|
|
Geological characteristics and metallogenic regularity of typical gold deposits in Fengtai ore concentration area, Shaanxi Province |
WANG Yingwei1,2, ZHAO Duanchang1,2, DU Biao1,2, ZHANG Zhenkai1,2 |
1. Shaanxi Institute of Geological Survey, Shaanxi Xi'an 710054, China; 2. Shaanxi Mineral Resources and Geological Survey, Shaanxi Xi'an 710068, China |
|
|
Abstract Fengtai ore concentration area is rich in gold resources, with great achievements and breakthrough from gold deposit detection in recent years. The authors in this paper summarized the metallogenic regularity in Fengtai ore concentration area through analysing and comparing the geological and ore-forming fluids characteristics of typical gold deposits. There are various types of gold mineralization in Fengtai ore concentration area, but properties and sources of ore-forming fluids and materials are unified. The ore-forming fluids with shallow metallogenic depth were mainly from atmospheric precipitation, while those with deep metallogenic depth were mainly from metamorphic fluid and magmatic hydrothermal fluid. The metallogenic environment of Pangjiahe gold deposit is medium and low temperature- low salinity- low density- medium hypabyssal, while the metallogenic environment of Baguamiao gold deposit is medium and high temperature-CO2 rich-medium and high salinity- medium plutonic. Besides, the metallogenic environment of Shuangwang gold deposit is medium and high temperature-CO2 rich-medium and low salinity-medium and high pressure-medium plutonic. The metamorphic fluid characteristics in these three gold deposits are obvious, with similar characteristics of orogenic gold deposits. The gold mineralization process in the study area was characterized by multi-period and multi-stage. And the gold mineralization was first pre-enriched by Au element in the strata, then mineralized with magmatic hydrothermal fluid, metamorphic hydrothermal fluid, and groundwater caused by the Indosinian (main metallogenic period) tectonic events. At last, the gold mineralization was superimposition reformed and enriched by the hydrothermal fluid during the Yanshanian.
|
Received: 11 November 2021
|
|
|
|
|
[1] 赵端昌,张振凯,杜彪,等.陕西凤太矿集区金成矿规律及找矿方向研究[R].西安:陕西省矿产地质调查中心,2021. Zhao D C,Zhang Z K,Du B,et al.Study on Gold Metallogenic Regularity and Prospecting Direction in Fengtai Ore Concentration Area,Shaanxi Province[R].Xi'an:Shaanxi Mineral Resources and Geological Survey,2021. [2] 陈衍景,张静,张复新,等.西秦岭地区卡林-类卡林型金矿床及其成矿时间、构造背景和模式[J].地质论评,2004,50(2):134-152. Chen Y J,Zhang J,Zhang F X,et al.Carlin and carlin-like gold deposits in western Qinling mountains and their metallogenic time,tectonic setting and model[J].Geol Rev,2004,50(2):134-152. [3] 王瑞廷,王涛,高章鉴,等.凤—太多金属矿集区主要金属矿床成矿系列与找矿方向[J].西北地质,2007,40(2):77-84. Wang R T,Wang T,Gao Z J,et al.The main metal deposits meta-llogenic series and exploration direction in Feng-tai ore cluster region,Shaanxi Province[J].Northwestern Geol,2007,40(2):77-84. [4] 王义天,王瑞廷,代军治,等.西秦岭凤太矿集区走滑双重构造及其控矿意义[J].矿物学报,2009,29(S1):188-189. Wang Y T,Wang R T,Dai J Z,et al.Strike slip dual structure and its ore controlling significance in Fengtai ore concentration area,West Qinling[J].Acta Mineral Sin,2009,29(S1):188-189. [5] 胡乔青.西秦岭凤太矿集区铅锌多金属矿床成矿作用特征、机制与成矿规律[D].北京:中国地质科学院,2015. Hu Q Q.The Mineralization Features,Mechanism and Metallo-genic Regularity of the Fengtai Pb-Zn Polymetallic Ore Cluster in West Qinling,China[D].Beijing:Chinese Academy of Geolo-gical Sciences,2015. [6] 刘方杰.