PROSPECTING PROGRESS AND EXPLORATION DIRECTION OF COPPER DEPOSITS IN NORTHERN DAXINGANLING MOUNTAINS

LIU Bao-shan; LI Cheng-lu; CHENG Zhao-xun; LIU Gui-xiang; WANG Ze-yu; ZHANG Chun-peng; KOU Lin-lin; HAN Ren-ping

doi:10.13686/j.cnki.dzyzy.2024.04.010

2024 Vol. 33, No. 4

Article Contents

Article navigation > Geology and Resources > 2024 > 33(4): 564-577

Next Article Previous Article

LIU Bao-shan, LI Cheng-lu, CHENG Zhao-xun, LIU Gui-xiang, WANG Ze-yu, ZHANG Chun-peng, KOU Lin-lin, HAN Ren-ping. PROSPECTING PROGRESS AND EXPLORATION DIRECTION OF COPPER DEPOSITS IN NORTHERN DAXINGANLING MOUNTAINS[J]. Geology and Resources, 2024, 33(4): 564-577. doi: 10.13686/j.cnki.dzyzy.2024.04.010

Citation:

LIU Bao-shan, LI Cheng-lu, CHENG Zhao-xun, LIU Gui-xiang, WANG Ze-yu, ZHANG Chun-peng, KOU Lin-lin, HAN Ren-ping. PROSPECTING PROGRESS AND EXPLORATION DIRECTION OF COPPER DEPOSITS IN NORTHERN DAXINGANLING MOUNTAINS[J]. Geology and Resources, 2024, 33(4): 564-577. doi: 10.13686/j.cnki.dzyzy.2024.04.010

PROSPECTING PROGRESS AND EXPLORATION DIRECTION OF COPPER DEPOSITS IN NORTHERN DAXINGANLING MOUNTAINS

1.
Shenyang Center of China Geological Survey, Shenyang 110034, China
2.
Heilongjiang Institute of Natural Resources Survey, Harbin 150036, China

More Information

Corresponding author: LIU Gui-xiang, 549462147@qq.com

Received Date: 27 February 2024

Revised Date: 02 July 2024

Publish Date: 25 August 2024

Abstract

Abstract

The northern Daxinganling Mountains is an important part of Daxinganling metallogenic belt, where copper is the main mineral, dominated by porphyry type, large in scale, with great economic value and scientific research significance. Based on the systematic summary of regional geological background and mineralization process of copper deposits in different ages in northern Daxinganling Mountains, the paper summarizes the new exploration results in the area in recent years, and points out that the western margin of Ergun block, southeastern margin of Xing'an block, and suture zone of the two blocks are important for copper deposit prospecting. Attention should be also paid nearby the existing deposits and blind orebodies in the deep for the exploration of copper deposits in northern Daxinganling Mountains.
- copper deposit /
- Ergun block /
- Xing'an block /
- metallogenic belt /
- ore prospecting /
- Daxinganling Mountains

FullText(HTML)

