|
|
Geological characteristics, diagenesis and mineralization of key gold concentration areas in Liaoning Province |
YUAN He1, BAI Yinzeng2, GENG Shufeng1, HONG Xiuwei1, WANG Denghong3 |
1. No.4 Geological Team of Liaoning Limited Liability Company, Liaoning Fuxin 123000, China; 2. No.109 Team of Liaoning Nonferrous Geology Co., Ltd, Liaoning Chaoyang 122000, China; 3. MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, China Academy of Geological Sciences, Beijing 100037, China |
|
|
Abstract As the important gold producing province in China, Liaoning Province has strong Mesozoic tectonic and magmatic activities, with great gold mineralization. Liaoning Province is divided into five key gold concentration areas, according to the spatial distribution characteristics of gold deposits. In order to deeply understand the diagenesis and mineralization of gold deposits in each gold concentration area, the authors systematically analyzed the geological characteristics, diagenesis and mineralization age, and the geochemistry of the gold concentration area. The results show that the gold mineralization in each gold concentration area is related to the magmatic activities of Indosinian and Yanshanian periods, and the metallogenic time is concentrated in 126~118 Ma and 225~188 Ma. The sulfur in gold ores in Western Liaoning gold concentration area belongs to mantle sulfur, while the sulfur in Eastern Liaoning gold concentration area comes from magmatic and metamorphic rock strata. The Pb in ore source of each ore concentration area has the characteristics of crust mantle mixed source. The source areas of the five key gold concentration areas are composed of the products of different magmatic evolution stages in the same magmatic source area. The ore material sources of five important gold concentration areas are magmatic evolution products from one magmatic source under different stages, and the diagenetic and diagenetic minerals are the products of partial melting of the lower crust, with the participation of some mantle derived materials. The geological model for gold prospecting prediction in Liaoning Province was established, combined with the recent prospecting progress, which could provide a new idea for further regional mineral exploration.
|
Received: 27 June 2022
|
|
|
|
|
[1] 刘国平,艾永富.辽宁白云金矿床成矿时代探讨[J].岩石学报,2000,16(4):627-632. Liu G P,Ai Y F.Studies on the mineralization age of Baiyun gold deposit in Liaoning[J].Acta Petrologica Sinica,2000,16(4):627-632. [2] 苗来成,范蔚茗,翟明国,等.金厂沟梁—二道沟金矿田内花岗岩类侵入体锆石的离子探针U-Pb年代学及意义[J].岩石学报,2003,19(1):71-80. Miao L C,Fan W M,Zhai M G,et al.Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefield and its significance[J].Acta Petrologica Sinica,2003,19(1):71-80. [3] 魏俊浩,刘丛强,李志德,等.论金矿床成矿年代的确定——以丹东地区成岩成矿Rb-Sr、U-Pb同位素年代为例[J].地质学报,2003,77(1):113-119. Wei J H,Liu C Q,Li Z D,et al.U-Pb,Rb-Sr Isotopic dating of the diagenesis and mineralization of gold deposits in the Dandong area[J].Acta Geologica Sinica,2003,77(1):113-119. [4] 袁和,王登红.辽宁省金矿成矿规律及成矿系列[J].中国地质调查,2022,9(2):73-82. Yuan H,Wang D H.Metallogenic regularity and series of gold deposits in Liaoning Province[J].Geological Survey of China,2022,9(2):73-82. [5] 贾三石,王恩德,付建飞,等.冀东—辽西主要金矿矿集区地质特征的差异性与成矿作用的统一性探析[J].地质学报,2011,85(9):1493-1506. Jia S S,Wang E D,Fu J F,et al.Geological differences and mi-neralization unity of the key gold ore concentrated regions in eas-tern Hebei and western Liaoning provinces[J].Acta Geologica Sinica,2011,85(9):1493-1506. [6] 孙守恪,刘红涛,褚少雄.辽宁省排山楼矿区二长花岗岩成因及其与金矿化的关系[J].岩石学报,2012,28(2):607-618. Sun S K,Liu H T,Chu S X.Origin of the Paishanlou monzogranite in Liaoning Province and its genetic connection with gold minera-lization[J].Acta Petrologica Sinica,2012,28(2):607-618. [7] 郝立波,赵昕,赵玉岩.