广西锑矿成矿规律研究

doi:10.19388/j.zgdzdc.2022.02.03

Abstract
Figure/Table
References
Related Citation (15)

Download: PDF (7199 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Guangxi antimony deposits resources are rich, which have become one of the dominant minerals in Guangxi. In order to investigate its metallogenic regularity, the authors of this paper have comprehensively summarized the Guangxi antimony deposits exploration, development, resource distribution, deposit genesis, spatial distribution characteristics and metallogenic regularity. The antimony deposits in Guangxi are divided into three genetic types, including magmatic hydrothermal type, epigenetic middle-low temperature hydrothermal type and weathering type, among which the magmatic hydrothermal type is the main type. 7 fourth-order genetic types are divided on the basis of the third-order genetic types, among which the compound cassiterite-sulfide antimony deposits are the largest, and most closely related to magmatic hydrothermal mineralization. In addition, the Guang-xi antimony distribution and enrichment are jointly controlled by the four in one, including the strata, structure, magmatic rocks and contact zone. These antimonies were mainly enriched in Dianqiangui passive continental margin tectonic units and Xiangzhong-Northern Guizhong (depression) metallogenic belt, and the antimony deposits with industrial value mainly occur in the Devonian system, which burst in Late Yanshanian.

Key words： antimony deposits genetic type metallogenic regularity metallogenic age Guangxi

Received: 26 January 2022

ZTFLH:	P618.66
	P612

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	WANG Gongmin
	WANG Chuanjian
	ZHOU Jianfei
	GUAN Xiaoyi
	HUANG Baoan
	PANG Caixin
	JIANG Zhilong

Cite this article:

WANG Gongmin,WANG Chuanjian,ZHOU Jianfei, et al. Research of metallogenic regularity of antimony deposits in Guangxi[J]. , 2022, 9(2): 25-38.

URL:

http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2022.02.03 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2022/V9/I2/25

