Shenyang Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2024 Vol. 33, No. 4
Article Contents
Article navigation > Geology and Resources > 2024 > 33(4): 467-492
Next Article Previous Article

ZHANG Peng, LYU Jun-chao, ZHAO Yan, KOU Lin-lin, YANG Hong-zhi, BI Zhong-wei, SHA De-ming, YANG Zhong-zhu, LI Dong-tao, LIU Chang-chun. CHARACTERISTICS, MINERALIZATION AND RESOURCE POTENTIAL OF ENDOGENOUS GOLD DEPOSITS IN LIAODONG PENINSULA[J]. Geology and Resources, 2024, 33(4): 467-492. doi: 10.13686/j.cnki.dzyzy.2024.04.004
Citation: ZHANG Peng, LYU Jun-chao, ZHAO Yan, KOU Lin-lin, YANG Hong-zhi, BI Zhong-wei, SHA De-ming, YANG Zhong-zhu, LI Dong-tao, LIU Chang-chun. CHARACTERISTICS, MINERALIZATION AND RESOURCE POTENTIAL OF ENDOGENOUS GOLD DEPOSITS IN LIAODONG PENINSULA[J]. Geology and Resources, 2024, 33(4): 467-492. doi: 10.13686/j.cnki.dzyzy.2024.04.004
shu

CHARACTERISTICS, MINERALIZATION AND RESOURCE POTENTIAL OF ENDOGENOUS GOLD DEPOSITS IN LIAODONG PENINSULA

  • 1.

    Shenyang Center of China Geological Survey, Shenyang 110034, China

  • 2.

    Mudanjiang Natural Resources Comprehensive Survey Center, CGS, Mudanjiang 157021, Heilongjiang Province, China

More Information
Received Date:  21 July 2023
Revised Date:  28 July 2023
Publish Date:  25 August 2024
    Abstract

  • Liaodong Peninsula is an important part of North China Craton, where intense tectonic movement, magmatic activities and gold mineralization occurred in Mesozoic, and gold deposits of different scales are distributed with typical regional characteristics. Through the systematic summary of basic characteristics such as spatial distribution, ore-bearing wall rock, ore-controlling structures and mineralized alteration, as well as the metallogenesis of gold deposits, the paper analyzes the resources potential of gold deposits in Liaodong Peninsula. According to the spatial distribution of gold deposits, four gold deposit concentration areas are divided, including Maoling, Baiyun-Qingchengzi, Wulong-Sidaogou and Xinfang gold deposit concentration areas. The ore-bearing wall rocks of Maoling and Baiyun-Qingchengzi concentration areas are Paleoproterozoic sedimentary metamorphic rock series, with the mineralization of altered rock type and quartz vein type, and the orebodies mainly controlled by low-angle interlayer faults. The wall rocks of Wulong-Sidaogou concentration area are Middle Jurassic gneissic biotite granite and Paleoproterozoic sedimentary metamorphic rock series respectively, with the main mineralization of quartz vein type, followed by altered rock type, and the orebodies controlled by high-angle fault and low-angle interlayer fault. The wall rocks of Xinfang concentration area are Archean gneisses and Neoproterozoic Qingbaikouan metamorphic sandstone, granulite and marble, with the mineralization of quartz vein type and altered rock type. The orebodies are mostly in veins and controlled by the ductile-brittle secondary faults developed in the foot wall of metamorphic core complex detachment fault and by the structural fractures in the Neoproterozoic Qingbaikouou cap rock. The geochronological study shows that the gold mineralization epoch can be divided into Late Triassic (~220 Ma), Early Jurassic (~190 Ma) and Early Cretaceous (~120 Ma). The study on fluid inclusions indicates that fluid immiscibility is the main mechanism of gold mineralization. The H-O isotopes reveal the ore-forming fluid mainly comes from magmatic water, with atmospheric precipitation added in later period. The He-Ar isotopes show that the ore-forming fluid is mainly derived from crustal source and a little from mantle source. The S-Pb-Sr isotopes indicate that the metallogenic materials mainly come from the Mesozoic magma. Besides, the ore-bearing strata play an indispensable role. The geological characteristics and isotopic data show that the gold deposits in Liaodong Peninsula are of magmatic hydrothermal origin. Combined with regional tectonic evolution, it is believed that the Late Triassic gold deposits in the area are related to the deep subduction of Yangtze plate to North China plate, the Early Jurassic gold deposits related to the subduction and compression of Paleo-Pacific plate to Eurasian plate, and the Early Cretaceous gold deposits were formed in the subduction and exhumation extensional setting of Paleo-Pacific plate to Eurasian plate. According to the geological, regional geochemical and geophysical characteristics of typical deposits, 23 prospecting targets are delineated and 2 414.56 t of gold resources at 3 000 m below surface are predicted.