辽宁白云金矿床稳定同位素地球化学特征及矿床成因[J].吉林大学学报: 地球科学版,2017,47(2):442-451. Hao L B,Zhao X,Zhao Y Y.Stable isotope characteristics and ore genesis of the Baiyun gold deposit,Liaoning Province[J].Journal of Jilin University:Earth Science Edition,2017,47(2):442-451. [8] 刘军,李铁刚,段超.辽宁猫岭大型金矿床成岩成矿年龄及同位素地球化学特征[J].地质通报,2018,37(7):1325-1337. Liu J,Li T G,Duan C.Geochronology and isotopic geochemistry characteristics of the Maoling large gold deposit,Liaoning Pro-vince,China[J].Geological Bulletin of China,2018,37(7):1325-1337. [9] 刘军,王树岭,李铁刚,等.辽宁省五龙金矿床成岩成矿年代学及同位素地球化学特征[J].矿床地质,2018,37(4):712-728. Liu J,Wang S L,Li T G,et al.Geochronology and isotopic geochemical characteristics of Wulong gold deposit in Liaoning Pro-vince[J].Mineral Deposits,2018,37(4):712-728. [10] 曾庆栋,陈仁义,杨进辉,等.辽东地区金矿床类型、成矿特征及找矿潜力[J].岩石学报,2019,35(7):1939-1963. Zeng Q D,Chen R Y,Yang J H,et al.The metallogenic characte-ristics and exploring ore potential of the gold deposits in eastern Liaoning Province[J].Acta Petrologica Sinica,2019,35(7):1939-1963. [11] 翟明国. 华北克拉通的形成演化与成矿作用[J].矿床地质,2010,29(1):24-36. Zhai M G.Tectonic evolution and metallogenesis of North China Craton[J].Mineral Deposits,2010,29(1):24-36. [12] 杨凤超,宋运红,杨佳林,等.辽东五龙—四道沟金矿集区花岗杂岩SHRIMP U-Pb年龄、地球化学特征及地质意义[J].大地构造与成矿学,2018,42(5):940-954. Yang F C,Song Y H,Yang J L,et al.SHRIMP U-Pb Age and geochemical characteristics of granites in Wulong-Sidaogou gold deposit,East Liaoning[J].Geotectonica et Metallogenia,2018,42(5):940-954. [13] 曲亚军. 辽宁省金矿成矿作用与成矿预测研究[D].长春:吉林大学,2006. Qu Y J.The Gold Mineralization and Prognosis in Liaoning Pro-vince[D].Changchun:Jilin University,2006. [14] 翟明国. 克拉通化与华北陆块的形成[J].中国科学:地球科学,2011,41(8):1037-1046. Zhai M G.Cratonization and the Ancient North China Continent:A summary and review[J].Science China Earth Sciences,2011,54(8):1110-1120. [15] 辽宁省地质矿产调查院.辽宁省矿产资源潜力评价报告[R].沈阳:辽宁省地质矿产调查院,2012. Institute of Geological and Mineral Survey of Liaoning Province.Report on Evaluation Results of Mineral Resources Potential in Li-aoning Province[R].Shenyang:Institute of Geological and Mineral Survey of Liaoning Province,2012. [16] 聂飞,刘书生,董国臣,等.辽西二道沟金矿成矿物质来源:来自S-Pb同位素的证据[J].现代地质,2018,32(6):1283-1291. Nie F,Liu S S,Dong G C,et al.The ore-forming material of the erdaogou gold deposit in west Liaoning Province:Evidence from S-Pb isotopes[J].Geoscience,2018,32(6):1283-1291. [17] 罗镇宽,苗来成,关康,等.辽宁阜新排山楼金矿区岩浆岩锆石SHRIMP定年及其意义[J].地球化学,2011,30(5):483-490. Luo Z K,Miao L C,Guan K,et al.SHRIMP U-Pb zircon age of magmatic rock in Paishanlou gold mine district,Fuxin,Liaoning Province,China[J].Geochimica,2001,30(5):483-490. [18] 段晓侠,刘建明,王永彬,等.辽宁青城子铅锌多金属矿田晚三叠世岩浆岩年代学、地球化学及地质意义[J].岩石学报,2012,28(2):595-606. Duan X X,Liu J M,Wang Y B,et al.Geochronology,geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield,Liaoning[J].Acta Petrologica Sinica,2012,28(2):595-606. [19] 顾玉超. 辽东五龙金矿区中生代构造-岩浆作用对金成矿制约[D].北京:中国地质大学(北京),2019. Gu Y C.The Mesozoic Tectonic-magmatic Constraints on the Gold Mineralization in Wulong Gold Mining Area,Eastern Liaoning[D].Beijing:China University of Geosciences (Beijing),2019. [20] 王志强,胡滑志帆,陈斌,等.辽东半岛早白垩世三股流岩体岩石成因:微量元素模拟和Sr-Nd同位素的制约[J].岩石学报,2020,36(12):3683-3704. Wang Z Q,Hu H Z F,Chen B,et al.The petrogenesis of the Early Cretaceous Sanguliu pluton in the Liaodong Peninsula,NE China:constrained from the trace-element modelling and Sr-Nd isotopes[J].Acta Petrologica Sinica,2020,36(12):3683-3704. [21] 张朋. 辽宁省东南部典型有色、贵金属矿床成矿特征、成因与成岩成矿地球动力学过程[D].长春:吉林大学,2018. Zhang P.Metallogenic Characteristics,Ore Genesis,Diagenesis and Metallogenic Geodynamic Process of Precious and Non Ferrous Metals Ore Deposits in Southeast Liaoning Province[D].Changchun:Jilin University,2018. [22] 张朋,李斌,李杰,等.