LATEST PROSPECTING PROGRESS AND EXPLORATION DIRECTION OF COPPER-GOLD POLYMETALLIC DEPOSITS IN NENJIANG-HEIHE AREA, HEILONGJIANG PROVINCE
LIU Bao-shan1, CHENG Zhao-xun2, SHAO Jun1, LI Cheng-lu2, ZHANG Chun-peng1, YANG Hong-zhi1, HAN Ren-ping1
1. Shenyang Center of China Geological Survey, Shenyang 110034, China; 2. Natural Resources Survey Institute of Heilongjiang Province, Harbin 150036, China
Abstract：The large Late Triassic Erdaokan silver deposit is discovered in Duobaoshan ore concentration area of Duobaoshan island arc in Nenjiang-Heihe area, and the exploration in the deep part of Tongshan deposit also makes a great breakthrough. The Late Triassic Mengdehe gold deposit is found in Keluo-Xinkailing tectonic melange belt, and the gold mineralization in the deep of Sanhetun goldfield periphery as well. The small Early Cretaceous Baoquan copper deposit is discovered in Taxi magmatic arc. These deposits are consistent with regionally delineated geochemical anomalies with obvious ore-forming regularity. Based on the new discoveries of copper and gold deposits, the paper summarizes the latest prospecting progress in Nenjiang-Heihe area in recent years, pointing out the next exploration direction and suggestions for future prospecting and providing reference for the upcoming strategic prospecting deployment.
周建波,张兴洲, Wilde S A,等.中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J].岩石学报, 2011, 27(4):1235-1245. Zhou J B, Zhang X Z, Wilde S A, et al. Confirming of the Heilongjiang~500 Ma Pan-African khondalite belt and its tectonic implications[J]. Acta Petrologica Sinica, 2011, 27(4):1235-1245.
[2]
许文良,王枫,孟恩,等.黑龙江省东部古生代-早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据[J].吉林大学学报(地球科学版), 2012, 42(5):1378-1389. Xu W L, Wang F, Meng E, et al. Paleozoic-Early Mesozoic tectonic evolution in the eastern Heilongjiang Province, NE China:Evidence from Igneous rock association and U-Pb geochronology of detrital zircons[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(5):1378-1389.
[3]
杜琦,赵玉明,卢秉刚,等.多宝山斑岩铜矿床[M].北京:地质出版社, 1988:1-335. Du Q, Zhao Y M, Lu B G, et al. The Duobaoshan Porphyry copper deposit[M]. Beijing:Geological Publishing House, 1988:1-335.(in Chinese)
[4]
赵一鸣,毕承思,邹晓秋,等.黑龙江多宝山、铜山大型斑岩铜(钼)矿床中辉钼矿的铼-锇同位素年龄[J].地球学报, 1997, 18(1):61-67. Zhao Y M, Bi C S, Zou X Q, et al. The Re-Os isotopic age of molybdenite from Duobaoshan and Tongshan porphyry copper (molybdenum) deposits[J]. Acta Geoscientia Sinica, 1997, 18(1):61-67.
[5]
韩振新,徐衍强,郑庆道.黑龙江省重要金属和非金属矿产的矿床成矿系列及其演化[M].哈尔滨:黑龙江人民出版社, 2004:1-240. Han Z X, Xu Y Q, Zheng Q D. Metallogenic series and evolution of important metallic and non-metallic minerals in Heilongjiang Province[M]. Harbin:Heilongjiang People's Publishing House, 2004:1-240.(in Chinese)
[6]
王喜臣,王训练,王琳,等.黑龙江多宝山超大型斑岩铜矿的成矿作用和后期改造[J].地质科学, 2007, 42(1):124-133. Wang X C, Wang X L, Wang L, et al. Metallogeny and Reformation of the Duobaoshan superlarge porphyry copper deposit in Heilongjiang[J]. Chinese Journal of Geology, 2007, 42(1):124-133.
[7]
向安平,杨郧城,李贵涛,等.黑龙江多宝山斑岩Cu-Mo矿床成岩成矿时代研究[J].矿床地质, 2012, 31(6):1237-1248. Xiang A P, Yang Y C, Li G T, et al. Diagenetic and metallogenic ages of Duobaoshan porphyry Cu-Mo deposit in Heilongjiang Province[J]. Mineral Deposits, 2012, 31(6):1237-1248.
