Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China
-
摘要: 五龙金矿床是辽东地区最大的石英脉型金矿床，矿区内矿体和岩脉受断裂构造控制明显.容矿构造几何学和运动学特征显示，早白垩世初近NS向挤压形成的近NS向张裂隙、共轭的剪裂隙及派生一对共轭剪裂隙奠定五龙金矿床的构造格架.早白垩世的伸展导致闪长岩脉、三股流岩体、五龙背岩体等沿着先存构造薄弱带内充填，出溶的岩浆热液流体沿着闪长岩充填残余空间继续充填形成石英脉.由于右形剪切变形导致石英脉发生碎裂，并伴随着区域伸展，赋存闪长岩脉和石英脉的构造空间复活，随后花岗岩脉等侵位及出溶的成矿流体通过闪长岩脉上侵的通道运移和充填于石英脉裂隙中并交代闪长岩脉和片麻状二长花岗岩，最后造就了岩脉-矿化-蚀变同构造空间共存的现象.通过成矿期运动学特征显示，NE向断裂带与胶东三山岛金矿带矿体群侧伏规律相似，断裂带北段深部具有找矿潜力.五龙矿区而言，NE向断裂的找矿潜力优于NW向断裂带，NE向断裂下盘平行断裂内张性空间是盲矿体的有利空间.本次首次获得了五龙金矿床辉钼矿-黄铁矿-磁黄铁矿-石英阶段辉钼矿Re-Os同位素模式年龄为125±2.1 Ma.辉钼矿中Re含量为12.8×10-6，显示成矿物质具有壳幔混合的特征.对比前人研究，钼矿化和金成矿均与早白垩世构造体制转换下中国东部强烈的壳幔岩浆活动有关，为同一构造背景下的产物.通过对比胶东地区的成矿系列，辽东地区与胶东地区具有极大的相似性，存在两期钼矿化作用，尤其早白垩世晚期钼矿化可以作为寻找金矿的标志之一.Abstract: The Wulong gold deposit is one of the most representative quartz-vein gold deposits in the Liaodong district in the NE China. The ore bodies and dikes are controlled by faults. The geometry,kinematics and kinetics characteristics of the ore-bearing structures indicate that the structural framework in the Wulong gold district is composed of the N-S tensile fracture,several NE-striking sinistral and NW-striking dextral conjugate faults and associated conjugate riedal fractures caused by the nearly N-S compression at the beginning of the Early Cretaceous. The diorites,Sanguliu pluton and Wulongbei pluton intruded into the pre-existing structures and NE-striking normal faults accompanied with the NW-SE extension during the Early Cretaceous. Hydrothermal fluid exsolution from the Early Cretaceous magmas migrated into the residual space in the fractures which were intruded by diorite. The dextral shear deformation led to the break of the quartz. The fractures infilled by granite dikes and quartz vines reactivated and the ore-forming fluids were characterized by vertical transport and lateral replacement in these fractures. The fluids infilled into the fractures of the broken quartz and replaced the Early Cretaceous dikes and gneissic monzonite granite. Therefore,the auriferous quartz veins share the similar space with the previous quartz and dikes. Kinetic characteristics of the ore-bearing structures indicate that the north of the NE-striking faults has the exploration potential and has a similar regularity for lateral trending of orebodies in the Sanshandao gold belt,Jiaodong district. In the Wulong gold district,the exploration potential of NE-striking faults is better than in the NW-striking faults and the tensile fractures in the footwall blocks of NE-striking faults are the advantageous space for searching for the concealed orebodies. This study first defines a molybdenite Re-Os isotopic model age of 125 ±2.1 Ma for the molybdenite-pyrite-pyrrhotite-quartz stage which represents the major ore-forming stage of the Wulong gold deposit. The Re concentrations of the molybdenite is 12.8×10-6,suggesting that ore-forming material contained a mixture of crustal and mantle components. The comparison of previous studies indicate that both of the molybdenum and gold mineralization are related with the intense crust-mantle magma activity in NE China. In comparison with the metallogenic series in the Jiaodong district,both of the Liaodong and Jiaodong have two stages of molybdenum mineralization. Especially,the late of the Early Cretaceous molybdenum mineralization could be one of the clues for gold prespecting in the Liaodong district.