References

[1]	佘宏全, 常国雄, 李进文, 等. 内蒙古大兴安岭北段及邻区铜钼铅锌多金属矿床成矿时代分布规律[J]. 矿床地质, 2010, 29(S1): 499-501. Google Scholar She H Q, Chang G X, Li J W, et al. Metallogenic epoch distribution of Cu-Mo-Pb-Zn polymetallic deposit in northern section of Greater Hinggan Mountains and adjacent areas of Inner Mongolia[J]. Mineral Deposits, 2010, 29(S1): 499-501. (in Chinese) Google Scholar
[2]	徐琳, 唐金荣. 我国铜资源供给风险识别及分析研究[J]. 北京大学学报(自然科学版), 2017, 53(3): 555-562. Google Scholar Xu L, Tang J R. Copper supply risk identification and analysis study in China[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2017, 53(3): 555-562. Google Scholar
[3]	Mao J W, Pirajno F, Lehmann B, et al. Distribution of porphyry deposits in the Eurasian continent and their corresponding tectonic settings[J]. Journal of Asian Earth Sciences, 2014, 79: 576-584. doi: 10.1016/j.jseaes.2013.09.002 CrossRef Google Scholar
[4]	武广, 王国瑞, 刘军, 等. 大兴安岭北部主要金属矿床成矿系列和区域矿床成矿谱系[J]. 矿床地质, 2014, 33(6): 1127-1150. doi: 10.3969/j.issn.0258-7106.2014.06.001 CrossRef Google Scholar Wu G, WangG R, Liu J, et al. Metallogenic series and ore-forming pedigree of main ore deposits in northern Great Xing'an Range[J]. Mineral Deposits, 2014, 33(6): 1127-1150. doi: 10.3969/j.issn.0258-7106.2014.06.001 CrossRef Google Scholar
[5]	Xu W L, Pei F P, Wang F, et al. Spatial-temporal relationships of Mesozoic volcanic rocks in NE China: Constraints on tectonic overprinting and transformations between multiple tectonic regimes[J]. Journal of Asian Earth Sciences, 2013, 74: 167-193. doi: 10.1016/j.jseaes.2013.04.003 CrossRef Google Scholar
[6]	Tang J, Xu W L, Wang F, et al. Geochronology, geochemistry, and deformation history of Late Jurassic-Early Cretaceous intrusive rocks in the Erguna Massif, NE China: Constraints on the Late Mesozoic tectonic evolution of the Mongol-Okhotsk orogenic belt[J]. Tectonophysics, 2015, 658: 91-110. doi: 10.1016/j.tecto.2015.07.012 CrossRef Google Scholar
[7]	Li Z Z, Qin K Z, Li G M, et al. Neoproterozoic and Early Paleozoic magmatic records from the Chalukou ore district, northern Great Xing'an Range, NE China: Implications for tectonic evolution and Mesozoic Mo mineralization[J]. Journal of Asian Earth Sciences, 2018, 165: 96-113. doi: 10.1016/j.jseaes.2018.06.020 CrossRef Google Scholar
[8]	Deng C Z, Sun D Y, Han J S, et al. Late-stage southwards subduction of the Mongol-Okhotsk oceanic slab and implications for porphyry Cu-Mo mineralization: Constraints from igneous rocks associated with the Fukeshan deposit, NE China[J]. Lithos, 2019, 326-327: 341-357. doi: 10.1016/j.lithos.2018.12.030 CrossRef Google Scholar
[9]	Xu C H, Sun F Y, Fan X Z, et al. The Early Cretaceous tectonic evolution of the southern Great Xing'an Range, northeastern China: New constraints from A2-type granite and monzodiorite[J]. Canadian Journal of Earth Sciences, 2022, 59(3): 135-155. doi: 10.1139/cjes-2021-0041 CrossRef Google Scholar
[10]	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. doi: 10.1016/j.jseaes.2013.02.007 CrossRef Google Scholar
