研究方向：

热液成矿系统的矿物表征

多尺度高光谱遥感矿产勘查

岩石破坏诱发物相和化学成分微细变化的光谱反映

个人简介：

杨凯教授从事高光谱技术研发和地质应用工作30多年，主持和参与了一系列政府和企业资金支持的科研项目(中国科技部、澳大利亚DIST、澳大利亚AMIRA等)。多年来深耕高光谱技术推广和生产应用领域，为矿业公司的矿床勘探和矿山采选业务提供技术服务，主导完成了约30个大洋洲和南北美洲大型矿山委托的技术服务项目。

教育背景：

1978.03-1982.01,长春地质学院，学士

1982.09-1985.10, 长春地质学院，硕士

1989.10-1993.10，University of Newcastle (澳大利亚), 博士

工作履历：

1985.10-1988.07，长春地质学院，讲师

1994.11-2013.10，澳大利亚联邦科学与工业研究组织，历任博士后、研究员和首席科学家，从事高光谱技术研发及其矿床勘探和采选矿应用，技术咨询服务。

2013.11-2019.09，中科遥感科技集团有限公司，总工程师

论文与专著：

[1]Zhou Y., Li L., Yang K., Xing G., Xiao W., Zhang H., Xiu L., Yao Z. & Xie Z. 2020. Hydrothermal alteration characteristics of the Chating Cu-Au deposit in Xuancheng City, Anhui Province, China: Significance of sericite alteration for Cu-Au exploration. Ore Geology Reviews 127, 103844.

[2]李建国, 金若时, 张博, 苗培森, 杨凯, 里宏亮, 魏佳林, 奥琮,曹民强, 张红亮, 朱强2018. 松辽盆地西南部上白垩统姚家组原生黏土矿物组合特征及其找铀意义. 地球学报39, 295-305.

[3]卢燕,杨凯,修连存2017.基于近红外光谱技术的烃类与粘土矿物识别及其地质意义[J].地质通报 ,36，1884-1891.

[4]Wells M., Ramanaidou E., Laukamp C., Yang K. & Pownceby M. 2017. Clays by deposit type, Chapter 5. In: Grafe M., Klauber C., McFarlane A. & Robinson D., editor/s. Clays in the Minerals Processing Value Chain. Cambridge University Press, p205-262.

[5]Yang K., Whitbourn L. Mason P & Huntington J. 2013. Mapping the chemical composition of nickel laterites with reflectance spectroscopy at Koniambo, New Caledonia. Economic Geology 108, 1285-1299.

[6]Yang K., Huntington J.F., Gemmell J.B. & Scott K.M. 2011. Variations in composition and abundance of white mica in the hydrothermal alteration system at Hellyer, Tasmania, as revealed by infrared reflectance spectroscopy. Journal of Geochemical Exploration, 108, 143-156.

[7]Roache T.J., Walshe J.L., Huntington J.F., Quigley M.A., Yang K., Bil B.W., Blake K.L. & Hyvärinen T. 2011. Epidote–clinozoisite as a hyperspectral tool in exploration for Archean gold. Australian Journal of Earth Sciences 58, 813–822.

[8]Thompson A., Scott K., Huntington J. & Yang K. 2009. Mapping mineralogy with reflectance spectroscopy: examples from volcanogenic massive sulfide deposits. Reviews in Economic Geology 16, 25-40.

[9]Cudahy T., Hewson R., Caccetta M., Roache A., Whitbourn L., Connor P., Coward D., Mason P., Yang K., Huntington J., & Quigley M. 2009. Drill core logging of plagioclase feldspar composition and other minerals associated with Archean gold mineralization at Kambalda, Western Australia, using a bidirectional thermal infrared reflectance system. Reviews in Economic Geology 16, 223-226.

[10]Xu X., Jiang N., Yang K., Zhang B., Liang G., Mao Q., Li J., Du S., Ma Y., Zhang Y. & Qin K. 2009. Accumulated phenocrysts and origin of feldspar porphyry in the Chanho area, western Yunnan, China. Lithos 113, 595–611.

[11]McConachy T, Yang K., Boni M, & Evans N. 2007. Spectral reflectance characteristics of non sulphide lead and zinc minerals and a novel application of U-Th/He thermochronometry using the zinc phosphate mineral tarbuttite to constrain the age of mineralization at Skorpion, Namibia. Geochemistry: Exploration, Environment, Analysis 7, 135-151.

[12]甘甫平, 张宗贵, 王润生, 杨凯, 刘圣伟, 闫柏琨. 2005. 光谱重建与光谱真实性检验中地物光谱的作用. 国土资源遥感 63 (No. 1).

[13]Yang K., Lian C., Huntington J., Peng Q. & Wang Q. 2005. Infrared Reflectance Spectral Characterization of the Hydrothermal Alteration at the Tuwu Cu-Au Deposit, Xinjiang, China. Mineralium Deposita 40, 324 – 336.

[14]Sun Y., Seccombe P.K. & Yang K. 2001. Application of short-wave infrared spectroscopy to define alteration zones associated with the Elura zinc-lead-silver deposit, NSW Australia. Journal of Geochemical Exploration 73, 11-26.

[15]Yang K., Browne P.R.L., Huntington J.F. & Walshe J.L. 2001. Characterising the hydrothermal alteration of the Broadlands-Ohaaki geothermal system, New Zealand, using short-wave infrared spectroscopy. Journal of Volcanology and Geothermal Research 106, 53-65.

[16]Yang K., Huntington J.F., Browne P.R.L. & Ma C. 2000. An infrared spectral reflectance study of hydrothermal alteration minerals from the Te Mihi sector of the Wairakei geothermal system, New Zealand. Geothermics 29, 377-392.

[17]Yang K., Huntington J.F. & Boardman J.W. 2000. Mapping hydrothermal alteration in the Comstock mining district, Nevada, using simulated satellite-borne hyperspectral data. Australian Journal of Earth Sciences 46, 915-922.

[18]Yang K. & Seccombe P.K. 1997. Geochemistry of the mafic-ultramafic complexes from the northern Great Serpentinite Belt, NSW: implications for first stage melting. In: Ashley P.M. & Flood P.G. (eds), Tectonics and Metallogenesis of the New England Orogen, Geological Society of Australia Special Publication 19, p.197-211.

[19]Yang K., Thalhammer O.A.R. & Seccombe P.K. 1995. Distribution of platinum-group elements in the Great Serpentinite Belt of New South Wales. Mineralogy and Petrology 54, 191-211.

[20]Yang K. & Seccombe P.K. 1994. Contrasting hydrothermal behaviour between IPGE and PPGE, as exemplified by platinum group minerals in the Great Serpentinite Belt, eastern Australia. Transactions of the Institution of Mining and Metallurgy 103B, 39-44.

[21]Yang K. & Seccombe P.K. 1993. Chemical variations of chromite in the ultramafic cumulates of the Great Serpentinite Belt, New South Wales, Australia. Canadian Mineralogist 31, 75-87.

[22]Yang K. & Seccombe P.K. 1993. Platinum-group minerals in the chromitites from the Great Serpentinite Belt, NSW, Australia. Mineralogy and Petrology 47, 263-286.

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