-
Key words:
- structural control /
- molybdenite Re-Os dating /
- Wulong gold deposit /
- Liaodong /
- Jiaodong /
- geochronology
-
图 1 辽东金矿区地质简图及主要金矿和钼铜矿分布
Fig. 1. Geological map of the Liaodong Peninsula, showing the distribution of basements, Mesozoic igneous rocks and major gold deposits and molybdenum-copper deposits
图 2 五龙矿集区地质图与剖面图
a.据Feng et al.（2019）修编；b.据肖世椰等（2018）修编
Fig. 2. Geological maps of the Wulong gold district and a cross-section
图 3 五龙金矿床含金石英脉与片麻状二长花岗岩面理方向斜交
Fig. 3. Auriferous quartz veins cross-cut the gneissic monzonitic granite in the Wolong deposit
图 4 五龙金矿床含矿石英脉与岩浆岩平面图
Fig. 4. Geological map of the Wulong gold deposit, showing major dike rocks, auriferous quartz veins and faults
图 5 五龙金矿床辉钼矿-磁黄铁矿充填和交代自形-半自形黄铁矿
Fig. 5. Molybdenite intergrown with pyrrhotite and infilled in the pyrite or replaced the euhedral to subhedral pyrite
图 7 走滑断裂应力状态（a）、南北向挤压应力作用下可能的断裂组合（b）和走形力偶作用下可能的构造组合（c）
σ1.最大主应力；σ3.最小主应力；R.里德尔剪切；R’.方向里德尔剪切；P.与R剪切对称的P剪切破裂；I.第一序次构造；II.第二序次构造
Fig. 7. Strike-slip faults at or near the surface of the earth (a), fault pattern under the N-S compression (b) and a fault system marked by straight runs, jogs that restrain, and jogs that release (open) (c)
图 8 五龙金矿床22中段NW向163号矿体容矿构造变形特征
Fig. 8. Deformation characteristics of ore-bearing structures of No.163 orebody in the at -796 m in the Wulong gold deposit
图 9 五龙金矿床19中段NNE向80号矿体容矿构造变形特征
Fig. 9. Deformation characteristics of ore-bearing structures of No. 80 orebody in the at -638 m in the Wulong gold deposit
图 10 五龙金矿床48 m标高（二中段）矿脉分布(a)和五龙金矿床矿体横向投影(b)
a.辽宁省有色地质局一〇三队内部资料修编；b.据肖国洪等（2003）
Fig. 10. Planar map showing orebodies at 48 m (a) and the projection map of the major orebody in the Wulong gold deposit (b)
图 11 三山岛金矿带矿体垂直纵投影剖面
Fig. 11. The vertical projection of the major orebody in the Sanshandao ore belt
图 12 辽东五龙矿集区成岩成矿年龄频谱图
Fig. 12. Geochronology framework of the Wulong gold district and associated magmatism in the Liaodong Peninsula, NE China
表 1 五龙金矿床辉钼矿Re-Os同位素测试结果
Table 1. Re-Os isotopic analyses of molybdenite separating from the Wulong gold deposit
样号 样重（g） Re（ng/g） 普Os（ng/g） 187Re（ng/g） 187Os（ng/g） 模式年龄(Ma) WL19-2 0.031 41 12 766 ±146 0.027 8 ±0.023 9 8 023 ±92 16.7 ±0.1 125 ±2.1 
下载: 导出CSV
-
[1] Bureau of Geology and Mineral Resources of Liaoning Province, 1989. Regional Geology of Liaoning Province. Geological Publishing House, Beijing, 1-856 (in Chinese with English abstract). [2] Deng, J., Qiu, K.F., Wang, Q.F., et al., 2020a. In-Situ Dating of Hydrothermal Monazite and Implications on the Geodynamic Controls of Ore Formation in the Jiaodong Gold Province, Eastern China. Economic Geology, 115(3):671-685. doi: 10.5382/econgeo.4711 [3] Deng, J., Yang, L.Q., Groves, D.I., et al., 2020b. An Integrated Mineral System Model for the Gold Deposits of the Giant Jiaodong Province, Eastern China. Earth-Science Reviews. http://doi.org/10.1016/j.earscirev.2020.103274 [4] Deng, J., Wang, C. M., Bagas, L., et al., 2018. Crustal