Volume 45 Issue 11
Nov.  2020
Turn off MathJax
Article Contents
Article Navigation >  Earth Science  > 2020  >  45(11): 3998-4013
Liu Xiangchong, Xiao Changhao, Zhang Shuanhong, Hu Guohui, Li Jianfeng, Wang Chenguang, 2020. Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?. Earth Science, 45(11): 3998-4013. doi: 10.3799/dqkx.2020.292
Citation: Liu Xiangchong, Xiao Changhao, Zhang Shuanhong, Hu Guohui, Li Jianfeng, Wang Chenguang, 2020. Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?. Earth Science, 45(11): 3998-4013. doi: 10.3799/dqkx.2020.292
shu

Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?

doi: 10.3799/dqkx.2020.292
  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, CAGS, Beijing 100081, China

  • 3.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China

  • 4.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • Received Date: 2020-05-18
  • Publish Date: 2020-11-15
    Abstract
  • The Wulong gold deposit located in Liaoning Province is a typical vein-type gold deposit in the eastern part of the North China craton,but how this large-scale gold deposit formed remains controversial. This deposit was interpreted to be genetically related to the Sanguliu granite because they are spatially close and have close chronological ages and the mineralizing fluids have a magmatic-hydrothermal origin. There is no sufficient evidence supporting that the Sanguliu granite provided the gold-bearing magmatic-hydrothermal fluids required for forming the Wulong deposit,so did the former provide sufficient energy for the latter? In order to answer this question,numerical modeling of heat-driven convection of meteoric water and magmatic-hydrothermal fluids released by the Sanguliu granite was built based on its geochemical and geophysical characteristics to simulate the evolution of fluid flow and temperature after emplacement of the granite. Numerical results indicate that the temperatures within 1 km of the Sanguliu granite were elevated to over 300℃ for hundreds of thousands of years. This long high temperature filed favors formation of magmatic-hydrothermal deposits. In contrast,the position of the Wulong deposit received insignificant energy from the Sanguliu granite. If magmatic-hydrothermal fluids were released from the Sanguliu granite,those magmatic-hydrothermal fluids should have caused alteration and minerlization at the granite margin and the contact between the granite and its wallrock. However,these phenomena have not been identified in the field. Therefore,there is probably no genetic relationship between the large-scale Wulong deposit and the Sanguliu granite,and further investigations are needed to identify the source for Au-mineralizing fluids.

     