[1] 王永磊,徐珏,张长青,等.中国锑矿成矿规律概要[J].地质学报,2014,88(12):2208-2215.
Wang Y L,Xu J,Zhang C Q,et al.Summary of metallogenic regularities of antimony deposits in China[J].Acta Geol Sin,2014,88(12):2208-2215.
[2] 丁建华,杨毅恒,邓凡.中国锑矿资源潜力及成矿预测[J].中国地质,2013,40(3):846-858.
Ding J H,Yang Y H,Deng F.Resource potential and metallogenic prognosis of antimony deposits in China[J].Geol China,2013,40(3):846-858.
[3] 广西自然资源厅.广西矿产资源储量数据库管理系统[R].南宁:广西自然资源厅,2018.
Guangxi Department of Natural Resources.Mineral Resources Reserve Database Management System in Guangxi[R].Nanning:Guangxi Department of Natural Resources,2018.
[4] 中国矿产地质志项目办公室,中国地质科学院矿产资源研究所.中国矿产地质志(省级矿产地质志研编技术要求)[M].北京:中国矿产地质志项目办公室,2016.
Project Office of China Mineral Geology,Institute of Mineral Resources,Chinese Academy of Geological Sciences.Technical Requirements of Provincial Geological Survey of Mineral Resources in China[M].Beijing:Project Office of China Mineral Geology,2016.
[5] 广西有色地质勘查局二七〇地质队.广西罗城县黑刚锑矿普查报告[R].广西融水:广西有色地质勘查局二七〇地质队,1992.
The 270 Geological Team of Guangxi Non-ferrous Geological Exploration Bureau.Antimony Mine Survey Report of Heigang of Luocheng in Guangxi[R].Guangxi Rongshui:The 270 Geological Team of Guangxi Non-ferrous Geological Exploration Bureau,1992.
[6] 张清,卜国基,农强,等.广西壮族自治区南丹县大厂锡多金属矿田巴力—龙头山矿区锡多金属矿资源储量核实报告[R].南丹:广西二一五地质队,2008.
Zhang Q,Bu G J,Nong Q,et al.Verification Report of Tin-polymetallic Mineral Resources and Reserves of Ba Li-Long Toushang of Tin-polymetallic Ore Field of Dachang in Nandang,Guangxi[R].Nandan:Guangxi 215th Geological Team,2008.
[7] 王思源.芒场矿田锡多金属成矿构造解析[J].地球科学:中国地质大学学报,1990,15(4):421-430,440.
Wang S Y.Metallotectonic analysis for tin-multimetal deposits of strata-bound type[J].Earth Sci J China Univ Geosci,1990,15(4):421-430,440.
[8] 童加松,黄子义,魏彭寿,等.广西南丹县芒场矿田大山锡多金属矿床详查地质报告[R].柳州:广西第七地质队,1990.
Tong J S,Huang Z Y,Wei P S,et al.Detailed Geological Report of the Tin-polymetallic Deposit of Dashang of Ore Field of Mang Chang in Nandang,Guangxi[R].Liuzhou:Guangxi 7th Geological Team,1990.
[9] 李容光.广西南丹县大厂锡多金属矿田茶山锑钨矿区28号脉详查报告书[R].南丹:广西二一五地质队,1987.
Li R G.Detailed Survey Report of Vein No.28 in Antimony and Tungsten Ore Area of Chashang of Tin-polymetallic Ore Field of Dachang in Nandan,Guangxi[R].Nandan:Guangxi 215th Geological Team,1987.
[10] 赵京.广西五圩铅锌锑多金属矿田成矿分带特征及找矿预测研究[D].南宁:广西大学,2015.
Zhao J.The Metallogenic Zoning Characteristics and Prospecting Prediction of Wuxu Lead-zinc-antimony Polymetallic Ore Field,Guangxi[D].Nanning:Guangxi University,2015.
[11] 贺光照.广西河池五圩多金属矿区三排洞、芙蓉厂、箭猪坡矿床地质普查报告[R].南宁:广西地质资料馆,1976.
He G Z.Geological Survey Report of Sanpaidong、Furongchang、Jianzhupo of Wuxu Polymetallic Mining Area of Hechi in Guang-xi[R].Nanning:Guangxi Geological Archive,1976.
[12] 徐立春.广西贵、横、宾阳县镇龙山银锑多金属矿区普查地质报告[R].南宁:广西地质资料馆,1976.
Xu L C.Geological Report of Ag-Sb Polymetallic Mining Area of Zhenglongshan of Gui、Heng、Bingyang in Guangxi[R].Nanning:Guangxi Geological Archive,1976.
[13] 尹朝斗.广西壮族自治区隆林县坡岩锑矿区勘探地质报告[R].南宁:广西地质资料馆,1989.
Yin C D.Report on Exploration Geology of Antimony Deposit of Poyan of Longlin in Guangxi[R].Nanning:Guangxi Geological Archive,1989.
[14] 陈毓川,王登红,朱裕生,等.中国成矿体系与区域成矿评价[M].北京:地质出版社,2007.
Chen Y C,Wang D H,Zhu Y S,et al.Metallogenic Regularity and Prospecting Direction of Zhaishang Gold Deposit,Shandong Pro-vince[M].Beijing:Geological Publishing House,2007.
[15] 徐志刚,陈毓川,王登红,等.中国成矿区带划分方案[M].北京:地质出版社,2008.
Xu Z G,Chen Y C,Wang D H,et al.Division Scheme of Metallogenic Zones in China[M].Beijing:Geological Publishing House,2008.
[16] 陈毓川,王登红,徐志刚,等.全国重要矿产和区域成矿规律研究技术要求[M].北京:地质出版社,2010.
Chen Y C,Wang D H,Xu Z G,et al.Technical Requirements for Research on Metallogenic Regularity of Important Minerals and Regions in China[M].Beijing:Geological Publishing House,2010.
[17] 陈毓川,王登红,李厚民,等.重要矿产预测类型划分方案[M].北京:地质出版社,2010.
Chen Y C,Wang D H,Li H M,et al.Classification Scheme of Important Mineral Prediction Types[M].Beijing:Geological Publishing House,2010.