[11]	Liu J, Li Y, Zhou Z H, et al. The Ordovician igneous rocks with high Sr/Y at the Tongshan porphyry copper deposit, satellite of the Duobaoshan deposit, and their metallogenic role[J]. Ore Geology Reviews, 2017, 86: 600-614. doi: 10.1016/j.oregeorev.2017.02.036 CrossRef Google Scholar
[12]	李春风, 柳振江, 宓奎峰, 等. 内蒙古八大关斑岩型铜钼矿地球化学特征与成矿过程探讨[J]. 矿床地质, 2014, 33(S1): 215-216. Google Scholar Li C F, Liu Z J, Mi K F, et al. Geochemical characteristics and metallogenic process of porphyry copper-molybdenum deposit in Badaguan, Inner Mongolia[J]. Mineral Deposits, 2014, 33(S1): 215-216. (in Chinese) Google Scholar
[13]	康永建, 向安平, 佘宏全, 等. 内蒙古八大关斑岩型Cu-Mo矿床成矿流体特征及成矿机制研究[J]. 地质学报, 2016, 90(8): 1778-1797. doi: 10.3969/j.issn.0001-5717.2016.08.010 CrossRef Google Scholar Kang Y J, Xiang A P, She H Q, et al. The characteristics of ore-forming fluids and mineralization mechanism in the Badaguan porphyry Cu-Mo deposit, Inner Mongolia, NE China[J]. Acta Geologica Sinica, 2016, 90(8): 1778-1797. doi: 10.3969/j.issn.0001-5717.2016.08.010 CrossRef Google Scholar
[14]	秦克章, 李惠民, 李伟实, 等. 内蒙古乌奴格吐山斑岩铜钼矿床的成岩、成矿时代[J]. 地质论评, 1999, 45(2): 180-185. doi: 10.3321/j.issn:0371-5736.1999.02.011 CrossRef Google Scholar Qin K Z, Li H M, Li W S, et al. Intrusion and mineralization ages of the Wunugetushan porphyry Cu-Mo deposit, Inner Mongolia, northwestern China[J]. Geological Review, 1999, 45(2): 180-185. doi: 10.3321/j.issn:0371-5736.1999.02.011 CrossRef Google Scholar
[15]	陈志广, 张连昌, 万博, 等. 内蒙古乌奴格吐山斑岩铜钼矿床低Sr-Yb型成矿斑岩地球化学特征及地质意义[J]. 岩石学报, 2008, 1: 115-128. Google Scholar Chen Z G, Zhang L C, Wan B, et al. Geochemistry and geological significances of ore-forming porphyry with low Sr and Yb value in Wunugetushan copper-molybdenum deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 2008, 24(1): 115-128. Google Scholar
[16]	Kan J, Qin KZ, Wang L, et al. The influence of fluid-exsolving depth on mineralization quality: Evidence from biotite and zircon mineralogy and fluid inclusions from the 460 Gaodi porphyry Mo-Cu deposit, NE China[J]. Minerals, 2023, 13(5): 699. doi: 10.3390/min13050699 CrossRef Google Scholar
[17]	尚毅广, 孙丰月, 姜和芳, 等. 大兴安岭北段霍洛台铜铅锌矿区花岗闪长岩的岩石成因: 地球化学和锆石U-Pb年代学制约[J]. 世界地质, 2017, 36(2): 474-485. doi: 10.3969/j.issn.1004-5589.2017.02.014 CrossRef Google Scholar Shang Y G, Sun F Y, Jiang H F, et al. Petrogenesis of granodiorites in Huoluotai Cu-Pb-Zn mining area: Constrain from geochemistry and zircon U-Pb geochronology, northern Daxing'anling[J]. Global Geology, 2017, 36(2): 474-485. doi: 10.3969/j.issn.1004-5589.2017.02.014 CrossRef Google Scholar
[18]	邓昌州. 大兴安岭北部中生代斑岩铜矿: 成岩与成矿[D]. 长春: 吉林大学, 2019: 1-236. Google Scholar Deng C Z. Petrology and metallogenesis of the porphyry Cu depositsin the northern Great Xing'an Range[D]. Changchun: Jilin University, 2019: 1-236. Google Scholar
[19]	Sun Y G, Li B L, Zhao Z H, et al. Late Jurassic adakitic ore-bearing granodiorite porphyry intrusions in the Xiaokele porphyry Cu (-Mo) deposit, Northeast China: Implications for petrogenesis and tectonic setting[J]. Acta Geochimica, 2021, 40(5): 702-717. doi: 10.1007/s11631-021-00485-z CrossRef Google Scholar