Architecture and Metallogenesis in the South-Eastern North China Craton. Earth-Science Reviews, 182:251-272. http://doi.org/10.1016/j.earscirev.2018.05.001. [5] Deng, J., Wang, Q. F., Li, G. J., 2017. Tectonic Evolution, Superimposed Orogeny, and Composite Metallogenic System in China. Gondwana Research, 50:216-266. http://doi.org/10.1016/j.gr.2017.02.005 [6] Ding, Z. J., Sun, F. Y., Liu, J. H., et al., 2012. Re-Os Dating of Molybdenites from the Xingjiashan Molybdenum-Tungsten Deposit in Jiaodong Peninsula, China and Its Geological Significance. Acta Petrologica Sinica, 28(9):2721-2732 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201209006.htm [7] Du, A.D., Qu, W.J., Li, C., et al., 2009, A Review on the Development of Re-Os Isotopic Dating Methods and Techniques. Rock and Mineral Analysis, 28(3):288-304 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS200903027.htm [8] Feng, H. X., Shen, P., Zhu, R. X., et al., 2019. Geology and He-Ar-S-Pb Isotope Constraints on the Genesis of the Sidaogou Gold Deposit in Liaodong Peninsula, Northeastern North China Craton. Ore Geology Reviews, 113:103080. http://doi.org/10.1016/j.oregeorev.2019.103080 [9] Guo, Q., 2019. Structural Regularity of Ore-Controlling and Mineralization Prediction of Wulong Gold Deposit in Liaodong (Dissertation). China University of Geosciences, Beijing, 1-66 (in Chinese with English abstract). [10] Li, J., Song, M. C., Wang, M. Y., et al., 2013. The Molybdenite Re-Os Age and Genetic Analysis of the Shangjiazhuang Mo Deposit in Jiaodong Area. Geology in China, 40(5):1612-1621 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_journal-jilin-university-earth-science-edition_thesis/0201247968429.html [11] Li, L., Zhou, X. W., 1992. Ore-Controlling Structures and Minerogenetic Prognosis of the Wulong Gold Deposit. Geology and Prospecting, 28(10):31-37 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT199210006.htm [12] Liu, J., Zhang, L. J., Wang, S. L., et al., 2019. 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. Ore Geology Reviews, 109:130-143. http://doi.org/10.1016/j.oreg eorev.2019.04.013 doi: 10.1016/j.oregeorev.2019.04.013 [13] Liu, S. B., Wang, D. H., Chen, Y. C., et al., 2011. Geological Characteristics and Molybdenite Re-Os Age of the Xingjiashan W-Mo Deposit in Yantai Area, Jiaodong Peninsula, Shandong Province. Geological Bulletin of China, 30(8):1294-1302 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201108016.htm [14] Lü, Y. F., Li, J. F., 1993. The Structural Characteristic of Ductile Shear Zone and Its Effect during Mineralization Process in Wulong Gold Deposit, Dandong. Earth Science, 18(4):415-424 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dqkx199304006.htm [15] Lü, Y. F., Li, J.F., Li, L., et al., 1994. Mineralization Type of Gold and Its Control Mechanism of Structure in Wulong Gold Deposit, Dandong, Liaoning Province. Geoscience, 8(3):309-316 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ403.010.htm [16] Ma, W. D., Fan, H. R., Liu, X., et al., 2017. Geochronological Framework of the Xiadian Gold Deposit in the Jiaodong Province, China:Implications for the Timing of Gold Mineralization. Ore Geology Reviews, 86:196-211. http://doi.org/10.1016/j.oregeorev.2017.02.016 [17] Qu, W.J., Du, A.D., 2003. Highly Precise Re-Os Dating of Molybdenite by ICP-MS with Carius Tube Sample Digestion. Rock and Mineral Analysis, 22(4):254-262 (in Chinese with English abstract). http://www.researchgate.net/publication/302500144_Highly_Precise_Re-Os_Dating_of_Molybdenite_by_ICP-MS_with_Carius_Tube_Sample_Digestion [18] Suzuki, K., Shimizu, H., Masuda, A., 1996. Re-Os Dating of Molybdenites from Ore Deposits in Japan:Implication for the Closure Temperature of the Re-Os System for Molybdenite and the Cooling History of Molybdenum Ore Deposits. Geochimica et Cosmochimica Acta, 60(16):3151-3159. doi: 10.1016/0016-7037(96)00164-0 [19] Wang, K. Y., Wan, D., Liu, Z. H., et al., 2011. Analysis of Structural Ore-Controlling Rules and Mechanism of the Sidaogou Gold Deposit in Dandong City, Liaoning Province. Journal of Jilin University (Earth Science Edition), 41(4):1048-1054 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ201104014.htm [20] Wei, J. H., Liu, C. Q., Zhao, Y. X., et al., 2001. Time Span of the Major Ore-Forming Stages of the Wulong Gold Deposit, Liaoning. Geological Review, 47(3):433-437 (in Chinese with English abstract). http://www.researchgate.net/publication/313722046_Time_span_of_the_major_ore-forming_stages_of_the_Wulong_gold_deposit_Liaoning [21] Wu, F. Y., Yang, J. H., Wilde, S. A., et al., 2005. Geochronology, Petrogenesis and Tectonic Implications of Jurassic Granites in the Liaodong Peninsula, NE China. Chemical Geology, 221:127-156. http://doi.org/10.1016/j.chemgeo.2005.04.010 [22] Xiao, G. H., Liu, T. X., Zhang, G. X., 2003. Probing into the Origin and Mineralization Model of Wulong Gold Deposit, Liaoning Province. Gold, 24:17-21 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HJZZ200311004.htm [23] Xiao, G. H., Zhang, G. X., 2004. Preliminary Analysis of West-North Fault Structure Ore Control in Wulong Gold Mine, Liaoning Province. Gold, 25:15-17 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HJZZ200409004.htm [24] Xiao, S. Y., 2019. Structural Evolution and Dike Emplacement Mechanism during Gold Mineralization in the Wulong Gold Mine Filed, Eastern Liaoning (Dissertation). Hefei University of Technology, Hefei, 1-74 (in Chinese with English abstract). [25] Xiao, S. Y., Zhu, G., Zhang, S., et al., 2018. Structural Processes and Dike Emplacement Mechanism in the Wulong Gold Field, Eastern Liaoning. Chinese Science Bulletin, 63(28):3022-3036 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTotal-KXTB2018Z2011.htm [26] Yang, C. F., 1997. The Characteristics of the Ore-Bearing Fractures and the Gold Orebody's Spatial Occurrence of Wulong Gold Deposit. Gold, 18(3):3-8 (in Chinese with English abstract). [27] Yang, C. F., Ji, Z. J., Zhang, G. X., et al., 1997. Restraining Mechanism of Veins in Wulong Gold Deposit on Au Orebodies. Geology and Prospecting, 33(6):7-11 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT199706001.htm [28] Yang, F. C., Yang, J. L., Gu, Y. C., et al., 2019. Emplacement and Deformation Age of Surrounding Gneissic Granite in Wulong Gold Deposit, Eastern Liaoning Province:SHRIMP U-Pb Age. Journal of Geomechanics, 25(Suppl.1):44-48 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLX2019S1008.htm [29] Yang, J.H., Wu, F. Y., Lo, C. H., et al., 2004. Deformation Age of Jurassic Granites in the Dandong Area, Eastern China:40Ar/39Ar Geochronological Constraints. Acta Petrologica Sinica, 20(5):1205-1214 (in Chinese with English abstract). http://www.oalib.com/paper/1472346 [30] Yang, J. H., Wu, F. Y., Wilde, S. A., 2003. A Review of the Geodynamic Setting of Large-Scale Late Mesozoic Gold Mineralization in the North China Craton:An Association with Lithospheric Thinning. Ore Geology Reviews, 23:125-152. http://doi.org/10.1016/S0169-1368(03)00033-7 [31] Yu, B., Zeng, Q. D., Frimmel, H. E., et al., 2018. Genesis of the Wulong Gold Deposit, Northeastern North China Craton:Constraints from Fluid Inclusions, H-O-S-Pb Isotopes, and Pyrite Trace Element Concentrations. Ore Geology Reviews, 102:313-337. http://doi.org/10.1016/j.oregeorev.2018.09.016 [32] Zhai, M. G., Zhu, R. X., Liu, J. M., et al., 2003. Key Time Limits for the Transition of the Mesozoic Structural System in Eastern North China. Science in China (Series D:Earth Sciences), 33 (10):913-920 (in Chinese). [33] Zhan, B. G., 1994. Geological Characteristics and Exploration Regularities of Wulong Gold Deposit. Journal of Materials and Metallurgy, 13:323-329 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/ http://search.cnki.net/down/default.aspx?filename=HUJI199404003&dbcode=CJFD&year=1994&dflag=pdfdown [34] Zhang, J. J., Ding, Z. J., Liu, D. H., et al., 2016. Exploration Practice and Prospecting Results of Super-Large Gold Mine of Sanshandao Northern Sea Area in Laizhou City, Shandong Province. Gold Science and Technology, 24(1):1-10 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HJKJ201601001.htm [35] Zhang, P., 2018. Metallogenic Characteristics, Ore Genesis, Diagenesis and Metallogenic Geodynamic Process of Precious and Nonferrous Metals Ore Deposits in Southeast Liaoning Province (Dissertation). Jilin University, Changchun, 1-229 (in Chinese with English abstract). [36] Zhang, P., Kou, L., Zhao, Y., et al., 2019. Genesis of the Wulong Gold Deposit, Liaoning Province, NE China:Constrains from Noble Gases, Radiogenic and Stable Isotope Studies. Geoscience Frontiers. http://doi.org/10.1016/j.gsf.2019.05.012 http://www.cqvip.com/QK/71129X/20202/7100979600.html [37] Zhang, P., Zhao, Y., Kou, L.L., et al., 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10):3297-3313 