秦岭泥盆纪凤太矿集区热水沉积金-多金属矿石建造的成矿建造分析及成矿模式研究[D].西安:西北大学,2001. Liu F J.The Minerotect Analysis and Metallogenetic Mode Stu-dying of the Hydrothermal Sedimentation Gold-polymetal Ore Formation in Fengtai Mine Gather Region in the Devonian in Qinling Orogen[D].Xi'an:Northwest University,2001. [7] 张亚峰,杨涛,易鹏飞,等.陕西省凤太矿田西部基础地质调查成果报告[R].陕西省矿产地质调查中心,2018. Zhang Y F,Yang T,Yi P F,et al.Report on Basic Geological Survey Results in the West of Fengtai Ore Field,Shaanxi Pro-vince[R].Shaanxi Mineral Resources and Geological Survey,2018. [8] 马健.陕西凤县庞家河地区金成矿作用过程及成因研究[D].武汉:中国地质大学(武汉),2018. Ma J.Ore-Forming Processes and Genesis of the Gold Deposits in Pangjiahe Region,Fengxian,Shaanxi Province[D].Wuhan:China University of Geosciences (Wuhan),2018. [9] 郑作平,于学元,郭键.八卦庙金矿地质及稳定同位素研究[J].陕西地质,1994(2):22-31. Zheng Z P,Yu X Y,Guo J.On the geology and stable isotope of the Baguamiao gold deposit[J].Geol Shaanxi,1994(2):22-31. [10] 邵世才,汪东波.南秦岭三个典型金矿床的Ar-Ar年代及其地质意义[J].地质学报,2001,75(1):106-110. Shao S C,Wang D B.39Ar-40Ar dating of the three typical gold deposits and its geological significance in the Southern Qinling region[J].Acta Geol Sin,2001,75(1):106-110. [11] 冯建忠,汪东波,王学明,等.陕西凤县八卦庙超大型金矿床成矿地质特征及成矿作用[J].地质学报,2003,77(3):387-398. Feng J Z,Wang D B,Wang X M,et al.Geology and metallogenesis of the Baguamiao giant gold deposit in Fengxian,Shaanxi Pro-vince[J].Acta Geol Sin,2003,77(3):387-398. [12] 张娟.陕西凤太矿集区八卦庙超大型金矿床成矿过程与成矿机制研究[D].北京:中国地质科学院,2016. Zhang J.Study of Mineralization Process and Mechanism in Baguamiao Super Large Gold Deposit,Fengtai Ore Region,Shaanxi,China[D].Beijing:Chinese Academy of Geological Sciences,2016. [13] 毛晨.南秦岭凤县地区金矿与铅锌矿成因研究[D].武汉:中国地质大学(武汉),2019. Mao C.Genesis of Gold and Lead-Zinc Deposits in Fengxian Area,South Qinling[D].Wuhan:China University of Geosciences (Wuhan),2019. [14] 严阵,许全成.陕西秦巴地区花岗岩类的时代及分期[J].陕西地质,1984(1):1-8. Yan Z,Xu Q C.The dating and phases of the granitoids in the area of the Qinling-Daba mountains within Shaanxi Province[J].Geol Shaanxi,1984(1):1-8. [15] 韦龙明,刘鸾玲,张选固.陕西八卦庙金矿金的赋存状态及其可选性研究[J].贵金属地质,1996,5(2):2-7. Wei L M,Liu L L,Zhang X G.Study on the gold occurrence state and the selectation in Baguamiao gold deposit[J].J Precious Metallic Geol,1996,5(2):2-7. [16] 张帆,刘树文,李秋根,等.秦岭西坝花岗岩LA-ICP-MS锆石U-Pb年代学及其地质意义[J].北京大学学报:自然科学版,2009,45(5):833-840. Zhang F,Liu S W,Li Q G,et al.LA-ICP-MS zircon U-Pb geo-chronology and geological significance of Xiba granitoids from Qinling,Central China[J].Acta Sci Nat Univ Pekinensis,2009,45(5):833-840. [17] 石准立,刘瑾漩,樊硕诚,等.陕西双王金矿床地质特征及其成因[M].西安:陕西科学技术出版社,1989. Shi Z L,Liu J X,Fan S C,et al.Geological Characteristics and Genesis of Shuangwang Gold Deposit in Shaanxi Province[M].Xi'an:Shaanxi Science and Technology Press,1989. [18] 范玉须,方维萱,李廷栋,等.陕西双王金矿钠长角砾岩锆石SHRIMP U-Pb年代学、岩石地球化学特征及其构造意义[J].地质学报,2018,92(9):1873-1887. Fan Y X,Fang W X,Li T D,et al.Zircon SHRIMP geochronology and geochemical characteristics of albite-carbonate breccia of Shuangwang gold deposit in Shaanxi Province and tectonic significance[J].Acta Geol Sin,2018,92(9):1873-1887. [19] 刘冲昊.陕西双王金矿床成矿机制与成矿规律[D].北京:中国地质大学(北京),2016. Liu C H.Metallogenic Mechanism and Regularity of the Shuangwang Gold Deposit,Shaanxi Province[D].Beijing:China University of Geosciences (Beijing),2016. [20] 宫勇军.陕西双王金矿床构造-流体系统及成矿机制研究[D].武汉:中国地质大学(武汉),2014. Gong Y J.The Study on the Tectonic-Fluid System and Metallogenic Mechanism of Shuangwang Gold Deposit in Shaanxi Pro-vince[D].Wuhan:China University of Geosciences (Wuhan),2014. [21] 张长年,陈丹玲.八卦庙金矿成矿物理化学条件研究[J].