    • FullText(HTML)
  • 加载中
    • References
  • [1] 宋明春, 宋英昕, 丁正江, 等. 胶东金矿床: 基本特征和主要争议[J]. 黄金科学技术, 2018, 26(4): 406-422.

    Google Scholar

    Song M C, Song Y X, Ding Z J, et al. Jiaodong gold deposits: Essential characteristics and major controversy[J]. Gold Science and Technology, 2018, 26(4): 406-422.

    Google Scholar

    [2] 薛春纪, 陈毓川, 路远发, 等. 辽东青城子矿集区金、银成矿时代及地质意义[J]. 矿床地质, 2003, 22(2): 177-184. doi: 10.3969/j.issn.0258-7106.2003.02.009

    CrossRef Google Scholar

    Xue C J, Chen Y C, Lu Y F, et al. Metallogenic epochs of Au and Ag deposits in Qingchengzi ore-clustered area, eastern Liaoning Province[J]. Mineral Deposits, 2003, 22(2): 177-184. doi: 10.3969/j.issn.0258-7106.2003.02.009

    CrossRef Google Scholar

    [3] 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.

    Google Scholar

    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.

    Google Scholar

    [4] 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.

    Google Scholar

    Zeng Q D, Chen R Y, Yang J H, et al. The metallogenic characteristics and exploring ore potential of the gold deposits in eastern Liaoning Province[J]. Acta Petrologica Sinica, 2019, 35(7): 1939-1963.

    Google Scholar

    [5] 孙立民, 孙文涛, 赵广繁. 青城子矿田小佟家堡子金银矿床地质特征及成矿物质来源探讨[J]. 黄金, 1997, 18(12): 13-18.

    Google Scholar

    Sun L M, Sun W T, Zhao G F. Geological characteristics of Xiaotongjiabaozi gold-silver deposit of Qingchengzi ore field and it source of mineralized matter[J]. Gold, 1997, 18(12): 13-18.

    Google Scholar

    [6] Yu G, Yang G, Chen J F, et al. Re-Os dating of gold-bearing arsenopyrite of the Maoling gold deposit, Liaoning Province, Northeast China and its geological significance[J]. Chinese Science Bulletin, 2005, 50(14): 1509-1514. doi: 10.1360/04wd0229

    CrossRef Google Scholar

    [7] 朱日祥, 范宏瑞, 李建威, 等. 克拉通破坏型金矿床[J]. 中国科学: 地球科学, 2015, 45(8): 1153-1168.

    Google Scholar

    Zhu R X, Fan H R, Li J W, et al. Decratonic gold deposits[J]. Science China Earth Science, 2015, 58(9): 1523-1537.

    Google Scholar

    [8] Feng H X, Shen P, Zhu R X, et al. Precise ages of gold mineralization and pre-gold hydrothermal activity in the Baiyun gold deposit, northeastern China: In situ U-Pb dating of hydrothermal xenotime and rutile[J]. Mineralium Deposita, 2022, 57(6): 1001-1022. doi: 10.1007/s00126-021-01082-z

    CrossRef Google Scholar

    [9] Liu S J, Chen B, Zheng J H, et al. Genesis of the Xinfang gold deposit, Liaodong Peninsula: Insights from fluid inclusions and S-Sr isotopic constraints[J]. Journal of Earth Science, 2021, 32(1): 68-80. doi: 10.1007/s12583-020-1074-7

    CrossRef Google Scholar

    [10] Sengör A M C, Natal'in B A. Paleotectonics of Asia: Fragments of a synthesis[C]//Yin A, Harrison T M. The Tectonic Evolution of Asia. Cambridge: Cambridge University Press, 1996: 486-640.