    • FullText(HTML)
  • loading
    • References(95)
  • Bao, Z.Y., 1992. Onset and Stability of Thermally-Driven Fluid Convection in a Vertical Rock Crack and Their Implication for Hydrothermal Ore-Forming Processes. Earth Science, 17(Suppl.1):57-67 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-ZDDY199200006.htm
    Buret, Y., von Quadt, A., Heinrich, C., et al., 2016. From a Long-Lived Upper-Crustal Magma Chamber to Rapid Porphyry Copper Emplacement:Reading the Geochemistry of Zircon Crystals at Bajo de La Alumbrera (NW Argentina). Earth and Planetary Science Letters, 450:120-131. https://doi.org/10.1016/j.epsl.2016.06.017
    Burnham, C. W., 1985. Energy Release in Subvolcanic Environments; Implications for Breccia Formation. Economic Geology, 80(6):1515-1522. https://doi.org/10.2113/gsecongeo.80.6.1515
    Burnham, C.W., 1997. Magmas and Hydrothermal Fluids. In: Barnes, H.L., ed., Geochemistry of Hydrothermal Ore Deposits (3rd Edition). John Wiley & Sons, New York, 63-123.
    Candela, P. A., Blevin, P. L., 1995. Do Some Miarolitic Granites Preserve Evidence of Magmatic Volatile Phase Permeability. Economic Geology, 90(8):2310-2316. https://doi.org/10.2113/gsecongeo.90.8.2310
    Cathles, L. M., 1977. An Analysis of the Cooling of Intrusives by Ground-Water Convection Which Includes Boiling. Economic Geology, 72(5):804-826. https://doi.org/10.2113/gsecongeo.72.5.804
    Cen, K., Tian, Z.X., 2012. Ore-Forming System around Magma:Model of Spatial Zonation for Magmatic Rock and Deposit Set. Geoscience, 26(5):1051-1057 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ201205027.htm
    Chi, G.X., Xue, C.J., 2011. An Overview of Hydrodynamic Studies of Mineralization. Geoscience Frontiers, 2(3):423-438. doi: 10.1016/j.gsf.2011.05.001
    Cui, B., Li, Z., 1998. Synthetic Metallogenic Prediction in the Material Field-Energy Field-Spatial Field. Geoscience, 12(4):501-505 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ804.006.htm
    Dutrow, B. L., Travis, B. J., Gable, C. W., et al., 2001. Coupled Heat and Silica Transport Associated with Dike Intrusion into Sedimentary Rock:Effects on Isotherm Location and Permeability Evolution. Geochimica et Cosmochimica Acta, 65(21):3749-3767. https://doi.org/10.1016/s0016-7037(01)00704-9
    Eldursi, K., Branquet, Y., Guillou-Frottier, L., et al., 2009. Numerical Investigation of Transient Hydrothermal Processes around Intrusions:Heat-Transfer and Fluid-Circulation Controlled Mineralization Patterns. Earth and Planetary Science Letters, 288(1/2):70-83. https://doi.org/10.1016/j.epsl.2009.09.009
    Gerdes, M. L., Baumgartner, L. P., Person, M., 1998. Convective Fluid Flow through Heterogeneous Country Rocks during Contact Metamorphism. Journal of Geophysical Research:Solid Earth, 103(B10):23983-24003. https://doi.org/10.1029/98jb02049
    Ghiorso, M.S., 1991. Temperatures in and around Cooling Magma Bodies. In: Perchuk, L.L., ed., Progress in Metamorphic and Magmatic Petrology. Cambridge University Press, New York, 387-410.
    Gu, Y.C., 2019. The Mesozoic Tectonic-Magmatic Constraints on the Gold Mineralization in Wulong Gold Mining Area, Eastern Liaoning (Dissertation). China University of Geosciences, Beijing, 156 (in Chinese with English abstract).
    Hanson, R.B., 1995. The Hydrodynamics of Contact Metamorphism. Geological Society of America Bulletin, 107(5):595-611. doi: 10.1130/0016-7606(1995)107<0595:THOCM>2.3.CO;2
    Hu, G.H., Zhang, Q.Q., Li, J.F., et al., 2020. Emplacement Ages of Mesozoic Granites in the Liaodong Area:Constraints from Zircon and Monazite U-Pb Dating. Earth Science, 45(11):3962-3981 (in Chinese with English abstract).
    Ingebritsen, S. E., Geiger, S., Hurwitz, S., et al., 2010. Numerical Simulation of Magmatic Hydrothermal Systems. Reviews of Geophysics, 48(1):1-33. https://doi.org/10.1029/2009rg000287