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201910010.htm [38] Zhang, X. O., 2002.Setting and Timing of Gold Mineralization in the Jiaodong and Liaodong Peninsulas, North China Craton (Dissertation). Curtin University of Technology, Perth, 1-236. http://www.researchgate.net/publication/44710158_Setting_and_timing_of_gold_mineralization_in_the_Jiadong_and_Liaodong_Peninsulas_North_China_Craton [39] Zhao, G. C., Cawood, P. A., Li, S. Z., et al., 2012. Amalgamation of the North China Craton:Key Issues and Discussion. Precambrian Research, 222-223:55-76. http://doi.org/10.1016/j.precamres.2012.09.016 [40] Zhao, G. C., Sun, M., Wilde, S. A., et al., 2005. Late Archean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited. Precambrian Research, 136:177-202. http://doi.org/10.1016/j.precamres.2004.10.002 [41] Zhao, Y., Chen, B., Zhang, S. H., et al., 2010. Pre-Yanshanian Geological Events in the Northern Margin of the North China Craton and Its Adjacent Areas. Geology in China, 37(4):900-915 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201004009.htm [42] Zhao, Y., Kou, L.L., Zhang, P., et al., 2019. Characteristics of Geochemistry and Hf Isotope from Meta- Gabbro in Longchang Area, Liaodong Peninsula:Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt. Earth Science, 44(10):3333-3345 (in Chinese with English abstract). [43] Zhou, W. J., Li, X.G., Qi, Z. H., et al., 2007. Relationship between Granite Porphyry and Ore-Forming in Liaoning Wulong Gold Area. Gold, 10(28):16-19 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_gold_thesis/0201219963870.html [44] Zhu, R. X., Chen, L., Wu, F. Y., et al., 2011. Timing, Scale and Mechanism of the Destruction of the North China Craton. Science in China (Series D:Earth Sciences), 41(5):583-592(in Chinese). http://gji.oxfordjournals.org/external-ref?access_num=10.1007/s11430-011-4203-4&link_type=DOI [45] Zhu, R. X., Fan, H. R., Li, J. W., et al., 2015. Destruction Gold Deposits. Science in China (Series D:Earth Sciences), 45(8):1153-1168 (in Chinese with English abstract). [46] Zhu, R.X., Xu, Y. G., Zhu, G., et al., 2012. Destruction of the North China Craton. Science in China (Series D:Earth Sciences), 42(8):1135-1159 (in Chinese). [47] 丁正江, 孙丰月, 刘建辉, 等, 2012.胶东刑家山钨钼矿床辉钼矿Re-Os同位素测年及其地质意义.岩石学报, 28(9):2721-2732. http://d.wanfangdata.com.cn/Periodical/ysxb98201201003 [48] 杜安道, 屈文俊, 李超, 等, 2009.铼-锇同位素定年方法及分析测试技术的进展.岩矿测试, 28(3):288-304 http://d.wanfangdata.com.cn/Periodical/ykcs200903019 [49] 郭祺, 2019.辽宁五龙金矿构造控矿规律及找矿预测(硕士学位论文).北京: 中国地质大学, 1-66. [50] 李杰, 宋明春, 王美云, 等, 2013.胶东尚家庄钼矿床Re-Os同位素年龄及其地质意义.中国地质, 40(5):1612-1621. http://www.cqvip.com/QK/90050X/20135/47604933.html [51] 李龙, 周学武, 1992.五龙金矿控矿构造研究及综合信息统计预测.地质与勘探, 28(10):31-37. http://www.cnki.com.cn/Article/CJFDTotal-DZKT199210006.htm [52] 刘善宝, 王登红, 陈毓川, 等, 2011.胶东半岛烟台地区刑家山钨钼矿床地质特征及其辉钼矿Re-Os同位素测年.地质通报, 30(8):1294-1302. http://d.wanfangdata.com.cn/Periodical/zgqydz201108016 [53] 吕贻峰, 李江风, 1993.丹东韧性剪切带变形特征及其在五龙金矿成矿过程中的意义.