4):187-201.
    [8]
    Meinert L D,Dipple G M,Nicolescu S.World skarn deposits[J].Economic Geology,100th Anniversary Volume,2005,100(2):299-236.
    [9]
    赵一鸣.夕卡岩矿床研究的某些重要新进展[J].矿床地质,200,21(2):113-120,136.
    [10]
    赵一鸣,张德全.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M].北京:地震出版社,1997:135-137.
    [11]
    张德全,赵一鸣.大兴安岭及邻区铜多金属矿床论文集[M].北京:地震出版社,1993:1-147.
    [12]
    芮宗瑶,施林道,方如恒,等.华北陆块北缘及邻区有色金属矿床地质[M].北京:地质出版社,1994:1-558.
    [13]
    张永正,李秀荣,杨宏智,等.大兴安岭东南段铜多金属成矿构造条件[J].地质与资源,2007,16(1):38-41.
    [14]
    王之田,张树文.大兴安岭东南缘成矿集中区成矿演化特征与找矿潜力[J].有色金属矿产与勘查,1997,6(增刊):6-12.
    [15]
    徐毅.黄岗-甘珠尔庙成矿带多金属矿构造控矿特征分析[D].北京:中国地质大学,2005:1-75.
    [16]
    任耀武.大兴安岭中南段铜多金属矿床的重要矿源层[J].华北地质矿产杂志,1994,9(3):313-316.
    [17]
    任耀武.大兴安岭东坡南段大型铜矿成矿条件分析[J].黑龙江地质,1998,9(1):1-8.
    [18]
    白大明,刘光海.黄岗梁-乌兰浩特铜多金属成矿带区域综合找矿模式[J].物探与化探,1996,20(6):444-454.
    [19]
    王淼,范继璋,王忠文,等.内蒙古黄岗-甘珠尔庙成矿带铅锌矿综合信息找矿模型[J].地学前缘,2009,16(6):318-324.
    [20]
    冯建忠,艾霞,吴俞斌.内蒙古黄岗梁-孟恩陶勒盖矿带成矿地质特征及成矿模式[J].辽宁地质,1993,10(3):244-253.
    [21]
    赵一鸣,王大畏,张德全,等.内蒙古东南部铜多金属成矿地质条件及找矿模式[M].北京:地震出版社,1994:1-231.
    [22]
    Wang L J,Shimazaki H,Shiga Y.Skarn genesis of the Huanggang Fe-Sn deposit,Inner Mogolia,China[J].Resource Geology,2001,51(4):359-376.
    [23]
    周振华,刘宏伟,常帼雄,等.内蒙古黄岗锡铁矿床夕卡岩矿物学特征及其成矿指示意义[J].岩石矿物学杂志,2011,30(1):97-112.
    [24]
    周振华,吕林素,冯佳睿,等.内蒙古黄岗锡铁矿床辉钼矿Re-Os年龄及其地质意义[J].岩石学报,2010,26(3):667-679.
    [25]
    周振华,吕林素,杨永军,等.内蒙古黄岗锡铁矿区早白垩世A型花岗岩成因:锆石U-Pb年代学和岩石地球化学制约[J].岩石学报,2010,26(12):3 521-3 537.
    [26]
    Zhou Z H,Mao J W,Peter Lyckberg.Geochronology and isotopic geochemistry of the A-type granites from the Huanggang Sn-Fe deposit,Southern Great Hinggan Range,NE China:Implication for their origin and tectonic setting[J].Journal of Asian Earth Sciences,2012,49(30):272-286.
    [27]
    周振华,吕林素,王挨顺.内蒙古黄岗锡铁矿床花岗岩深部源区特征与构造岩浆演化:Sr-Nd-Pb-Hf多元同位素制约[J].地质科技情报,2011,30(1):1-14.
    [28]
    周振华,王挨顺,李涛,等.内蒙古黄岗锡铁矿床流体包裹体特征及成矿机制初步研究[J].矿床地质,2011,30(5):867-889.
    [29]
    李鹤年,段国正.黄岗式铁锡多金属矿床的成矿模式[J].世界地质,1988,7(2):17-28.
    [30]
    王莉娟,王京彬,王玉往,等.内蒙黄岗梁夕卡岩型铁锡矿床稀土元素地球化学[J].岩石学报,200,18(4):575-584.
    [31]
    周振华.大型国际矿物晶体展览会巡视[J].中国观赏石,2007(4):74-77.
    [32]
    刘光华.国际矿物收藏纵横谈[J].中国观赏石,2007(4):86-90.
    • Related Articles

Catalog

    Get Citation
    PDF
    XML

    Article Metrics

    Article views (125) PDF downloads (23) Cited by()
    Related
    Email alert RSS
    二维码

    Supported by Beijing Renhe Information Technology Co., Ltd.  Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return