    Lange, R. A., Cashman, K. V., Navrotsky, A., 1994. Direct Measurements of Latent Heat during Crystallization and Melting of a Ugandite and an Olivine Basalt. Contributions to Mineralogy and Petrology, 118(2):169-181. https://doi.org/10.1007/bf01052867
    Li, S.Z., Liu, J.Z., Zhao, G.C., et al., 2004. Key Geochronology of Mesozoic Deformation in the Eastern Block of the North China Craton and Its Constraints on Regional Tectonics:A Case of Jiaodong and Liaodong Peninsula. Acta Petrologica Sinica, 20(3):633-646 (in Chinese with English abstract). http://www.researchgate.net/publication/232696982_Key_geochronology_of_Mesozoic_deformation_in_the_Eastern_Block_of_the_North_China_Craton_and_its_constrains_on_regional_tectonics-a_case_of_Jiaodong_and_Liaodong_Peninsula
    Li, Y., Selby, D., Condon, D., et al., 2017. Cyclic Magmatic-Hydrothermal Evolution in Porphyry Systems:High-Precision U-Pb and Re-Os Geochronology Constraints on the Tibetan Qulong Porphyry Cu-Mo Deposit. Economic Geology, 112(6):1419-1440. https://doi.org/10.5382/econgeo.2017.4515
    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. https://doi.org/10.1016/j.oregeorev.2019.04.013
    Liu, Y. D., 1987. Discussion on the Geological Characteristics and Genesis of Granite in Sanguliu of Liaoning. Liaoning Geology, 3:245-260 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LOAD198703005.htm
    Lv, Y.F., Li, J.F., Zhang, M., 1993. The Structural Character of Syntectonic Granite Body with Forceful Emplacement and Its Relationship with the Gold Deposit:The Example of Sanguliu Granite Body, Dandong. Land & Resources, 1(2):120-128 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LOAD199302001.htm
    Ma, C.Q., Li, Y.Q., 2017. Incremental Growth of Granitoid Plutons and Highly Crystalline Magmatic Differentiation. Acta Petrologica Sinica, 33(5):1479-1488 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201705007.htm
    Ma, Y.M., Lu, X.C., Zhang, X.F., et al., 2013. A Numerical Simulation of the Heat Transfer in Granite Intrusion-Mudstone Contact Zone and Its Geological Implication:A Case Study from Eastern Guangdong Province, China. Geological Journal of China Universities, 19(2):307-315 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX201302013.htm
    Nabelek, P. I., Hofmeister, A. M., Whittington, A. G., 2012. The Influence of Temperature-Dependent Thermal Diffusivity on the Conductive Cooling Rates of Plutons and Temperature-Time Paths in Contact Aureoles. Earth and Planetary Science Letters, 317/318:157-164. https://doi.org/10.1016/j.epsl.2011.11.009
    Ni, P., Wang, X. D., Wang, G. G., et al., 2015. An Infrared Microthermometric Study of Fluid Inclusions in Coexisting Quartz and Wolframite from Late Mesozoic Tungsten Deposits in the Gannan Metallogenic Belt, South China. Ore Geology Reviews, 65(4):1062-1077. http://www.sciencedirect.com/science/article/pii/S0169136814001954
    Norton, D., Knight, J. E., 1977. Transport Phenomena in Hydrothermal Systems; Cooling Plutons. American Journal of Science, 277(8):937-981. https://doi.org/10.2475/ajs.277.8.937
    Ren, Q.J., Guo, G.Z., Feng, Z.J., et al., 1994. Computer Simulation of Heat and Fluid Transport in the Ore-Forming Process of the Jinduicheng Porphyry Molybdenum Deposit, Shaanxi Province. Mineral Deposits, 13(1):88-959 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ401.008.htm
    Schön, J.H., 2015. Physical Properties of Rocks: Fundamentals and Principles of Petrophysics. Elsevier, Amsterdam, 378-380. https://doi.org/ 10.1016/c2014-0-03002-x
    Sillitoe, R. H., 2010. Porphyry Copper Systems. Economic Geology, 105(1):3-41. https://doi.org/10.2113/gsecongeo.105.1.3