[20]	宫永吉, 孙景贵, 刘阳. 再论大兴安岭中东部六九山铜矿床成矿地质特征、成因与成矿地质背景[J]. 吉林地质, 2020, 39(4): 1-10. doi: 10.3969/j.issn.1001-2427.2020.04.001 CrossRef Google Scholar Gong Y J, Sun J G, Liu Y. A re-evaluation on the deposit geological features, genesis and metallogenic geological setting of Liujiushan Cu deposit in the central-eastern segment of the Greater Xing'an Range[J]. Jilin Geology, 2020, 39(4): 1-10. doi: 10.3969/j.issn.1001-2427.2020.04.001 CrossRef Google Scholar
[21]	杨元江, 吕长禄, 李科, 等. 黑龙江六九铜矿区岩浆岩年代学及成矿指示意义[J]. 矿物岩石, 2021, 41(3): 118-127. Google Scholar Yang Y J, Lv C L, Li K, et al. Magmatic geochronology and metallogenic geological significance in Liujiu Cu deposit, Heilongjiang Province[J]. Mineralogy and Petrology, 2021, 41(3): 118-127. Google Scholar
[22]	王磊. 黑龙江省漠河县霍洛台铜钼矿床地质特征及找矿方向研究[D]. 长春: 吉林大学, 2018. Google Scholar Wang L. Study on geological characteristics and prospecting direction of copper-molybdenum deposit in Helotai, Mohe County, Heilongjiang Province[D]. Changchun: Jilin University, 2018. Google Scholar
[23]	李文龙, 杨晓平, 钱程, 等. 大兴安岭北段富克山岩浆弧的组成: 对蒙古-鄂霍茨克洋南向俯冲的制约[J]. 地学前缘, 2022, 29(2): 146-163. Google Scholar Li W L, Yang X P, Qian C, et al. Composition of the Fukeshan magmatic arc in the northern Great Xing'an Range: Constraints on the southward subduction of the Mongol-Okhotsk oceanic plate[J]. Earth Science Frontiers, 2022, 29(2): 146-163. Google Scholar
[24]	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. Google Scholar Liu B S, Cheng Z X, Kou L L, 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. Google Scholar
[25]	佘宏全, 李红红, 李进文, 等. 内蒙古大兴安岭中北段铜铅锌金银多金属矿床成矿规律与找矿方向[J]. 地质学报, 2009, 83(10): 1456-1472. doi: 10.3321/j.issn:0001-5717.2009.10.010 CrossRef Google Scholar She H Q, Li H H, Li J W, et al. The Metallogenetical characteristics and prospecting direction of the copper-lead-zinc polymetal deposits in the northern-central Daxing'anling Mountain, Inner Monglia[J]. Acta Geologica Sinica, 2009, 83(10): 1456-1472. doi: 10.3321/j.issn:0001-5717.2009.10.010 CrossRef Google Scholar
[26]	孙永刚. 大兴安岭北段晚侏罗世斑岩型铜(钼)矿床成矿作用及找矿方向研究[D]. 长春: 吉林大学, 2021. Google Scholar Sun Y G. Study on metallogenesis and prospecting direction of Late Jurassic porphyry Cu (Mo) deposits in the northern segmentof the Great Xing'an Range[D]. Changchun: Jilin University, 2021. Google Scholar
[27]	Zhang Y H, Xu W L, Tang J, et al. Age and provenance of the Ergunahe Group and the Wubinaobao Formation, northeastern Inner Mongolia, NE China: Implications for tectonic setting of the Erguna massif[J]. International Geology Review, 2014, 56(6): 653-671. doi: 10.1080/00206814.2013.877856 CrossRef Google Scholar
[28]	Zhao S, Xu W L, Tang J, et al. Timing of formation and tectonic nature of the purportedly Neoproterozoic Jiageda Formation of the Erguna massif, NE China: Constraints from field geology and U-Pb geochronology of detrital and magmatic zircons[J]. Precambrian Research, 2016, 281: 585-601. doi: 10.1016/j.precamres.2016.06.014 CrossRef Google Scholar
[29]	许文良, 孙晨阳, 唐杰, 等. 兴蒙造山带的基底属性与构造演化过程[J]. 地球科学, 2019, 44(5): 1620-1646. Google Scholar Xu W L, Sun C Y, Tang J, et al. Basement nature and tectonic evolution of the Xing'an-Mongolian orogenic belt[J]. Earth Science, 2019, 44(5): 1620-1646. Google Scholar
