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[an error occurred while processing this directive]Geological Characteristics and Ore-controlling Factors of Liyuan Gold Deposit, Shanxi Province
Received date: 2018-03-16
Revised date: 2018-09-04
Online published: 2019-01-24
Liyuan gold deposit is located in the tectonic-magmaic-polymetallic metallogenic belt of Taihang Mountain.The outcropping strata are mainly banded gneiss and amphibolite of Neo-Archean Fuping Group. The orebody is generally hand-shaped and mainly occurs in the NNE-trending structural zone.The metal minerals in ore are mainly pyrite,followed by galena,sphalerite and chalcopyrite.The non-metallic minerals are mainly quartz, potassium feldspar, plagioclase and sericite.The precious metal is natural gold (silver-gold ore). The wall-rock alteration closely related to gold mineralization are mainly silicification,sericitization and pyrite mineralization.The formation of the deposit can be divided into two episodes,including hydrothermal episode and epigenetic episode.The hydrothermal episode is the main mineralization period,which can be divided into four stages,namely,quartz silification stage,quartz-pyrite stage,quartz-sulfide stage and quartz-carbonate stage.Based on field geological survey and indoor analysis,the ore-bearing wall-rocks and strutural ore-controlling raw were summarized,the prospecting mark was specified,and the metallogenic process was preliminarily analyzed. It is considered that Liyuan gold deposit belongs to magmatic hydrothermal altered rock type gold deposit controlled by fracture zone.The results provide certain scientific basis for gold prospecting in this area.
Peijiao JU . Geological Characteristics and Ore-controlling Factors of Liyuan Gold Deposit, Shanxi Province[J]. Gold Science and Technology, 2018 , 26(6) : 706 -717 . DOI: 10.11872/j.issn.1005-2518.2018.06.706
| 1 |
许小平 .山西省灵丘县梨园金矿矿体赋存特征及成因浅析[J].华北国土资源,2009(3):3−5.
|
| 2 |
朱晓强,庞振山,甄世民,等 .山西灵丘梨园金矿床地质特征及认识[J].矿物学报,2015(增1):773.
|
| 3 |
鞠培姣,赖健清,杨洪基,等 .山西灵丘县梨园金矿流体包裹体特征及成矿作用[J].中国有色金属学报,2015,25(9):2537-2550.
|
| 4 |
朱晓强,庞振山,甄世民,等 .山西灵丘梨园金矿床流体包裹体特征[J].地质论评,2016,62(增1):149-150.
|
| 5 |
张春华 .河北太行山阜平期变质作用分析[J].中国区域地质,1987(2):121-127.
|
| 6 |
伍家善 .阜平群变质地质[M].北京:地质出版社,1989.
|
| 7 |
刘墩一,伍家善 .阜平群、五台群、滹沱群的界限年龄[J].中国地质研究院地质研究所所刊,1988,2:58-66.
|
| 8 |
王凯怡,李继亮,刘如琦 .阜平片麻岩之成因[J].地质科学,1991(3):254-266.
|
| 9 |
朱有光,蒋敬业 .金矿地球化学找矿[M].武汉:中国地质大学出版社,1993.
|
| 10 |
罗照华,邓晋福,赵国春,等 .太行山造山带岩浆活动特征及其造山过程反演[J].地球科学,1997,22(3):279-283.
|
| 11 |
马宝军,高风刚,牛树银,等 .冀西石湖金矿田构造控矿分析及成矿远景[J].黄金科学技术,2012,20(1):8-14.
|
| 12 |
朱亮璞 .太行山北段控岩控矿构造的遥感地质研究[J].国土资源遥感,1992(3):21-25.
|
| 13 |
陈桂华 .紫荆关断裂带构造活动特征——以太行山北段为例[D].北京:中国地质大学(北京),2003:1-28.
|
| 14 |
赵夫旺,高银仓,王建成 .浅议西石门—李家庄金矿区控矿因素[J].河北地质,2011(2):20-23.
|
| 15 |
张志军,李爱勤,李志国 .青海双朋西金铜矿床成矿控矿条件和成因分析研究[J].西部探矿工程,2013,25(1):121-123.
|
| 16 |
牛树银,陈超,孙爱群,等 .冀西石湖金矿成矿地质特征[J].黄金科学技术,2008,16(6):1-5.
|
| 17 |
陈超,牛树银,王宝德,等 .冀西石湖金矿成矿物质来源及成矿作用探讨[J].中国地质,2009,36(6):1340-1346.
|
| 18 |
曹烨 .冀西灵寿县石湖金矿床的矿物地球化学及深部远景预测[D].北京:中国地质大学(北京),2012.
|
| 19 |
高太忠,赵伦山,杨敏之 .山东牟乳金矿带成矿演化机理探讨[J].大地构造与成矿学,2001,25(2):155-160.
|
| 20 |
周利敏,张德会 .太行山北段王安镇—大河南岩体岩石地球化学特征及成因与成矿关系的探讨[J].矿床地质,2006,25(增):391-394.
|
| 21 |
杨殿范,李高山 .含矿岩体的评价标志——以太行山北段四个岩体为例[J].吉林地质,1994,13(2):22-28.
|
| 22 |
黄颖洲 .河北省石湖金矿矿床地质特征及控矿因素分析[D].长沙:中南大学,2008.
|
| 23 |
张亚雄,胡祥昭 .麻棚岩体特征及其与金矿成因关系研究[J].中南大学学报(自然科学版),1994,25(3):275-281.
|
| 24 |
吴迪,元凯军,门文辉,等 .石湖金矿区麻棚岩体主量元素地球化学特征[J].吉林大学学报(地球科学版),2015,45(1):527.
|
/
| 〈 |
|
〉 |