    Spencer, E. T., Wilkinson, J. J., Creaser, R. A., et al., 2015. The Distribution and Timing of Molybdenite Mineralization at the El Teniente Cu-Mo Porphyry Deposit, Chile. Economic Geology, 110(2):387-421. https://doi.org/10.2113/econgeo.110.2.387
    Vosteen, H. D., Schellschmidt, R., 2003. Influence of Temperature on Thermal Conductivity, Thermal Capacity and Thermal Diffusivity for Different Types of Rock. Physics and Chemistry of the Earth, Parts A/B/C, 28(9/10/11):499-509. https://doi.org/10.1016/s1474-7065(03)00069-x
    Wagner, W., Pruss, A., 2002. The IAPWS Formulation 1995 for the Thermodynamic Properties of Ordinary Water Substance for General and Scientific Use. Journal of Physical and Chemical Reference Data, 31(2):387-535. https://doi.org/10.1063/1.1461829
    Wang, D.L., Shen, J.F., Qiu, H.C., et al., 2019. Study on Typomorphic Characteristics of Pyrite and Prediction of Deep Prospecting of Wulong Gold Deposit in Liaoning Province. Journal of Nanjing University (Natural Science), 55(6):898-915 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-NJDZ201906003.htm
    Wang, D. Y., 2013. Magma Heat NS1D:One-Dimensional Visualization Numerical Simulator for Computing Thermal Evolution in a Contact Metamorphic Aureole. Computers & Geosciences, 54:21-27. https://doi.org/10.1016/j.cageo.2013.01.006
    Wang, K.Y., Qing, M., Bian, H.Y., et al., 2010. The Geological Features and Geochemistry of Ore-Forming Fluids of Wulong Gold Deposit in Liaoning Province. Journal of Jilin University (Earth Science Edition), 40(3):557-564 (in Chinese with English abstract).
    Wang, Y. Z., Wang, F., Wu, L., et al., 2018. (U-Th)/He Thermochronology of Metallic Ore Deposits in the Liaodong Peninsula:Implications for Orefield Evolution in Northeast China. Ore Geology Reviews, 92:348-365. https://doi.org/10.1016/j.oregeorev.2017.11.025
    Wei, J.H., Liu, C.Q., Tang, H.F., 2003. Metallogeny of Gold Deposits and Evidence of Isotopes and Trace Elements for the Comagmatic Evolution of the Yanshanian Intrusive Rocks in the Wulong Area, Eastern Liaoning. Geological Review, 49(3):265-271 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200303007.htm
    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(4):433-437 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200104020.htm
    Weis, P., Driesner, T., Heinrich, C. A., 2012. Porphyry-Copper Ore Shells Form at Stable Pressure-Temperature Fronts within Dynamic Fluid Plumes. Science, 338(6114):1613-1616. https://doi.org/10.1126/science.1225009
    Wu, F., Lin, J., Wilde, S., et al., 2005a. Nature and Significance of the Early Cretaceous Giant Igneous Event in Eastern China. Earth and Planetary Science Letters, 233(1/2):103-119. https://doi.org/10.1016/j.epsl.2005.02.019
    Wu, F. Y., Yang, J. H., Wilde, S. A., et al., 2005b. Geochronology, Petrogenesis and Tectonic Implications of Jurassic Granites in the Liaodong Peninsula, NE China. Chemical Geology, 221(1/2):127-156. https://doi.org/10.1016/j.chemgeo.2005.04.010
    Xiao, C.H., Liu, X.C., Zhao, Y., et al., 2020. Structural Controls and Re-Os Dating of Molybdenite of the Wulong Gold Deposit, NE China. Earth Science, 45(11):3982-3997 (in Chinese with English abstract).
    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
    Xing, H. L., 2014. Finite Element Simulation of Transient Geothermal Flow in Extremely Heterogeneous Fractured Porous Media. Journal of Geochemical Exploration, 144:168-178. https://doi.org/10.1016/j.gexplo.2014.03.002
    Yang, C.F., 1997. The Characteristics of the Ore Bearing Fracture Tectonics and the Gold Orebody's Spatial Occurrence of Wulong Gold Deposit. Gold, 18(3):3-8 (in Chinese with English abstract).
    Yang, F.C., Song, Y.H., Yang, J.L., et al., 2018. SHRIMP U-Pb Age and Geochemical Characteristics of Granites in Wulong-Sidaogou Gold Deposit, East Liaoning. Geotectonica et Metallogenia, 42(5):940-954 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DGYK201805013.htm