[18] 陈毓川,毛景文.桂北地区矿床成矿系列和成矿历史演化轨迹[M].南宁:广西科学技术出版社,1995:200-410.
Chen Y C,Mao J W.Metallogenic Series and Evolution Track of Ore Deposits in North Guangxi[M].Nanning:Guangxi Science and Technology Press,1995:200-410.
[19] 陈毓川,毛景文,王平安.桂北地区金属矿床成矿历史演化程式[J].地质学报,1994,68(4):324-338.
Chen Y C,Mao J W,Wang P A.The evolutionary history of metallic deposits in Northern Guangxi,China[J].Acta Geol Sin,1994,68(4):324-338.
[20] 彭建堂,胡瑞忠.华南锑矿带的成矿时代和成矿构造环境[J].地质地球化学,2001,29(3):104-108.
Peng J T,Hu R Z.Metallogenic epoch and metallogenic tectonic environment of antimony deposits,South China[J].Geol Geochem,2001,29(3):104-108.
[21] 何海洲.桂北黑刚地区锑矿地质特征及控矿条件[J].有色金属矿产与勘查,1996,5(1):34-41.
He H Z.Geological features and ore-controlling factors of the antimony deposits in the Heigang District,Northern Guangxi[J].Geol Expl Non-Ferr Met,1996,5(1):34-41.
[22] 蔡明海,梁婷,韦可利,等.大厂锡多金属矿田铜坑—长坡92号矿体Rb-Sr测年及其地质意义[J].华南地质与矿产,2006(2):31-36.
Cai M H,Liang T,Wei K L,et al.Rb-Sr dating of the No.92 orebody of the Tongkeng-Changpo deposit in the Dachang tin-polymetallic ore field,Guangxi,and its significance[J].Geol Mineral Res South China,2006(2):31-36.
[23] 梁婷,王登红,李华芹,等.广西大厂石榴石REE含量及Sm-Nd同位素定年[J].西北大学学报:自然科学版,2011,41(4):676-681.
Liang T,Wang D H,Li H Q,et al.REE Geochemistry and Sm-Nd isotope Age of Garnet from the Dachang,Guangxi[J].J Northwest Univ:Nat Sci Ed,2011,41(4):676-681.
[24] 邹锡青,王思源.广西芒场锡多金属矿田稳定同位素组成对矿床成因探讨[J].广西地质,1993,6(2):63-68.
Zou X Q,Wang S Y.Discussion on stable isotopic composition and genesis of Mangchang tin-polymetallic Orefield,Guangxi[J].Guangxi Geol,1993,6(2):63-68.
[25] 王东明.广西丹池成矿带锑矿成矿特征及成因探讨[D].西安:长安大学,2012:82-90.
Wang D M.A Study on the Characteristic and Origin of the Antimony Deposit in Danchi Metallogenic Belt,Guangxi[D].Xi'an:Chang'an University,2012:82-90.
[26] 胡乔帆,刘伟,安玉伟,等.广西河池箭猪坡铅锌锑矿地质地球化学特征及矿床成因[J].地质论评,2017,63(S1):47-48.
Hu Q F,Liu W,An Y W,et al.The geological geochemical chara-cteristics and ore genesis of Jianzhupo Pb-Zn-Sb deposit in Hechi of Guangxi[J].Geol Rev,2017,63(S1):47-48.
[27] 陈玲,黄文婷,伍静,等.广西五圩矿田成矿温度变化及找矿方向分析[J].地球化学,2015,44(6):546-555.
Chen L,Huang W T,Wu J,et al.Ore-forming temperature variation and prospecting target of the Wuxu ore field in Guangxi[J].Geochimica,2015,44(6):546-555.
[28] 成涵.广西南丹县罗富锑矿床地质特征和成矿预测[D].长沙:中南大学,2014:28-30.
Cheng H.Study on Geological Characteristics and Metallogenic Prediction of Luofu Antimony Deposit,Nandan,Guangxi[D].Changsha:Central South University,2014:28-30.
[29] 王葆华,曾南石,欧阳菲,等.广西镇龙山—龙山金(银)多金属成矿带的成矿规律及找矿方向研究[J].矿床地质,2012,31(S1):39-40.
Wang B H,Zeng N S,Ouyang F,et al.Study on metallogenic regularity and prospecting direction of Gold (silver) polymetallic metallogenic belt of Zhenglongshan-Longshang in Guangxi[J].Miner Depos,2012,31(S1):39-40.
[30] 韦文灼.马雄锑矿床地质特征[J].西南矿产地质,1993,7(2):8-16.
Wei W Z.Geological characteristics and prospecting potential of stibnite deposit in Hunan Province[J].Southwest Mineral Geology,1993,7(2):8-16.
[31] 王国田.桂西北地区三条铷-锶等时线年龄[J].广西地质,1992,5(1):29-35.
Wang G T.Three strontium and rubidium isotime ages in North-west Guangxi[J].Guangxi Geol,1992,5(1):29-35.
[32] 余勇,李晓峰,肖荣,等.广西珊瑚钨锡矿田锆石U-Pb和绢云母⁴⁰Ar/³⁹Ar年龄及其地质意义[J].矿物学报,2014,34(3):297-304.
Yu Y,Li X F,Xiao R,et al.Zircon LA-ICP-MS U-Pb and sericite ⁴⁰Ar/³⁹Ar ages at Shanhu W-Sn deposit,Guangxi Pro-vince,China,and its implications for W-Sn minerlization[J].Acta Mineral Sin,2014,34(3):297-304.
[33] 吴善益.广西都结锑矿地质特征与成因探讨[J].矿业工程,2010,8(3):12-13.
Wu S Y.Geological features and genesis-probing of Dujie Sb deposits of Guangxi province[J].Mining Engineering,2010,8(3):12-13.
[34] 黄任军.广西右江流域红锑矿产出特征与成因浅析[J].矿山地质,1994,15(4):253-260.
Huang R J.Characteristics and genesis of the Hongantimony deposit in Youjiang River Basin,Guangxi[J].Min Geol,1994,15(4):253-260.
[35] 王登红,陈郑辉,陈毓川,等.我国重要矿产地成岩成矿年代学研究新数据[J].地质学报,2010,84(7):1030-1040.
Wang D H,Chen Z H,Chen Y C,et al.New data of the rock-forming and ore-forming chronology for China's important mine-ral resources areas[J].Acta Geol Sin,2010,84(7):1030-1040.