    Google Scholar

    [11] Deng J, Wang Q F. Gold mineralization in China: Metallogenic provinces, deposit types and tectonic framework[J]. Gondwana Research, 2016, 36: 219-274. doi: 10.1016/j.gr.2015.10.003

    CrossRef Google Scholar

    [12] Li Y J, Li S R, Santosh M, et al. Isotope geochemistry and geochronology of the Niujuan silver deposit, northern North China Craton: Implications for magmatism and metallogeny in an extensional tectonic setting[J]. Ore Geology Reviews, 2017, 90: 36-51. doi: 10.1016/j.oregeorev.2017.10.004

    CrossRef Google Scholar

    [13] Zhang P, Kou L L, Zhao Y, et al. Genesis of the Wulong gold deposit, Liaoning Province, NE China: Constrains from noble gases, radiogenic and stable isotope studies[J]. Geoscience Frontiers, 2020, 11(2): 547-563. doi: 10.1016/j.gsf.2019.05.012

    CrossRef Google Scholar

    [14] Zhang P, Kou L L, Zhao Y. Three periods of gold mineralization in the Liaodong Peninsula, North China Craton[J]. International Geology Review, 2022, 64(20): 2922-2940. doi: 10.1080/00206814.2021.2009046

    CrossRef Google Scholar

    [15] Wu F Y, Zhang Y B, Yang J H, et al. Zircon U-Pb and Hf isotopic constraints on the Early Archean crustal evolution in Anshan of the North China Craton[J]. Precambrian Research, 2008, 167(3/4): 339-362.

    Google Scholar

    [16] 孟恩, 刘福来, 刘平华, 等. 辽东半岛东北部宽甸地区南辽河群沉积时限的确定及其构造意义[J]. 岩石学报, 2013, 29(7): 2465-2480.

    Google Scholar

    Meng E, Liu F L, Liu P H, et al. Depositional ages and tectonic implications for South Liaohe Group from Kuandian area in northeastern Liaodong Peninsula, Northeast China[J]. Acta Petrologica Sinica, 2013, 29(7): 2465-2480.

    Google Scholar

    [17] Xu W, Liu F L. Geochronological and geochemical insights into the tectonic evolution of the Paleoproterozoic Jiao-Liao-Ji Belt, Sino-Korean Craton[J]. Earth-Science Reviews, 2019, 193: 162-198. doi: 10.1016/j.earscirev.2019.04.019

    CrossRef Google Scholar

    [18] Lu X P, Wu F Y, Guo J H, et al. Zircon U-Pb geochronological constraints on the Paleoproterozoic crustal evolution of the eastern block in the North China Craton[J]. Precambrian Research, 2016, 146(3/4): 138-164.

    Google Scholar

    [19] Luo Y, Sun M, Zhao G C, et al. A comparison of U-Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe groups: Constraints on the evolution of the Jiao-Liao-Ji Belt, North China Craton[J]. Precambrian Research, 2018, 163(3/4): 279-306.

    Google Scholar

    [20] Wang H Z, Mo X X. An outline of the tectonic evolution of China[J]. Episodes, 1995, 18(1/2): 6-16.

    Google Scholar

    [21] Yang J H, Wu F Y, Wilde S A, et al. Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China Craton[J]. Chemical Geology, 2007, 242(1/2): 155-175.

    Google Scholar

    [22] Wu F Y, Yang J H, Wilde S A, et al. Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE China[J]. Chemical Geology, 2005, 221(1/2): 127-156.

    Google Scholar

    [23] Yang J H, Sun J F, Zhang J H, et al. Petrogenesis of Late Triassic intrusive rocks in the northern Liaodong Peninsula related to decratonization of the North China Craton: Zircon U-Pb age and Hf-O isotope evidence[J]. Lithos, 2012, 153: 108-128. doi: 10.1016/j.lithos.2012.06.023

    CrossRef Google Scholar

    [24] Zhang P, Zhao Y, Kou L L, et al. Geochronology and geochemistry of the Late Triassic intrusive rocks in the Liaodong Peninsula, NE China: Petrogenesis and implications for Early Mesozoic tectonic evolution[J]. International Geology Review, 2023, 65(2): 219-235. doi: 10.1080/00206814.2022.2042743

    CrossRef Google Scholar

    [25] 裴福萍. 辽南-吉南中生代侵入岩锆石U-Pb年代学和地球化学: 对华北克拉通破坏时空范围的制约[D]. 长春: 吉林大学, 2008: 1-186.

    Google Scholar

    Pei F P. Zircon U-Pb chronology and geochemistry of Mesozoic intrusive rocks in southern Liaoning and Jilin provinces: Constraints on the spatial-temporal extent of the North China Craton destruction[D]. Changchun: Jilin University, 2008: 1-186.