[8]
赵忠海,孙景贵,郭艳.黑龙江永新金矿床原生晕轴向分带特征及深部矿体预测[J].地质论评, 2017, 63(S1):157-158. Zhao Z H, Sun J G, Guo Y. Axial zoning characteristics of primary halos and deep orebody prediction in Yongxin gold deposit, Heilongjiang Province[J]. Geological Review, 2017, 63(S1):157-158.
[9]
Zeng Q D, Liu J M, Chu S X, et al. Re-Os and U-Pb geochronology of the Duobaoshan porphyry Cu-Mo-(Au) deposit, Northeast China, and its geological significance[J]. Journal of Asian Earth Sciences, 2014, 79:895-909.
[10]
Wang L, Qin K Z, Song G X, et al. Geology and genesis of the Early Paleozoic Zhengguang intermediate-sulfidation epithermal Au-Zn deposit, northeast China[J]. Ore Geology Reviews, 2020, 124:103602.
[11]
武子玉,王洪波,徐东海,等.黑龙江黑河三道湾子金矿床地质地球化学研究[J].地质论评, 2005, 51(3):264-267. Wu Z Y, Wang H B, Xu D H, et al. Geological and geochemical studies of the Sandaowanzi gold deposit, Heihe County, Heilongjiang Province[J]. Geological Review, 2005, 51(3):264-267.
[12]
李成禄,李胜荣,袁茂文,等.黑龙江省嫩江-黑河构造混杂岩带科洛金矿床成因:来自黄铁矿化学成分及He-Ar、S、Pb同位素证据[J].地学前缘, 2020, 27(5):99-115. Li C L, Li S R, Yuan M W, et al. Genesis of the Keluo Au deposit in the Nenjiang-Heihe tectonic melange belt, Heilongjiang Province:Evidence from chemical composition and pyrite He-Ar, S, Pb isotopes[J]. Earth Science Frontiers, 2020, 27(5):99-115.
[13]
刘宝山,寇林林,张春鹏,等.黑龙江嫩江地区三合屯金矿区糜棱岩锆石LA-ICP-MS U-Pb年龄与成矿的关系[J].地质学报, 2022, 96(3):954-970. Liu B S, Kou L L, Zhang C P, et al. Research on the relationship between mineralization and zircon LA-ICP-MS U-Pb dating of the mylonite from the Sanhetun gold deposit in Nenjiang region, Heilongjiang Province[J]. Acta Geologica Sinica, 2022, 96(3):954-970.
[14]
徐备,赵盼,鲍庆中,等.兴蒙造山带前中生代构造单元划分初探[J].岩石学报, 2014, 30(7):1841-1857. Xu B, Zhao P, Bao Q Z, et al. Preliminary study on the pre-Mesozoic tectonic unit division of the Xing-Meng Orogenic Belt (XMOB)[J]. Acta Petrologica Sinica, 2014, 30(7):1841-1857.
[15]
李成禄.黑龙江省嫩江-黑河构造混杂岩带金矿成矿作用及找矿预测[D].北京:中国地质大学, 2018:1-273. Li C L. Gold metallogeny and prospecting in the Nenjiang-Heihe tectonic mélange zone, Heilongjiang Province[D]. Beijing:China University of Geosciences, 2018:1-273.
[16]
赵超.中亚造山带东段多宝山含金斑岩铜矿床多期岩浆-构造-成矿作用[D].北京:中国科学院大学, 2019:1-223. Zhao C. Multistage magmatism-structure-mineralization of the Duobaoshan gold-bearing porphyry copper deposit in the eastern CAOB[D]. Beijing:University of Chinese Academy of Sciences, 2019:1-223.(in Chinese)
[17]
刘宝山,张春鹏,宋万兵,等.黑龙江多宝山斑岩铜矿床叠加改造地质特征及成因[J].大地构造与成矿学, 2020, 44(6):1076-1095. Liu B S, Zhang C P, Song W B, et al. Genesis and geological characteristics of superposition and deformation of the Duobaoshan porphyry Cu (Mo) deposit, Heilongjiang[J]. Geotectonica et Metallogenia, 2020, 44(6):1076-1095.