[30]	唐杰. 额尔古纳地块中生代火成岩的年代学与地球化学: 对蒙古-鄂霍茨克缝合带构造演化的制约[D]. 长春: 吉林大学, 2016: 1-189. Google Scholar Tang J. Geochronology and geochemistry of the Mesozoic igneous rocks in the Erguna massif, NE China: Constraints on the tectonic evolution of the Mongol-Okhotsk suture zone[D]. Changchun: Jilin University, 2016: 1-189. Google Scholar
[31]	葛文春, 吴福元, 周长勇, 等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报, 2005, 21(3): 749-762. Google Scholar Ge W C, Wu F Y, Zhou C Y, et al. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3): 749-762. Google Scholar
[32]	Zhao S, Xu W L, Wang W, et al. Geochronology and geochemistry of Middle-Late Ordovician granites and gabbros in the Erguna region, NE China: Implications for the tectonic evolution of the Erguna Massif[J]. Journal of Earth Science, 2014, 25(5): 841-853. doi: 10.1007/s12583-014-0476-9 CrossRef Google Scholar
[33]	Feng Z Q, Jia J, Liu Y J, et al. Geochronology and geochemistry of the Carboniferous magmatism in the northern Great Xing'an Range, NE China: Constraints on the timing of amalgamation of Xing'an and Songnen blocks[J]. Journal of Asian Earth Sciences, 2015, 113: 411-426. doi: 10.1016/j.jseaes.2014.12.017 CrossRef Google Scholar
[34]	Li Y, Xu W L, Wang F, et al. Geochronology and geochemistry of Late Paleozoic volcanic rocks on the western margin of the Songnen-Zhangguangcai Range massif, NE China: Implications for the amalgamation history of the Xing'an and Songnen-Zhangguangcai Range massif[J]. Lithos, 2014, 205: 394-410. doi: 10.1016/j.lithos.2014.07.008 CrossRef Google Scholar
[35]	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: 1-174. Google Scholar 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: 1-174. Google Scholar
[36]	白令安. 大兴安岭中北部热液铜矿床的成矿机制与资源预测[D]. 长春: 吉林大学, 2013: 1-130. Google Scholar Bai L A. Study on metallogenic mechanism and resource forecast of hydrothermal Cu deposits in the central and north of the Great Xing'an Range, NE China[D]. Changchun: Jilin University, 2013: 1-130. Google Scholar
[37]	李宇. 兴安地块中生代火成岩的年代学与地球化学: 对蒙古-鄂霍茨克构造体系演化的制约[D]. 长春: 吉林大学, 2018: 1-142. Google Scholar Li Y. Geochronology and geochemistry of the Mesozoic igneous rocks in the Xing'an massif, NE China: Constraints on the evolution of the Mongol-Okhotsk tectonic regime[D]. Changchun: Jilin University, 2018: 1-142. Google Scholar
[38]	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. doi: 10.3969/j.issn.0258-7106.2012.06.009 CrossRef Google Scholar 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. doi: 10.3969/j.issn.0258-7106.2012.06.009 CrossRef Google Scholar
[39]	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. Google Scholar Zhao C. Multistage magmatic-tectonic-mineralization of the Duobaoshan gold-bearing porphyry copper deposit in the eastern part of the Central Asian orogenic belt[D]. Beijing: University of Chinese Academy of Sciences, 2019: 1-223. (in Chinese) Google Scholar