    Google Scholar

    [26] 王玉往, 解洪晶, 李德东, 等. 矿集区找矿预测研究——以辽东青城子铅锌-金-银矿集区为例[J]. 矿床地质, 2017, 36(1): 1-24.

    Google Scholar

    Wang Y W, Xie H J, Li D D, et al. Prospecting prediction of ore concentration area exemplified by Qingchengzi Pb-Zn-Au-Ag ore concentration area, eastern Liaoning Province[J]. Mineral Deposits, 2017, 36(1): 1-24.

    Google Scholar

    [27] Zhang P, Kou L L, Zhao Y, et al. Fluid inclusions, H-O, S, Pb, and noble gas isotope studies of the Baiyun gold deposit in the Qingchengziorefield, NE China[J]. Journal of Geochemical Exploration, 2019, 200: 37-53. doi: 10.1016/j.gexplo.2019.01.016

    CrossRef Google Scholar

    [28] Zhang P, Zhao Y, Chai P, et al. Geochemistry, zircon U-Pb analysis, and biotite 40Ar/39Ar geochronology of the Maoling gold deposit, Liaodong rift, NE China[J]. Resource Geology, 2017, 67(4): 426-441. doi: 10.1111/rge.12133

    CrossRef Google Scholar

    [29] Feng H X, Shen P, Zhu RX, et al. Geology and He-Ar-S-Pb isotope constraints on thegenesis of the Sidaogou gold deposit in Liaodong Peninsula, northeastern North China Craton[J]. Ore Geology Reviews, 2019, 113: 103080. doi: 10.1016/j.oregeorev.2019.103080

    CrossRef Google Scholar

    [30] 仲米山, 张国仁, 杨中柱, 等. 辽东半岛南部早白垩世变质核杂岩时空分布及动力学特征[J]. 地质与资源, 2020, 29(5): 411-418.

    Google Scholar

    Zhong M S, Zhang G R, Yang Z Z, et al. Spatiotemporal distribution and dynamic characteristics of the Early Cretaceous metamorphic core complexes in southern Liaodong Peninsula[J]. Geology and Resources, 2020, 29(5): 411-418.

    Google Scholar

    [31] 宋运红, 杨凤超, 闫国磊, 等. 辽东地区古元古代花岗岩SHRIMP U-Pb年龄、Hf同位素组成及构造意义[J]. 地质学报, 2016, 90(10): 2620-2636. doi: 10.3969/j.issn.0001-5717.2016.10.006

    CrossRef Google Scholar

    Song Y H, Yang F C, Yan G L, et al. SHRIMP U-Pb ages and Hf isotopic compositions of paleoproterozoic granites from the eastern part of Liaoning Province and their tectonic significance[J]. Acta Geologica Sinica, 2016, 90(10): 2620-2636. doi: 10.3969/j.issn.0001-5717.2016.10.006

    CrossRef Google Scholar

    [32] Yu G, Chen J F, Xue C J, et al. Geochronological framework and Pb, Sr isotope geochemistry of the Qingchengzi Pb-Zn-Ag-Au orefield, northeastern China[J]. Ore Geology Reviews, 2009, 35(3/4): 367-382.

    Google Scholar

    [33] 张朋, 杨宏智, 李斌, 等. 辽东青城子矿集区姚家沟钼矿床成矿物质来源、成矿年代及成矿动力学背景[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1684-1696.

    Google Scholar

    Zhang P, Yang H Z, Li B, et al. Ore source, ore-forming age and geodynamic setting of Yaojiagou molybdenum deposit in Qingchengzi ore-clustered area, eastern Liaoning Province[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(6): 1684-1696.

    Google Scholar

    [34] 张朋, 赵岩, 寇林林, 等. 辽东青城子矿田煌斑岩锆石U-Pb年龄及其地质意义[J]. 东北大学学报(自然科学版), 2016, 37(7): 1056-1060. doi: 10.3969/j.issn.1005-3026.2016.07.030

    CrossRef Google Scholar

    Zhang P, Zhao Y, Kou L L, et al. Zircon U-Pb dating and its geological significance of lamprophyres from Qingchengzi Orefield, Liaodong[J]. Journal of Northeastern University (Natural Science), 2016, 37(7): 1056-1060. doi: 10.3969/j.issn.1005-3026.2016.07.030

    CrossRef Google Scholar

    [35] 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.

    Google Scholar

    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.

    Google Scholar

    [36] 孙文涛, 孙吉国, 孙红云, 等. 青城子矿田杨树区超大型金银铅锌矿床地质特征及成矿机理[J]. 地质与勘探, 2008, 44(4): 24-30.

