Wechat
J4 ›› 2012, Vol. 20 ›› Issue (4): 104-108.
• article • Previous Articles Next Articles
LI Taibing,LI Yongguang,YI Jianchun
Received:
Revised:
Online:
Published:
Abstract:
Lengjiaxi strata in Quxi gold deposit with high initial gold background value,gold that is easily to be released was activated,migrated,and then precipitated,enriched in local area,due to metamorphism and tectonism.In Early Yanshanian,due to compression of the intra-continental subduction and collision,tectonic thermal event resulting in melting of diver deep or melting in the Lengjiaxi Group strata to form granite magma.Magma underplating along the deep fault intrusion,in the process of intrusion the deep fluid mixed with metamorphic water and meteoric water,and extract the mineral formation of gold in Lengjiaxi group,the hydrothermal bring gold migrate to construct favorable parts of the uninstall enrichment and mineralization.Lengjiaxi stratum provide gold material sources for the mineralization of Quxi gold deposit.While Granite not only provide the source of the gold material,but also provide thermal power for the mineralization.
Key words: Lengjiaxi group, Granite, Mineralization, Material source, Quxi gold deposit, Hunan Province
CLC Number:
LI Taibing,LI Yongguang,YI Jianchun. Discussion on the Mineralization and Material Sources of Quxi Gold Deposit in Hunan Province[J].J4, 2012, 20(4): 104-108.
0 / / Recommend
Add to citation manager EndNote|Reference Manager|ProCite|BibTeX|RefWorks
URL: http://www.goldsci.ac.cn/EN/
http://www.goldsci.ac.cn/EN/Y2012/V20/I4/104
[1] 涂光炽,王秀璋,陈远沛,等.中国层控矿床地球化学[M].北京:科学出版社,1984:1-350. [2] 刘英俊,孙承辕,马东升.江南金矿及其成矿地球化学背景[M].南京:南京大学出版社,1991:1-26. [3] 马东升,刘英俊.江南金成矿带层控金矿的地球化学特征与成因研究[J].中国科学(B辑),1991,(4):424-433. [4] 毛景文,李红艳.江南古陆某些金矿床成因讨论[J].地球化学,1997,26(5):71-81. [5] 毛景文.湖南万古地区金矿地质与成因[M].北京:原子能出版社,1997. [6] 毛景文,华仁民,李晓波.浅议大规模成矿作用与大型矿集区[J].矿床地质,1999,18(4):291-299. [7] 程国满.湘东赣西地区金矿矿源层的初步研究[J].黄金地质,1999,5(2):32-35. [8] 柳德荣,吴延之,刘石年.平江万古金矿床地球化学研究[J].湖南地质,1994,13(2):83-90. [9] 刘亮明,彭省临,吴延之.湘东北地区脉型金矿床成矿构造特征及构造成矿机制[J].大地构造与成矿学, 1997,21:197-204. [10] 刘亮明,彭省临,吴延之.湘东北地区脉型金矿床的活化转移[J].中南工业大学学报,1999,30(1):4-7. [11] 刘姤群,张录秀,金维群,等.湘东北燕山期花岗岩[J].华南地质与矿产,1999,(4):1-9. [12] 傅昭仁,李紫金,郑大瑜.湘赣边区NNE向走滑造山带构造发展样式[J].地学前缘,1999,(4):263-272. [13] 陈衍景.影响碰撞造山成岩成矿模式的因素及其机制[J].地学前缘,1998,(增):109-118.
Cited