[40]	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: 1-199. Google Scholar Hao Y J. Mineralization and metallogenic regularity of Duobaoshan ore concentration area in Heilongjiang Province, Northeast China[D]. Changchun: Jilin University, 2015: 1-199. Google Scholar
[41]	康永建, 佘宏全, 向安平, 等. 内蒙古八大关矿区印支期岩浆活动及其找矿意义[J]. 中国地质, 2014, 41(4): 1215-1225. doi: 10.3969/j.issn.1000-3657.2014.04.015 CrossRef Google Scholar Kang Y J, She H Q, Xiang A P, et al. Indo-Chinese magmatic activity in the Badaguan ore district of Inner Mongolia and its metallogenic implications[J]. Geology in China, 2014, 41(4): 1215-1225. doi: 10.3969/j.issn.1000-3657.2014.04.015 CrossRef Google Scholar
[42]	王召林, 李占龙, 郑小明. 内蒙古太平川钼铜矿床岩石地球化学、热液活动记录与年代学[J]. 矿产勘查, 2017, 8(2): 184-195. doi: 10.3969/j.issn.1674-7801.2017.02.001 CrossRef Google Scholar Wang Z L, Li Z L, Zheng X M. Petrogeochemistry, records of hydrothermal activities and geochronology of the Taipingchuan Mo-Cu deposit, Inner Mongolia[J]. Mineral Exploration, 2017, 8(2): 184-195. doi: 10.3969/j.issn.1674-7801.2017.02.001 CrossRef Google Scholar
[43]	谭钢. 内蒙古乌奴格吐山斑岩铜钼矿床成矿作用研究[D]. 北京: 中国地质科学院, 2011: 1-91. Google Scholar Tan G. The ore-forming processes and mineralization of Wunugetushan porphyry Cu-Mo deposit, Inner Mongolia[D]. Beijing: Chinese Academy of Geological Sciences, 2011: 1-91. Google Scholar
[44]	吕鹏瑞, 李德荣, 彭义伟, 等. 黑龙江三矿沟矽卡岩型Cu-Fe-Mo矿床矿石硫化物硫、铅同位素特征及锆石U-Pb定年[J]. 中国地质, 2012, 39(3): 717-728. doi: 10.3969/j.issn.1000-3657.2012.03.013 CrossRef Google Scholar Lv P R, Li D R, Peng Y W, et al. S-Pb isotopic characteristics of ore sulfides and U-Pb dating of zircon from the Sankuanggou skarn-type Cu-Fe-Mo deposit in Heilongjiang Province[J]. Geology in China, 2012, 39(3): 717-728. doi: 10.3969/j.issn.1000-3657.2012.03.013 CrossRef Google Scholar
[45]	Sun Y G, Li B L, Zhao Z H, et al. Age and petrogenesis of late Mesozoic intrusions in the Huoluotai porphyry Cu-(Mo) deposit, Northeast China: implications for regional tectonic evolution[J]. Geoscience Frontiers, 2022, 13(2): 101344. doi: 10.1016/j.gsf.2021.101344 CrossRef Google Scholar
[46]	王筱筝, 吕骏超, 胥嘉, 等. 黑龙江六九山铜银矿床地质特征[J]. 地质与资源, 2016, 25(2): 137-143. doi: 10.3969/j.issn.1671-1947.2016.02.007 CrossRef Google Scholar Wang X Z, Lyu J C, Xu J, et al. Geological characteristics of the Liujiushan copper-silver deposit in Heilongjiang Province[J]. Geology and Resources, 2016, 25(2): 137-143. doi: 10.3969/j.issn.1671-1947.2016.02.007 CrossRef Google Scholar
[47]	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: 1-223. Google Scholar Cai W Y. Metallogenesis of copper-molybdenum-gold polymetallic in the Duobaoshan orefield, Heilongjiang Province[D]. Changchun: Jilin University, 2020: 1-223. Google Scholar
[48]	Zhang F F, Wang Y H, Liu J J, et al. Origin of the Wunugetushan porphyry Cu-Mo deposit, Inner Mongolia, NE China: Constraints from geology, geochronology, geochemistry, and isotopic compositions[J]. Journal of Asian Earth Sciences, 2016, 117: 208-224. doi: 10.1016/j.jseaes.2015.12.018 CrossRef Google Scholar
[49]	Zhai M G, Santosh M. Metallogeny of the North China Craton: Link with secular changes in the evolving earth[J]. Gondwana Research, 2013, 24(1): 275-297. doi: 10.1016/j.gr.2013.02.007 CrossRef Google Scholar