    Google Scholar

    Sun W T, Sun J G, Sun H Y, et al. Geology and mineralization of superlarge Yangshuqu Au-Ag-Pb-Zn deposit in the Qinchengzi mine field[J]. Geology and Exploration, 2008, 44(4): 24-30.

    Google Scholar

    [37] Liu J, Liu F X, Li S H, et al. Formation of the Baiyun gold deposit, Liaodong gold province, NE China: Constraints from zircon U-Pb age, fluid inclusion, and C-H-O-Pb-He isotopes[J]. Ore Geology Review, 2019, 104: 686-706. doi: 10.1016/j.oregeorev.2018.12.006

    CrossRef Google Scholar

    [38] Sun G T, Zeng Q D, Zhou L L, et al. Trace element contents and in situ sulfur isotope analyses of pyrite in the Baiyun gold deposit, NE China: Implication for the genesis of intrusion-related gold deposits[J]. Ore Geology Reviews, 2020, 118: 103330. doi: 10.1016/j.oregeorev.2020.103330

    CrossRef Google Scholar

    [39] Liu J, Liu F X, Li S H, et al. Genesis of the Xiaotongjiapuzi gold deposit of the Liaodong gold province, Northeast China: Fluid inclusion thermometry and S-Pb-H-O-He isotope constraints[J]. Geological Journal, 2020, 55(1): 1023-1040. doi: 10.1002/gj.3454

    CrossRef Google Scholar

    [40] 孙国强, 孙启明, 郑廷. 辽宁青城子矿田桃源金矿床地质特征及成矿机制探讨[J]. 甘肃冶金, 2008, 30(6): 49-51.

    Google Scholar

    Sun G Q, Song Q M, Zheng T. Geological characteristics and causes of Taoyuan gold deposit in Liaoning Qingchengzi[J]. Gansu Metallurgy, 2008, 30(6): 49-51.

    Google Scholar

    [41] Yu B, Zeng Q D, Frimmel H E, et al. Genesis of the Wulong gold deposit, northeastern North China Craton: Constraints from fluid inclusions, H-O-S-Pb isotopes, and pyrite trace element concentrations[J]. Ore Geology Reviews, 2008, 102: 313-337.

    Google Scholar

    [42] Yu B, Zeng Q D, Frimmel H E, et al. The 127 Ma gold mineralization in the Wulong deposit, Liaodong Peninsula, China: constraints from molybdenite Re-Os, monazite U-Th-Pb, and zircon U-Pb geochronology[J]. Ore Geology Reviews, 2020, 121: 103542. doi: 10.1016/j.oregeorev.2020.103542

    CrossRef Google Scholar

    [43] Chen C, Li D T, Wu T T, et al. Genesis of gold deposits in the Wulong orefield, Liaodong Peninsula, North China Craton: Constraints from ore deposit geology, REE, and C-H-O-S-Pb isotopes[J]. Geological Journal, 2020, 55(8): 5914-5933. doi: 10.1002/gj.3661

    CrossRef Google Scholar

    [44] 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.

    Google Scholar

    Liu J, Li T G, Duan C. Geochronology and isotopic geochemistry characteristics of the Maoling large gold deposit, Liaoning Province, China[J]. Geological Bulletin of China, 2018, 37(7): 1325-1337.

    Google Scholar

    [45] 孙宝亮, 梁俊红, 姚玉增, 等. 猫岭-王家崴子金成矿带铅同位素地球化学特征[J]. 辽宁地质, 2000, 17(4): 259-262.

    Google Scholar

    Sun B L, Liang J H, Yao Y Z, et al. Geochemical characteristics of lead isotope in Maoling-Wangjiawaizi gold metallogenic belt[J]. Liaoning Geology, 2000, 17(4): 259-262.

    Google Scholar

    [46] 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.

    Google Scholar

    Hao R X, Peng S L. Geochemical study of Wangjiawaizi gold deposit in Liaoning[J]. Gold Geology, 1999, 5(2): 47-51.

    Google Scholar

    [47] 郭大招, 魏俊浩, 张可清, 等. 辽东庄河金矿同位素地球化学特征及成矿时代[J]. 地质学报, 2005, 79(5): 671-678.

    Google Scholar

    Guo D Z, Wei J H, Zhang K X, et al. The isotope geochemical characteristics and ore-forming time of Zhuanghe gold deposit, eastern Liaoning[J]. Acta Geologica Sinica, 2005, 79(5): 671-678.