西北大学学报,1993,23(2):141-149. Zhang C N,Chen D L.An analysis of metallogenic physical-chemical condition of Baguamiao gold deposit[J].J Northwest Univ,1993,23(2):141-149. [22] 权志高,张万云.陕西凤县庞家河金矿床矿石自然类型划分及表生作用特征[J].矿产与地质,1996,10(4):240-244. Quan Z G,Zhang W Y.Supergenesis and classification of natural type of ores in the Pangjiahe gold deposit,Fengxian,Shaanxi[J].Mineral Resour Geol,1996,10(4):240-244. [23] 王颖维,赵端昌,杜彪,等.陕西凤县左家庄金矿床流体包裹体地球化学特征与成因[J].矿物学报,2022,42(1):71-82. Wang Y W,Zhao D C,Du B,et al.Geochemical characteristics of fluid inclusions and their implications for the genesis of the Zuo-jiazhuang gold deposit in Fengxian county,Shaanxi Province,China[J].Acta Mineral Sin,2022,42(1):71-82. [24] 韦龙明.陕西八卦庙金矿成矿流体初步研究[J].岩石学报,2007,23(9):2257-2262. Wei L M.Preliminary study on the ore-forming fluids of Baguamiao gold deposit,Shaanxi Province[J].Acta Petrol Sin,2007,23(9):2257-2262. [25] 王可新,王建平,刘家军,等.陕西太白双王金矿床地质特征及稳定同位素地球化学研究[J].中国地质,2012,39(5):1359-1374. Wang K X,Wang J P,Liu J J,et al.Geology and stable isotope geo-chemistry of the Shuangwang gold deposit in Taibai County,Shaanxi Province[J].Geol China,2012,39(5):1359-1374. [26] 王国富.陕西双王金矿床构造成矿作用及成矿预测研究[D].长沙:中南大学,2006. Wang G F.Researches on Tectono-Metallogenesis and Metallogenic Prognosis in Shuangwang Gold Deposit,Shaanxi Province,China[D].Changsha:Central South University,2006. [27] 张作衡,毛景文,李晓峰.双王角砾岩型金矿床地质地球化学及成矿机制[J].矿床地质,2004,23(2):241-252. Zhang Z H,Mao J W,Li X F.Geology,geochemistry and metallogenic mechanism of Shuangwang breccia type gold deposit[J].Miner Deposits,2004,23(2):241-252. [28] 权志高.陕西凤县庞家河金矿床基本地质特征及成矿作用分析[J].陕西地质,1996,14(2):43-52. Quan Z G.The metallogenesis and geological features of the Pang-jiahe gold deposit in Fengxian County,Shaanxi[J].Geol Shaanxi,1996,14(2):43-52. [29] Hoefs J.Stable Isotope Geochemistry[M].4th ed.Berlin:Springer-Verlag,1997:1-250. [30] 陈丹玲.八卦庙金矿床地质地球化学特征及成矿机制研究[D].西安:西北大学,1992. Chen D L.Study on Geology,Geochemistry and Metallogenic Mechanism of Baguamiao Gold Deposit[D].Xi'an:Northwest University,1992. [31] 何知礼,徐九华,谢玉玲,等.陕西太白金矿主矿段深部及东部成矿预测研究[R].北京:北京科技大学,1995:1-85. He Z L,Xu J H,Xie Y L,et al.Metallogenic Prediction of the Deep and Eastern Part of the Main Ore Section of Taibai Gold Deposit,Shaanxi Province[R].Beijing:University of Science and Technology,1995:1-85. |
[1] |
HONG Dajun, SONG Shiming, ZHANG Xu, CHEN Kefu, LIU Hong. Analysis of mineral prospecting potential in the periphery of Chating copper-gold mining area in Xuancheng City of Anhui Province[J]. , 2022, 9(3): 23-31. |
[2] |
HUANG Fan, WANG Denghong, WANG Yan, CHEN Yuchuan, ZHU Mingyu, CHEN Zhenghui, ZHAO Zhi, ZHAO Ruyi, GAO Yanfeng. Research and compilation progress of “Annals of Geology of Mineral Resources of China” (2018-2021)[J]. , 2022, 9(2): 1-14. |
[3] |
WU Kanglin, YANG Bin, ZHANG Zengqi, TIAN Jingxiang, XIAO Bingjian, LUO Wenqiang. A study of metallogenic regularity and geological characteristics of primary diamond deposits in Shandong Province[J]. , 2022, 9(2): 39-49. |
[4] |
FU Shengyun, CHEN Qiliang, DENG Lei. Geological characteristics and metallogenic regularity of lead-zinc-gold-silver polymetallic deposits in Hunan Province[J]. , 2022, 9(2): 50-62. |
[5] |
YUAN He, WANG Denghong. Metallogenic regularity and series of gold deposits in Liaoning Province[J]. , 2022, 9(2): 73-82. |
[6] |
HE Tianquan, LI Binbin, ZHANG Chunying. Geological characteristics and metallogenic model of phosphate deposit of Kunyang type in Sichuan Province[J]. , 2022, 9(2): 15-24. |
|
|
|
|