    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
    Yang, J., Large, R. R., Bull, S., et al., 2006. Basin-Scale Numerical Modeling to Test the Role of Buoyancy-Driven Fluid Flow and Heat Transfer in the Formation of Stratiform Zn-Pb-Ag Deposits in the Northern Mount Isa Basin. Economic Geology, 101(6):1275-1292. https://doi.org/10.2113/gsecongeo.101.6.1275
    Yang, J.H., Wu, F.Y., Luo, Q.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
    Yang, R.Y., Ma, D.S., Pan, J.Y., 2005. Effect of Annual Precipitation to Geotherm of Ore-Forming Fluid:A Case of Antimony Deposits in Xikuangshan. Earth Science, 30(3):366-370 (in Chinese with English abstract). http://www.researchgate.net/publication/289039033_Effect_of_annual_precipitation_to_geotherm_of_ore-forming_fluid_A_case_of_antimony_deposits_in_Xikuangshan
    Yang, S.S., Wang, K.Y., Hao, T.S., et al., 2010. Characteristics of Fluid Inclusions and Genesis of Sidaogou Gold Deposit in Dandong Area, Liaoning Province. Journal of Jilin University (Earth Science Edition), 40(4):773-780 (in Chinese with English abstract). http://www.researchgate.net/publication/290308650_Characteristics_of_fluid_inclusions_and_genesis_of_Sidaogou_gold_deposit_in_Dandong_Area_Liaoning_Province?ev=auth_pub
    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. https://doi.org/10.1016/j.oregeorev.2018.09.016
    Yu, C.W., Cen, K., Bao, Z. Y., et al., 1997. Dynamics of Ore-Forming Processes. Geological Publishing House, Beijing, 224 (in Chinese).
    Zeng, Q.D., Chen, R.Y., Yang, J.H., et al., 2019. The Metallogenic Characteristics and Exploring Ore Potential of the Gold Deposits in Eastern Liaoning Province. Acta Petrologica Sinica, 35(7):1939-1963 (in Chinese with English Abstract). doi: 10.18654/1000-0569/2019.07.01
    Zhang, D.H., Jin, X.D., Mao, S.D., et al., 2011. The Classification of Ore-Forming Fluid and the Efficiency of Ore Formation of Magmatic Hydrothermal Solution. Earth Science Frontiers, 18(5):90-102 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201105009.htm
    Zhang, D.H., Yu, C.W., Bao, Z.Y., et al., 1998. Fluid Dynamics and Numerical Simulation of Ore Zoning of Yinshan Polymetallic Deposit in Dexing, Jiangxi Province. Earth Science, 23(3):267-271 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX803.010.htm
    Zhang, P., Kou, L. L., Zhao, Y., et al., 2020. Genesis of the Wulong Gold Deposit, Liaoning Province, NE China:Constrains from Noble Gases, Radiogenic and Stable Isotope Studies. Geoscience Frontiers, 11(2):547-563. https://doi.org/10.1016/j.gsf.2019.05.012
    Zhang, Q., Jin, W.J., Li, C.D., et al., 2014. Magma-Thermal Field:Its Basic Characteristics, and Differences with Geothermal Field. Acta Petrologica Sinica, 30(2):341-349 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201402003.htm
    Zhang, Q., Jin, W.J., Wang, J.R., et al., 2016. Relationship between Magma-Thermal Field and Hydrocarbon Accumulation. Progress in Geophysics, 31(4): 1525-1541 (in Chinese with English abstract). doi: 10.1016/j.oregeorev.2019.103138
    Zhang, Z. Q., Wang, G. W., Carranza, E. J. M., et al., 2019. Metallogenic Model of the Wulong Gold District, China, and Associated Assessment of Exploration Criteria Based on Multi-Scale Geoscience Datasets. Ore Geology Reviews, 114:103138. https://doi.org/10.1016/j.oregeorev.2019.103138
    Zhao, C., Hobbs, B.E., Ord, A., 2008. Convective and Advective Heat Transfer in Geological Systems. Springer, Berlin, 229.
    Zhao, C. B., Reid, L. B., Regenauer-Lieb, K., 2012. Some Fundamental Issues in Computational Hydrodynamics of Mineralization:A Review. Journal of Geochemical Exploration, 112:21-34. https://doi.org/10.1016/j.gexplo.2011.10.005