    Google Scholar

    [48] Zhang P, Zhao Y, Kou L L, et al. Genesis of the Xinfang gold deposit, Liaodong Peninsula: Constraints from fluid inclusions, H-O-S-Pb isotopes, pyrite trace element concentrations, and chronology[J]. Gondwana Research, 2023, 113: 210-231. doi: 10.1016/j.gr.2022.11.002

    CrossRef Google Scholar

    [49] Zhang P, Zhao Y, Kou L L, et al. Genesis of the Xinfang magmatic-hydrothermal gold deposit, Liaodong Peninsula, China: Constraints from pyrite Re-Os isotopes, C, O, S, Pb, Si, He and Ar isotopes[J]. Ore Geology Reviews, 2022, 148: 105025.

    Google Scholar

    [50] 冯啸宇. 辽南盖县组地层中金矿床地质特征及找矿方向[J]. 地质与资源, 2011, 20(1): 36-69.

    Google Scholar

    Feng X Y. Geologic characteristics and prospecting direction of gold deposits in Gaixian formation in southern Liaoning Province[J]. Geology and Resources, 2011, 20(1): 36-69.

    Google Scholar

    [51] 张朋, 陈冬, 寇林林, 等. 辽东卧龙泉岩体锆石U-Pb年龄、地球化学、Sr-Nd-Pb同位素特征及其构造意义[J]. 地质学报, 2015, 89(10): 1762-1772.

    Google Scholar

    Zhang P, Chen D, KouL L, et al. Geochronology, geochemistry and Sr-Nd-Pb isotopes of the Wolongquan intrusion in Liaodong and its tectonic significance[J]. Acta Geologica Sinica, 2015, 89(10): 1762-1772.

    Google Scholar

    [52] 刘文彬, 彭游博, 赵辰, 等. 辽南盖州卧龙泉岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征[J]. 地质与资源, 2018, 27(6): 531-539.

    Google Scholar

    Liu W B, Peng Y B, Zhao C, et al. LA-ICP-MS zircon U-Pb dating and geochemistry of Wolongquan intrusion in Gaizhou, Southern Liaoning Province[J]. Geology and Resources, 2018, 27(6): 531-539.

    Google Scholar

    [53] 杨进辉, 吴福元, 谢烈文, 等. 辽东矿洞沟正长岩成因及其构造意义: 锆石原位微区U-Pb年龄和Hf同位素制约[J]. 岩石学报, 2007, 23(2): 263-276.

    Google Scholar

    Yang J H, Wu F Y, Xie L W, et al. Petrogenesis and tectonic implications of Kuangdonggou syenites in the Liaodong Peninsula, east North China Croton: Constraints from in-situ zircon U-Pb ages and Hf isotopes[J]. Acta Petrologica Sinica, 2007, 23(2): 263-276.

    Google Scholar

    [54] 徐山. 辽东地区金矿矿产资源评价[D]. 长春: 吉林大学, 2013: 1-158.

    Google Scholar

    Xu S. The mineral resources assessment of gold deposits in eastern Liaoning[D]. Changchun: Jilin University, 2013: 1-158.

    Google Scholar

    [55] 余昌涛, 贾斌, 刘斌. 辽宁省盖县猫岭金矿床地质特征及成因探讨[J]. 贵金属地质, 1992, 1(1): 37-47.

    Google Scholar

    Yu C T, Jia B, Liu B. Geological characteristic and genesis of Maoling gold deposit in Liaoning Province[J]. Journal of Precious Metallic Geology, 1992, 1(1): 37-47.

    Google Scholar

    [56] 吴福元, 杨进辉, 柳小明. 辽东半岛中生代花岗质岩浆作用的年代学格架[J]. 高校地质学报, 2005, 11(3): 305-317.

    Google Scholar

    Wu F Y, Yang J H, LiuX M. Geochronological framework of the Mesozoic granitic magmatism in the Liaodong Peninsula, Northeast China[J]. Geological Journal of China Universities, 2005, 11(3): 305-317.

    Google Scholar

    [57] 张朋, 赵岩, 寇林林, 等. 辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义[J]. 地球科学, 2019, 44(10): 3297-3313.

    Google Scholar

    Zhang P, Zhao Y, Kou L L, et al. Zircon U-Pb ages, Hf isotope sand geological significance of Mesozoic granites in Dandong area, Liaodong Peninsula[J]. Earth Science, 2019, 44(10): 3297-3313.