[18]
Zhao C, Qin K Z, Song G X, et al. Switch of geodynamic setting from the Paleo-Asian Ocean to the Mongol-Okhotsk Ocean:Evidence from granitoids in the Duobaoshan ore field, Heilongjiang Province, Northeast China[J]. Lithos, 2019, 336-337:202-220.
[19]
那福超,付俊彧,宋维民,等.小兴安岭西北部科洛杂岩的岩石学与年代学[J].地球科学, 2019, 44(10):3265-3278. Na F C, Fu J Y, Song W M, et al. Petrological and geochronological study of Keluo complex in northwestern Lesser Xing'an Range[J]. Earth Science, 2019, 44(10):3265-3278.
[20]
杨文鹏,张立东,张俭峰,等.东北地区新开岭-科洛杂岩变形规律与成因[J].地球科学, 2019, 44(7):2551-2566. Yang W P, Zhang L D, Zhang J F, et al. Deformation characteristics and genesis of the Xinkailing-Keluo complex in NE China[J]. Earth Science, 2019, 44(7):2551-2566.
[21]
刘永江,冯志强,温泉波,等.东北大兴安岭地区古生代构造演化[C]//2014年中国地球科学联合学术年会——专题45:中亚-兴蒙造山带论文集.北京:中国地球物理学会, 2014:2138. Liu Y J, Feng Z Q, Wen Q B, et al. Paleozoic tectonic evolution in Daxinganling area, Northeast China[C]//Annual Meeting of China Geoscience Association. Beijing:Chinese Geophysical Society, 2014:2138.(in Chinese)
[22]
李伟民,刘永江,冯志强,等.黑河-贺根山缝合带中段的闭合时限及位置[C]//2016中国地球科学联合学术年会论文集(七).北京:中国地球物理学会, 2016:250-251. Li W M, Liu Y J, Feng Z Q, et al. Closure time limit and position of the middle section of Heihe-Hegenshan suture zone[C]//Annual Meeting of China Geoscience Association. Beijing:Chinese Geophysical Society, 2016:250-251.(in Chinese)
[23]
苗来成,范蔚茗,张福勤,等.小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义[J].科学通报, 2003, 48(22):2315-2323. Miao L C, Fan W M, Zhang F Q, et al. Zircon SHRIMP geochronology of Xinkailing-Kolo complex in northwest Xiaoxing'an Mountains and its significance[J]. Chinese Science Bulletin, 2003, 48(22):2315-2323.
[24]
梁琛岳,刘永江,李伟,等.黑龙江嫩江地区科洛杂岩伸展构造特征[J].地质通报, 2011, 30(2/3):291-299. Liang C Y, Liu Y J, Li W, et al. Characteristics of extensional structure of Keluo complex in Nenjiang area, Heilongjiang, China[J]. Geological Bulletin of China, 2011, 30(2/3):291-299.
[25]
刘宝山,杨晓平,李成禄.黑龙江省嫩江三合屯韧性剪切带与金矿化[J].矿产与地质, 2017, 31(3):503-506, 513. Liu B S, Yang X P, Li C L. Ductile shear zone and gold mineralization of Sanhetun gold deposit in Nenjiang, Heilongjiang Province[J]. Mineral Resources and Geology, 2017, 31(3):503-506, 513.
[26]
徐文喜,李成禄,鲍希波,等.大兴安岭东北部首个三叠纪银矿床地质特征及矿床成因分析[J].矿产与地质, 2019, 33(3):434-441. Xu W X, Li C L, Bao X B, et al. Geological characteristics and genesis analysis of the first Triassic silver deposit discovered in Northeast of Da Hinggan Mountains[J]. Mineral Resources and Geology, 2019, 33(3):434-441.
[27]
袁茂文.天然沥青与非层控金属成矿关系研究——以二道坎银铅锌矿床为例[D].北京:中国地质大学(北京), 2020:1-123. Yuan M W. The contribution of the bitumen to the mineralization of the non-strata bound metal deposit:Ag-Pb-Zn deposits in the Great Xing'an Range[D]. Beijing:China University of Geosciences, 2018:1-273.
[28]
鲍希波,尹国良,于宪章.黑龙江省嫩江县二道坎村银多金属矿床地质特征及找矿标志[J].黄金, 2019, 40(7):20-23. Bao X B, Yin G L, Yu X Z. Geological characteristics of Erdaokancun silver polymetallic deposit, Nenjiang County, Heilongjiang Province and its prospecting indicators[J]. Gold, 2019, 40(7):20-23.