[50]	王献忠, 宋贵斌, 公维国, 等. 黑龙江塔河宝兴沟金矿床地质特征及流体包裹体研究[J]. 黄金, 2014, 35(4): 19-25. Google Scholar Wang X Z, Song G B, Gong W G, et al. Study on geological characteristics and fluid inclusions of Baoxinggou gold deposit in Tahe, Heilongjiang Province[J]. Gold, 2014, 35(4): 19-25. Google Scholar
[51]	李良, 孙丰月, 李碧乐, 等. 黑龙江省漠河县砂宝斯金矿床流体特征及矿床成因[J]. 地球科学——中国地质大学学报, 2015, 40(7): 1163-1176. Google Scholar Li L, Sun F Y, Li B L, et al. Ore-forming fluid features and genesis of Shabaosi gold deposit in Mohe County, Heilongjiang Province[J]. Earth Science-Journal of China University of Geosciences, 2015, 40(7): 1163-1176. Google Scholar
[52]	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. doi: 10.3321/j.issn:0563-5020.2007.01.011 CrossRef Google Scholar 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. doi: 10.3321/j.issn:0563-5020.2007.01.011 CrossRef Google Scholar
[53]	刘宝山, 程招勋, 邵军, 等. 黑龙江嫩江-黑河地区铜金多金属找矿新进展及勘查方向[J]. 地质与资源, 2022, 31(3): 331-341. doi: 10.13686/j.cnki.dzyzy.2022.03.008 CrossRef Google Scholar Liu B S, Cheng Z X, Shao J, et al. Latest prospecting progress and exploration direction of copper-gold polymetallic deposits in Nenjiang-Heihe area, Heilongjiang Province[J]. Geology and Resources, 2022, 31(3): 331-341. doi: 10.13686/j.cnki.dzyzy.2022.03.008 CrossRef Google Scholar
[54]	付忠才. 黑龙江省呼玛县北西里钒钛磁铁矿成矿岩体特征[J]. 中国金属通报, 2019(11): 61, 63. Google Scholar Fu Z C. Characteristics of ore-forming rock mass of vanadium-titanium magnetite in Beili, Huma County, Heilongjiang Province[J]. China Metal Bulletin, 2019(11): 61, 63. (in Chinese) Google Scholar
[55]	王朝亮. 黑龙江省新林区小柯勒河铜(钼)矿成矿与找矿模型研究[D]. 长春: 吉林大学, 2018: 1-72. Google Scholar Wang C L. Study on the mineralization and prospecting model of Xiaokele River copper (molybdenum) ore in Xinlin District, Heilongjiang Province[D]. Changchun: Jilin University, 2018: 1-72. Google Scholar
[56]	孟凡波, 邓昌州, 冯雨周, 等. 大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义[J]. 矿物岩石地球化学通报, 2021, 40(4): 914-924. Google Scholar Meng F B, Deng C Z, Feng Y Z, et al. Mineral geochemistry of biotites from the mineralized intrusive bodies in the Late Mesozoic porphyry Cu-Mo deposits, northern Great Xing'an range and its geological implications[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2021, 40(4): 914-924. Google Scholar
[57]	汤中立. 中国的小岩体岩浆矿床[J]. 中国工程科学, 2002, 4(6): 9-12. doi: 10.3969/j.issn.1009-1742.2002.06.003 CrossRef Google Scholar Tang Z L. Magmatic ore deposits in small rockbody in China[J]. Engineering Science, 2002, 4(6): 9-12. doi: 10.3969/j.issn.1009-1742.2002.06.003 CrossRef Google Scholar
[58]	李文渊, 张照伟, 陈博. 小岩体成大矿的理论与找矿实践意义——以西北地区岩浆铜镍硫化物矿床为例[J]. 中国工程科学, 2015, 17(2): 29-34. doi: 10.3969/j.issn.1009-1742.2015.02.004 CrossRef Google Scholar Li W Y, Zhang Z W, Chen B. The theory on small intrusions forminglarge deposits and its explorationsignificance: Taking for magmatic Ni-Cu sulfide deposits example in the northwestern of China[J]. Engineering Sciences, 2015, 17(2): 29-34. doi: 10.3969/j.issn.1009-1742.2015.02.004 CrossRef Google Scholar