    Google Scholar

    [58] 仲米山, 张国仁, 高福亮, 等. 辽南新房变质核杂岩的发现及地质意义[J]. 地质科学, 2021, 56(1): 272-287.

    Google Scholar

    Zhong M S, Zhang G R, Gao F L, et al. Discovery and geological implication of Xinfang metamorphic core complex in southern Liaoning[J]. Chinese Journal of Geology, 2021, 56(1): 272-287.

    Google Scholar

    [59] 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.

    Google Scholar

    Liu G P, Ai Y F. Studies on the mineralization age of Baiyung old deposit in Liaoning[J]. Acta Petrologica Sinica, 2000, 16(4): 627-632.

    Google Scholar

    [60] 周国超, 王玉往, 李德东, 等. 辽东白云金矿区脉岩锆石的U-Pb年代学研究[J]. 矿物岩石地球化学通报, 2017, 36(4): 620-627.

    Google Scholar

    Zhou G C, Wang Y W, Li D D, et al. LA-ICP-MS zircon U-Pb dating of dykes from the Baiyun gold deposit in eastern Liaoning[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2017, 36(4): 620-627.

    Google Scholar

    [61] Sun G T, Zeng Q D, Li T Y, et al. Ore genesis of the Baiyun gold deposit in Liaoning Province, NE China: Constraints from fluid inclusions and zircon U-Pb ages[J]. Arabian Journal of Geosciences, 2019, 12(9): 299.

    Google Scholar

    [62] Sun G T, Zeng Q D, Zhou J X. Jurassic Au-Ag mineralization of the Linjiasandaogou deposit in the Liaodong Peninsula, Northeast China: Evidence from apatite U-Pb dating and the in situ geochemistry of sulfides[J]. Journal of Geochemical Exploration, 2023, 251: 107242.

    Google Scholar

    [63] Zhang P, Kou L L, Zhao Y, et al. Genesis of the Maoling gold deposit in the Liaodong Peninsula: Constraints from a combined fluid inclusion, C-H-O-S-Pb-He-Ar isotopic and geochronological studies[J]. Geoscience Frontiers, 2022, 13(4): 101379.

    Google Scholar

    [64] 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: 62-67.

    Google Scholar

    Zhang P. Metallogeniccharacteristics, oregenesis, diagenesis and metallogenic geodynamic process of precious and nonferrous metals ore deposits in southeast Liaoning Province[D]. Changchun: Jilin University, 2018: 62-67.

    Google Scholar

    [65] 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.

    Google Scholar

    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.

    Google Scholar

    [66] Liu J, Zhang L J, Wang S L, et al. Formation of the Wulong gold deposit, Liaodong gold province, NE China: Constraints from zircon U-Pb age, sericite Ar-Ar age, and H-O-S-He isotopes[J]. Ore Geology Reviews, 2019, 109: 130-143.

    Google Scholar

    [67] Feng H X, Shen P, Zhu R X, et al. SIMS U-Pb dating of vein-hosted hydrothermal rutile and carbon isotope of fluids in the Wulong lode gold deposit, NE China: Linking gold mineralization with craton destruction[J]. Ore Geology Reviews, 2020, 127: 103838.

    Google Scholar

    [68] 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.

    Google Scholar

    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.

    Google Scholar

    [69] 赵鸿志, 杨沈生, 李辉. 白云金矿床地质特征及成因探讨[J]. 有色矿冶, 2009, 25(3): 4-7.

    Google Scholar

    Zhao H Z, Yang S S, Li H. Geologic features of Baiyun gold ore deposit and discussion of the genesis[J]. Non-Ferrous Miningand Metallurgy, 2009, 25(3): 4-7.

    Google Scholar

    [70] 关广岳, 金成洙. 白云金矿床的成因[J]. 地质与勘探, 1983(10): 12-20.

    Google Scholar

    Guan G Y, Jin C Z. Genesis of Baiyun gold deposit[J]. Geology and Exploration, 1983(10): 12-20. (in Chinese)

    Google Scholar

    [71] 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.

    Google Scholar

    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.

    Google Scholar

    [72] 刘先利, 姜瑛, 刘志远. 青城子矿田高家堡子大型金银矿床地质特征及成矿机制[J]. 辽宁地质, 2000, 17(2): 121-127.