[29]
刘宝山.黑龙江黑河孟德河金矿床控矿因素及找矿标志[J].黄金, 2015, 36(1):18-21. Liu B S. Ore-controlling factors and prospecting marks of gold deposit in Mengdehe, Heihe City[J]. Gold, 2015, 36(1):18-21.
[30]
郝宇杰.黑龙江省多宝山矿集区成矿作用与成矿规律研究[D].长春:吉林大学, 2015:1-130. Hao Y J. Mineralization and metallogenic regularity of Duobaoshan ore concentration area in Heilongjiang Province, Northeast China[D]. Changchun:Jilin University, 2015:1-130.
[31]
杨永胜,吕新彪,高荣臻,等.黑龙江争光金矿床英云闪长斑岩年代学、地球化学及地质意义[J].大地构造与成矿学,2016, 40(4):674-700. Yang Y S, Lv X B, Gao R Z, et al. Geochronology, geochemistry and geological significance of the Tonalite porphyry in Zhengguang gold deposit, Heilongjiang Province[J]. Geotectonica et Metallogenia, 2016, 40(4):674-700.
[32]
佘宏全,李进文,向安平,等.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J].岩石学报, 2012, 28(2):571-594. She H Q, Li J W, Xiang A P, et al. U-Pb ages of the zircons from primary rocks in middle-northern Daxinganling and its implications to geotectonic evolution[J]. Acta Petrologica Sinica, 2012, 28(2):571-594.
[33]
黄道袤,赵元艺,符家俊,等.黑龙江省铜山地区岩浆岩年代学、地球化学及其地质意义[J].矿床地质, 2014, 33(S1):399-400. Huang D M, Zhao Y Y, Fu J J, et al. Geochronology, geochemistry and geological significance of magmatic rocks in Tongshan area, Heilongjiang Province[J]. Mineral Deposits, 2014, 33(S1):399-400.(in Chinese)
[34]
胡新露.大兴安岭北段-小兴安岭地区斑岩型铜、钼矿床成矿作用与岩浆活动[D].武汉:中国地质大学, 2015:1-30. Hu X L. Mineralization and magmatism of the porphyry Cu, Mo deposits in the northern great Xing'an and Lesser Xing'an Ranges[D]. Wuhan:China University of Geosciences, 2015:1-30.
[35]
蔡文艳.黑龙江省多宝山矿集区铜-钼-金多金属成矿作用研究[D].长春:吉林大学, 2020:1-130. Cai W Y. Metallogenesis of copper-molybdenum-gold polymetallic in the Duobaoshan orefield, Heilongjiang Province[D]. Changchun:Jilin University, 2020:1-130.
[36]
刘宝山,张春鹏,寇林林,等.黑龙江争光金矿床方铅矿黄铁矿Rb-Sr年龄及地质意义[J].大地构造与成矿学,2022, 46(1):102-111. Liu B S, Zhang C P, KouL L, et al. Rb-Sr age of galena and pyrite from the Zhengguang gold deposit, Heilongjiang Province and its geological significance[J]. Geotectonica et Metallogenia,2022, 46(1):102-111.
[37]
刘宝山,程招勋,寇林林,等.黑龙江多宝山地区晚三叠世岩浆活动对蒙古-鄂霍茨克洋南向俯冲的响应[J].地学前缘, 2022, 29(2):132-145. Liu B S, ChengZ X, Kou LL, et al. Late Triassic magmatic activity in Duobaoshan area, Heilongjiang Province:Response to the southward subduction of the Mongol-Okhotsk Ocean[J]. Earth Science Frontiers, 2022, 29(2):132-145.
[38]
赵忠海.小兴安岭西北部永新大型金矿成因、成矿地质模式与深部三维成矿预测[D].长春:吉林大学, 2019:1-248. Zhao Z H. Ore genesis, metallogenic geological mode and deep metallogenic prediction of the Yongxin large Au deposit based on 3D digital model in the northwestern Lesser Xing'an Range[D]. Changchun:Jilin University, 2019:1-248.
2022, Vol. 31 
辽公网安备 21010502000112号