辽东裂谷白云金矿载金黄铁矿Re-Os定年及其地质意义[J].大地构造与成矿学,2016,40(4):731-738. Zhang P,Li B,Li J,et al.Re-Os isotopic dating and its geological implication of gold bearing pyrite from the Baiyun gold deposit in Liaodong rift[J].Geotectonica et Metallogenia,2016,40(4):731-738. [23] 马玉波,邢树文,张增杰,等.辽吉裂谷区铅锌金矿床S、Pb同位素组成特征及其地质意义[J].地质学报,2013,87(9):1399-1410. Ma Y B,Xing S W,Zhang Z J,et al.Characteristics of the sulfur and lead isotope compositions of the polymetallic deposit in the Liaoji rift and their geological significance[J].Acta Geologica Sinica,2013,87(9):1399-1410. [24] 王义文. 辽宁省金矿床铅同位素组成特征及其地质意义[J].辽宁地质,1992(3):241-254. Wan Y W.Lead isotope features of gold deposits of Liaoning province and its geological significance[J].Liaoning Geology,1992(3):241-254. [25] 张博文,孙丰月,常国林,等.辽宁朝阳东五家子金矿床成因类型讨论[J].世界地质,2009,28(3):297-304. Zhang B W,Sun F Y,Chang G L,et al.Discussion on genetic type of Dongwujiazi gold deposit of Chaoyang,Liaoning[J].Global Geology,2009,28(3):297-304. [26] 王安建,李树勋,曲亚军.脉状金矿地质与成因[M].长春:吉林科学技术出版社,1996. Wang A J,Li S X,Qu Y J.Geology and Origin of Lode Gold Deposits[M].Changchun:Jilin Science and Technology Press,1996. [27] Zhang X H,Liu Q,Ma Y J,et al.Geology,fluid inclusions,isotope geochemistry,and geochronology of the Paishanlou shear zone-hosted gold deposit,North China Craton[J].Ore Geology Reviews,2005,26(3/4):325-348. [28] 郝瑞霞,彭省临.辽宁王家崴子金矿床地球化学研究[J].黄金地质,1999,5(2):47-51. Hao R X,Peng S L.Geochemical study of Wangjiawaizi gold deposit in Liaoning[J].Gold Geology,1999,5(2):47-51. [29] 张森,张迪,沙德喜,等.辽东林家三道沟—小佟家堡子地区金(银)矿成矿特征及成因[J].吉林大学学报(地球科学版),2012,42(3):725-732. Zhang S,Zhang D,Sha D X,et al.Metallogenetic characteristics and genesis of the gold (silver) mineralization in Linjiasandaogou-Xiaotongjiapuzi area,eastern Liaoning Province[J].Journal of Jilin University (Earth Science Edition),2012,42(3):725-732. [30] 吴兴华,关广岳,金成洙.四道沟金矿床地质地球化学研究[J].地质与勘探,1990,26(10):1-6. Wu X H,Guan G Y,Jin C Z.Geological and geochemical studies on the Sidaogou gold deposit[J].Geology and Prospecting,1990,26(10):1-6. [31] 杨凤超,宋运红,张朋,等.辽宁青城子矿集区金银矿成矿流体特征和成矿物质来源示踪[J].地质学报,2016,90(10):2775-2785. Yang F C,Song Y H,Zhang P,et al.Forming fluid characteristics and tracing of Ore-forming source materials of gold-silver deposit in the Qingchengzi ore concentration area[J].Acta Geologica Sinica,2016,90(10):2775-2785. [32] Haschke M,Ahmadian J,Murata M,et al.Copper mineralization prevented by arc-root delamination during Alpine-Himalayan collision in central Iran[J].Economic Geology,2010,105(4):855-865. [33] 付乐兵. 华北克拉通北缘赤峰—朝阳地区中生代构造岩浆演化与金成矿[D].武汉:中国地质大学,2012. Fu L B.The Mesozoic Tectonic-magmatic Evolution Process and Gold Metallogenesis in Chifeng-Chaoyang Region,Northern,North China Craton[D].Wuhan:China University of Geosciences,2012. [34] 李阳. 辽东青城子矿集区三叠纪侵入岩地球化学特征研究[D].北京:中国地质大学(北京),2020. Li Y.Study on the Origin and Genesis of Metallogenic Materials in Baiyun Gold Deposit in Eastern Liaoning Province[D].Beijing:China University of Geosciences (Beijing),2020. [35] Jahn B M,Wu F Y,Hong D W.Important crustal growth in the Phanerozoic:Isotopic evidence of granitoids from east-central Asia[J].Journal of Earth System Science,2000,109(1):5-20. |
[1] |
YUAN He, WANG Denghong. Metallogenic regularity and series of gold deposits in Liaoning Province[J]. , 2022, 9(2): 73-82. |
[2] |
YAO Yonglong. Features and buried environment analysis of fossils specimens in Shuangmiao region of Kazuo County in Liaoning Province[J]. , 2020, 7(3): 61-66. |
[3] |
XUE Qing, WU Wei, LI Mingsong, DONG Shuangfa, WANG Bing, FAN Yunxiang. Application of remote sensing technology in mine environment monitoring in Liaoning Province[J]. , 2016, 3(5): 54-59. |
|
|
|
|