    Google Scholar

    Liu X L, Jiang Y, Liu Z Y. Geological characteristics and metallogenic mechanism of Gaojiapuzi large-scale Au-Ag deposits in Qingchengzi orefield[J]. Liaoning Geology, 2000, 17(2): 121-127.

    Google Scholar

    [73] 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.

    Google Scholar

    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.

    Google Scholar

    [74] 刘辉, 金成洙, 关广岳. 辽南猫岭金矿床的成矿物质来源及金的活化、迁移及富集机理[J]. 地质找矿论丛, 1990, 5(4): 57-68.

    Google Scholar

    Liu H, Jin C Z, Guan G Y. A mechanism study on the source of minerogenic material and the activation transportation and concentration of gold in Maoling gold deposit[J]. Contributions to Geology and Mineral Resources Research, 1990, 5(4): 57-68.

    Google Scholar

    [75] 成曦晖. 辽东中生代岩浆活动及金铀成矿作用[D]. 北京: 北京科技大学, 2017: 1-207.

    Google Scholar

    Cheng X H. Integrated research on Mesozoic magmatism and gold-uranium metallogenesis in the Liaodong Peninsula, Liaoning Province[D]. Beijing: University of Science and Technology, 2017: 1-207.

    Google Scholar

    [76] 吴兴华. 辽南马蹄形带金矿床层控-多因成矿模式[D]. 沈阳: 东北工学院, 1990: 1-99.

    Google Scholar

    Wu X H. Stratabound-polygenetic metallogenic model of the C-shaped gold deposit belt in southern Liaoning[D]. Shenyang: Northeastern Institute of Technology, 1990: 1-99. (in Chinese)

    Google Scholar

    [77] Chen J F, Yu G, Xue C J, et al. Pb isotope geochemistry of lead, zinc, gold and silver deposit clustered region, Liaodong rift zone, northeastern China[J]. Science in China Series D: Earth Sciences, 2005, 48(4): 467-476.

    Google Scholar

    [78] Yao X F, Yan T J, Lü Z C, et al. Ore-forming age and tectonic setting of the Linjiasandaogou gold deposit in the Liaodong Peninsula, Northeast China: Constraints from geochronology and geochemistry[J]. Acta Geochimica, 2022, 41(2): 244-266.

    Google Scholar

    [79] 李兆龙, 许文斗, 秦敏琪, 等. 辽宁五龙金矿地质特征及矿床成因[J]. 地质找矿论丛, 1987, 2(3): 31-39.

    Google Scholar

    Li Z L, Xu W D, Qin M Q, et al. Geological characteristics and ore genesis of Wulong gold deposits, Liaoning Province[J]. Contributions to Geology and Mineral Resources Research, 1987, 2(3): 31-39.

    Google Scholar

    [80] 刘国平, 艾永富. 辽宁白云金矿床某些基本问题探讨[J]. 矿床地质, 1999, 18(3): 219-225.

    Google Scholar

    Liu G P, Ai Y F. A discussion on some major problems of the Baiyun gold deposit, eastern Liaoning[J]. Mineral Deposits, 1999, 18(3): 219-225.

    Google Scholar

    [81] Faure G. Principles of isotope geology[M]. 2nd ed. New York: John Wiley and Sons, 1986: 1-589.

    Google Scholar

    [82] 赵岩, 张朋, 吕骏超, 等. 辽宁青城子矿田高家堡子银矿成矿流体特征及地质意义[J]. 地质与勘探, 2015, 51(3): 441-450.

    Google Scholar

    Zhao Y, Zhang P, Lü J C, et al. Characteristics of ore-forming fluids in the Gaojiapuzi Ag deposit of the Qingchengzi orefield, Liaoning Province and geological implications[J]. Geology and Exploration, 2015, 51(3): 441-450.

    Google Scholar

    [83] Stuart F M, Burnard P G, Taylor R P, et al. Resolving mantle and crustal contributions to ancient hydrothermal fluids: He-Ar isotopes in fluid inclusions from Dae Hwa W-Mo mineralisation, South Korea[J]. Geochimica et Cosmochimica Acta, 1995, 59(22): 4663-4673.

    Google Scholar

    [84] Burnard P G, Hu R, Turner G, et al. Mantle, crustal and atmospheric noble gases in Ailaoshan gold deposits, Yunnan Province, China[J]. Geochimica et Cosmochimica Acta, 1999, 63(10): 1595-1604.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(16)

Tables(2)

Export Citation
PDF
XML

Article Metrics

Article views(667) PDF downloads(99) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020