    Zhu, R.X., Fan, H.R., Li, J.W., et al., 2015. Decratonic Gold Deposits. Scientia Sinica (Terrae), 45(8):1153-1168 (in Chinese). doi: 10.1360/zd2015-45-8-1153
    鲍征宇, 1992.垂直裂隙中热驱动流体对流的发生和稳定性及其热液成矿作用意义.地球科学, 17(S1):57-67. http://www.cnki.com.cn/Article/CJFDTotal-DQKX1992S1009.htm
    岑况, 田兆雪, 2012.岩浆中心成矿系:岩浆岩体和矿床组合的空间分带理想模式.现代地质, 26(5):1051-1057. http://d.wanfangdata.com.cn/Periodical/xddz201205026
    崔彬, 李忠, 1998.物质场-能量场-空间场综合成矿预测.现代地质, 12(4):501-505.
    顾玉超, 2019.辽东五龙金矿区中生代构造-岩浆作用对金成矿制约(博士学位论文).北京: 中国地质大学, 156.
    胡国辉, 张琪琪, 李建锋, 等, 2020.辽东地区中生代花岗岩的侵位时代:锆石和独居石U-Pb年代学.地球科学, 45(11):3962-3981. doi: 10.3799/dqkx.2020.293
    李三忠, 刘建忠, 赵国春, 等, 2004.华北克拉通东部地块中生代变形的关键时限及其对构造的制约:以胶辽地区为例.岩石学报, 20(3):633-646. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200403027.htm
    刘义德, 1987.辽宁省三股流花岗岩地质特征及成因探讨.辽宁地质, 3:245-260. http://www.cnki.com.cn/Article/CJFDTotal-LOAD198703005.htm
    吕贻峰, 李江风, 张鸣, 1993.强力侵位花岗岩体与金矿的关系:以丹东三股流岩体为例.国土资源, 1(2):120-128.
    马昌前, 李艳青, 2017.花岗岩体的累积生长与高结晶度岩浆的分异.岩石学报, 33(5):1479-1488. http://d.wanfangdata.com.cn/Periodical/ysxb98201705007
    马野牧, 陆现彩, 张雪芬, 等, 2013.花岗岩侵入体-泥质围岩热传输过程的数值模拟及其地质意义:以粤东典型接触带剖面为例.高校地质学报, 19(2):307-315. http://www.cnki.com.cn/Article/CJFDTotal-GXDX201302013.htm
    任启江, 郭国章, 冯祖钧, 等, 1994.陕西金堆城斑岩钼矿成矿过程中热及流体传输的计算模拟.矿床地质, 13(1):88-95. http://www.cqvip.com/Main/Detail.aspx?id=1418808
    王冬丽, 申俊峰, 邱海成, 等, 2019.辽宁五龙金矿黄铁矿标型特征研究及深部找矿预测.南京大学学报(自然科学版), 55(6):898-915. http://www.cqvip.com/QK/95251X/20196/7100287129.html
    王可勇, 卿敏, 边红业, 等, 2010.辽宁五龙金矿床地质特征及成矿流体地球化学性质.吉林大学学报(地球科学版), 40(3):557-564. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201003012.htm
    魏俊浩, 刘丛强, 唐红峰, 2003.辽东五龙地区燕山期侵入岩类同源岩浆演化微量元素、同位素证据与金矿成矿.地质论评, 49(3):265-271. http://www.cnki.com.cn/Article/CJFDTotal-DZLP200303007.htm
    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.
    肖昌浩, 刘向冲, 赵岩, 等, 2020.辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄, 地球科学, 45(11):3982-3997. doi: 10.3799/dqkx.2020.217
    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
    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
    杨凤超, 宋运红, 杨佳林, 等, 2018.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.大地构造与成矿学, 42(5):940-954. http://d.old.wanfangdata.com.cn/Periodical_ddgzyckx201805013.aspx
    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(S1):44-48. http://www.cqvip.com/QK/98414X/2019A01/68907688504849578349484856.html
    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
    杨瑞琰, 马东升, 潘家永, 2005.大气降水量对成矿流体热场的影响:以锡矿山锑矿床成矿流体为例.地球科学, 30(3):366-370. http://www.earth-science.net/article/id/1419
    杨帅师, 王可勇, 郝通顺, 等, 2010.辽宁丹东四道沟金矿床流体包裹体特征及矿床成因.吉林大学学报(地球科学版), 40(4):773-780.
    於崇文, 岑况, 鲍征宇, 等, 1998.成矿作用动力学.北京:地质出版社, 224.
    曾庆栋, 陈仁义, 杨进辉, 等, 2019.辽东地区金矿床类型、成矿特征及找矿潜力.岩石学报, 35(7):1939-1963. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201907001.htm
    张德会, 金旭东, 毛世德, 等, 2011.成矿热液分类兼论岩浆热液的成矿效率.地学前缘, 18(5):90-102.
    张德会, 於崇文, 鲍征宇, 等, 1998.银山多金属矿床成矿分带的流体动力学计算模拟.地球科学, 23(3):267-271. http://www.earth-science.net/article/id/648
    张旗, 金惟俊, 李承东, 等, 2014.岩浆热场:它的基本特征及其与地热场的区别.岩石学报, 30(2):341-349. http://d.wanfangdata.com.cn/Periodical/ysxb98201402003
    张旗, 金维浚, 王金荣, 等, 2016.岩浆热场对油气成藏的影响.地球物理学进展, 31(4):1525-1541.
    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
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    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(13)

    Get Citation
    PDF
    XML
    Article views (551) PDF downloads(40) Cited by()
    Proportional views

    Address：湖北省武汉市洪山区鲁磨路388号《地球科学》编辑部 China Pos：430074

    Tel：027-67885075 Fax：027-67885075

    Copyright ©2020 鄂ICP备15021562号-2

    Supported by: Beijing Renhe Information Technology Co. Ltd  support: info@rhhz.net

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return