地球科学, 18(4):415-424. http://www.earth-science.net/article/id/54 [54] 吕贻峰, 李江风, 李龙, 等, 1994.辽东丹东五龙金矿矿化类型及其构造控制机理.现代地质, 8(3):309-316. http://www.cnki.com.cn/Article/CJFDTotal-XDDZ403.010.htm [55] 辽宁省地质矿产局, 1989.辽宁省区域地质志.北京:地质出版社, 1-856. [56] 屈文俊, 杜安道, 2003.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄.岩矿测试, 22(4):254-262. http://d.wanfangdata.com.cn/Periodical/ykcs200304003 [57] 王可勇, 万多, 刘正宏, 等, 2011.辽宁丹东四道沟金矿床构造控矿规律及其机制分析.吉利大学学报(地球科学版), 41(4):1048-1054. http://d.wanfangdata.com.cn/Periodical/cckjdxxb201104013 [58] 魏俊浩, 刘丛强, 赵永鑫, 等, 2001.辽宁五龙金矿主成矿阶段成矿持续时限.地质论评, 47(4):433-437. http://d.wanfangdata.com.cn/Periodical/OA000006655 [59] 肖国洪, 刘铁侠, 张国宪, 2003.辽宁五龙金矿床成因与成矿模式探讨.黄金, 24:17-21. http://www.cnki.com.cn/Article/CJFDTotal-HJZZ200311004.htm [60] 肖国洪, 张国宪, 2004.辽宁五龙金矿北西向断裂构造控矿浅析.黄金, 25:15-17. http://www.cqvip.com/QK/90449X/20049/10474201.html [61] 肖世椰, 2019.辽东五龙金矿区构造演化及金矿期岩脉就位机制(硕士学位论文).合肥: 合肥工业大学, 1-74. [62] 肖世椰, 朱光, 张帅, 等, 2018.辽东五龙金矿区成矿期构造过程与岩脉就位机制.科学通报, 63(28):3022-3036. http://www.cqvip.com/QK/94252X/201828/676541281.html [63] 杨春福, 1997.辽宁五龙金矿容矿断裂构造与金矿体空间赋存特征.黄金, 18(3):3-8. http://www.cqvip.com/Main/Detail.aspx?id=2452073 [64] 杨春福, 纪兆家, 张国宪, 等, 1997.五龙金矿脉岩对金矿体的制约机制.地质勘探, 33(6):7-11. http://www.cqvip.com/QK/93079X/19976/2868185.html [65] 杨凤超, 杨佳林, 顾玉超, 等, 2019.辽东五龙金矿围岩片麻状花岗岩的侵位和变形时代:SHRIMP U-Pb年代学制约.地质力学学报, 25(增刊1):44-48. http://www.cqvip.com/QK/98414X/2019A01/68907688504849578349484856.html [66] 杨进辉, 吴福元, 罗清华, 等, 2004.辽宁丹东地区侏罗纪花岗岩的变形时代:40Ar/39Ar年代学制约.岩石学报, 20(5):1205-1214. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200412002043.htm [67] 翟明国, 朱日祥, 刘建明, 等, 2003.华北东部中生代构造体制转换的关键时限.中国科学(D辑:地球科学), 33(10):913-920. [68] 战宝贵, 1994.五龙金矿地质特征及找矿规律.材料与冶金学报, 13:323-329. http://www.cnki.com.cn/Article/CJFDTotal-HUJI199404003.htm [69] 张军进, 丁正江, 刘殿浩, 等, 2016.山东莱州三山岛北部海域超大型金矿勘查实践与找矿成果.黄金科学与技术, 24(1):1-10. http://www.cnki.com.cn/Article/CJFDTotal-HJKJ201601001.htm [70] 张朋, 2018.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.(博士学位论文).长春:吉林大学, 1-229. http://cdmd.cnki.com.cn/Article/CDMD-10183-1018213504.htm [71] 张朋, 赵岩, 寇林林, 等, 2019.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.地球科学, 44(10):3297-3313. doi: 10.3799/dqkx.2019.129 [72] 赵越, 陈斌, 张栓宏, 等, 2010.华北克拉通北缘及邻区前燕山期主要地质事件.中国地质, 37(4):900-915. http://www.cqvip.com/Main/Detail.aspx?id=35237912 [73] 赵岩, 寇林林, 张朋, 等, 2019.辽东半岛隆昌地区~2 113 Ma变辉长岩地球化学与Hf同位素研究:对胶辽吉造山带构造演化的制约.地球科学, 44(10):3333-3345. doi: 10.3799/dqkx.2019.185 [74] 周文军, 李兴国, 齐增辉, 等, 2007.辽宁五龙金矿区花岗斑岩与成矿关系浅析.黄金, 10(28):16-19. http://www.cnki.com.cn/Article/CJFDTotal-HJZZ200710005.htm [75] 朱日祥, 陈凌, 吴福元, 等, 2011.华北克拉通破坏时间、范围与机制.中国科学(D辑:地球科学), 41(5):583-592. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201105001 [76] 朱日祥, 范宏瑞, 李建威, 等, 2015.克拉通破坏型金矿床.中国科学(D辑:地球科学), 45(8):1153-1168. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201508006 [77] 朱日祥, 徐义刚, 朱光, 等, 2012.华北克拉通破坏.中国科学(D辑:地球科学), 42(8):1135-1159. -
点击查看大图
图(12) / 表(1)
计量
- 文章访问数: 893
- HTML全文浏览量: 429
- PDF下载量: 53
- 被引次数: 0