[59]	陈志广, 张连昌, 卢百志, 等. 内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义[J]. 岩石学报, 2010, 26(5): 1437-1449. Google Scholar Chen Z G, Zhang L C, Lu B Z, et al. Geochronology and geochemistry of the Taipingchuan copper-molybdenum deposit in Inner Mongolia, and its geological significances[J]. Acta Petrologica Sinica, 2010, 26(5): 1437-1449. Google Scholar
[60]	侯召硕. 内蒙古额尔古纳地区八大关铜钼矿床成因与构造背景[D]. 长春: 吉林大学, 2014: 1-56. Google Scholar Hou Z S. Ore genesis and tectonic setting of Badaguan copper-molybdenum deposit in Erguna region, Inner Mongolia[D]. Changchun: Jilin University, 2014: 1-56. Google Scholar
[61]	刘翼飞, 聂凤军, 江思宏, 等. 蒙古国阿林诺尔钼矿床赋矿花岗岩年代学及地球化学特征[J]. 地球学报, 2010, 31(3): 343-349. Google Scholar Liu Y F, Nie F J, Jiang S H, et al. The geochronology and geochemical features of ore-hosting granite in the Aryn Nuur molybdenum deposit, Mongolia[J]. Acta Geoscientica Sinica, 2010, 31(3): 343-349. Google Scholar
[62]	Wang W, Tang J, Xu W L, et al. Geochronology and geochemistry of Early Jurassic volcanic rocks in the Erguna massif, Northeast China: Petrogenesis and implications for the tectonic evolution of the Mongol-Okhotsk suture belt[J]. Lithos, 2015, 218-219: 73-86. doi: 10.1016/j.lithos.2015.01.012 CrossRef Google Scholar
[63]	葛文春, 隋振民, 吴福元, 等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J]. 岩石学报, 2007, 23(2): 423-440. Google Scholar Ge W C, Sui Z M, Wu F Y, et al. Zircon U-Pb ages, Hf isotopic characteristics and their implications of the Early Paleozoic granites in the northeastern Da Hinggan Mts., northeastern China[J]. Acta Petrologica Sinica, 2007, 23(2): 423-440. Google Scholar
[64]	褚少雄, 刘建明, 徐九华, 等. 黑龙江三矿沟铁铜矿床花岗闪长岩锆石U-Pb定年、岩石成因及构造意义[J]. 岩石学报, 2012, 28(2): 433-450. Google Scholar Chu S X, Liu J M, Xu J H, et al. Zircon U-Pb dating, petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit, Heilongjiang Province[J]. Acta Petrologica Sinica, 2012, 28(2): 433-450. Google Scholar
[65]	盛继福, 傅先政. 大兴安岭中段成矿环境与铜多金属矿床地质特征[M]. 北京: 地震出版社, 1999. Google Scholar Sheng J F, Fu X Z. Metallogenic environment and geological characteristics of copper polymetallic deposit in the middle part of the Greater Hinggan Mountains[M]. Beijing: Seismological Press, 1999. (in Chinese) Google Scholar
[66]	Cooke D R, Hollings P, Walshe J L. Giant porphyry deposits: Characteristics, distribution, and tectonic controls[J]. Economic Geology, 2005, 100(5): 801-818. doi: 10.2113/gsecongeo.100.5.801 CrossRef Google Scholar
[67]	Asadi S, Moore F, Zarasvandi A. Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcano-plutonic belt, Kerman region, Iran: A review[J]. Earth-Science Reviews, 2014, 138: 25-46. doi: 10.1016/j.earscirev.2014.08.001 CrossRef Google Scholar
[68]	Deng C Z, Sun G Y, Sun D Y, et al. Origin of C type adakite magmas in the NE Xing'an block, NE China and tectonic implication[J]. Acta Geochimica, 2018, 37(2): 281-294. doi: 10.1007/s11631-017-0190-2 CrossRef Google Scholar
[69]	芮宗瑶, 张立生, 陈振宇, 等. 斑岩铜矿的源岩或源区探讨[J]. 岩石学报, 2004, 20(2): 229-238. Google Scholar Rui Z Y, Zhang L S, Chen Z Y, et al. Approachon source rock or source region of porphyry copper deposits[J]. Acta Petrologica Sinica, 2004, 20(2): 229-238. Google Scholar