姓名： 于宋月                        性别： 男

出生年月：1979年6月         学历学位：博士

职称：研究员                         专业：岩石地球化学

Tel：0851-85895538

E-mail：yusongyue@mail.gyig.ac.cn

主要研究方向:

1．峨眉山大火成岩省基性-超基性岩浆作用及成矿

2．中国东部玄武岩及幔源包体

学习及工作经历：

学历

1999.09－2003.06 吉林大学地球科学学院，固体资源勘查专业，获学士学位

2003.09－2008.06 中国科学院广州地球化学研究所，岩石地球化学，硕博连读，获博士学位

工作经历

2008.06－2011.12 中国科学院地球化学研究所，助理研究员

2012.01－2017.12 中国科学院地球化学研究所，副研究员、硕士生导师

2018.01－现在 中国科学院地球化学研究所，研究员、博士生导师

2016.08－2017.08 美国印第安纳大学地质系，访问学者

承担科研项目情况：

作为负责人的主要科研项目：

1．国家自然科学基金面上项目，苦橄岩斑晶矿物的O-Li同位素研究：峨眉山大火成岩省岩浆地幔源区的制约

2．国家自然科学基金面上项目，云南牟定地区基性-超基性岩体的成因及对峨眉山地幔柱晚期基性岩浆活动的约束

3．国家自然科学基金青年项目，吉林蛟河幔源含石榴石辉石岩包体的地球化学研究

4．中国科学院“西部青年学者”项目，橄榄石斑晶O-Li同位素研究：对峨眉山大火成岩省及俄罗斯Pechenga苦橄岩地幔源区性质的制约

5．中国科学院“西部之光”博士项目，云南元谋地区两种不同类型矿床成因研究—以朱布和安益岩体为例

6．贵州省科学技术基金，贵州水城-威宁地区二叠纪玄武岩PGE和Re-Os同位素研究

作为主要参加者的科研项目：

1．中科院B类先导专项子课题“地幔柱岩浆分异与成矿多样性”

2．国家973 项目“我国富铁矿形成机制与预测研究”中的子课题“岩浆型大型铁矿成矿过程和控矿因素”

3.国家重点研发计划子课题“地幔柱形成演化的深部地质过程与多因耦合-自组织临界转换”

代表论著：

第一作者及通讯作者文章：

[1] Yu, S.Y., Xu, Y.G., Zhou, S.H., Lan, J.B., Chen, L.M., Shen, N.P., Zhao, J.X., Feng, Y.X., 2018. Late Cenozoic basaltic lavas from the Changbaishan-Baoqing Volcanic Belt, NE China: Products of lithosphere-asthenosphere interaction induced by subduction of the Pacific plate. Journal of Asian Earth Sciences, 164: 260-273.

[2] Zhou, S.H., Yu, S.Y*., Zhou, T., Lan, J.B., Kang, J., Chen, L.M., Hu, J.H., 2018. Lithium elemental and isotopic disequilibrium in minerals from peridotite xenoliths from Shangzhi, NE China: products of recent melt/fluid-peridotite interaction. Acta Geochimica.37(5): 769-789.

[3] Yu, S.Y., Shen, N.P., Song, X.Y., Ripley, E.M., Li, C. and Chen, L.M., 2017. An integrated chemical and oxygen isotopic study of primitive olivine grains in picrites from the Emeishan Large Igneous Province, SW China: Evidence for oxygen isotope heterogeneity in mantle sources. Geochimica et Cosmochimica Acta, 215: 263-276.

[4] Yu S.Y., Song X.Y., Ripley, E.M., Chusi Li, Chen L.M., She Y.W., Luan Y. 2015. Integrated O–Sr–Nd isotope constraints on the evolution of four important Fe–Ti oxide ore-bearing mafic–ultramafic intrusions in the Emeishan large igneous province, SW China. Chemical Geology 401: 28-42.

[5] Yu, S.Y., Song, X.Y., Chen, L.M., Li, X.B. 2014. Postdated melting of subcontinental lithospheric mantle by the Emeishan mantle plume: Evidence from the Anyi intrusion, Yunnan,SW China. Ore geology reviews, 2014, 57: 560-573.

[6] Yu, S.Y., Song, X.Y. Xu, Y.G., Chen, L.M., Li, J. 2012. Effects of melt percolation on the Re-Os systematics of continental mantle lithosphere: A case study of spinel peridotite xenoliths from Heilongjiang, NE China. Science in China Series D 55：869-1042.

[7] Yu, S.Y., Xu, Y.G, Ma, J.L., Zheng Y.F., Kuang, Y.S., Hong, L.B., Ge, W.C., Tong, L.X. 2010. Remnants of oceanic lower crust in the subcontinental lithospheric mantle: Trace element and Sr-Nd-O isotope evidence from aluminous garnet pyroxenite xenoliths from Jiaohe, Northeast China. Earth and Planetary Science Letters 297(3-4): 413-422.

[8] Yu, S.Y., Xu, YG, Huang, X.L., Ma, J.L., Ge, W.C., Zhang, H.H., Qin, X.F. 2009. Hf-Nd isotopic decoupling in continental mantle lithosphere beneath Northeast China: Effects of pervasive mantle metasomatism. Journal of Asian Earth Sciences 35: 554-570.

[9] 于宋月，徐义刚，黄小龙，葛文春，程锦. 2007. 东北和华北地区上地幔成分和热状态对比及对中国东部岩石圈减薄的启示. 岩石学报 23（6）：1252-1268.

[10] 于宋月，徐义刚，黄小龙，葛文春，马金龙. 2007.吉林双辽地区橄榄岩包体中熔体-岩石作用特征及其对地幔交代作用的启示. 岩石矿物学杂志 26（3）：213-222.

[11] 于宋月; 宋谢炎; E.M.Ripley; Chusi Li; 陈列锰; 佘宇伟; 栾燕, 2015. O-Sr-Nd同位素对峨眉山大火成岩省中含钒钛磁铁矿岩体成因的制约, 矿物学报, S1：177.

共同作者文章：

[1] Yao, J.-H., Zhu, W.-G., Li, C., Zhong, H., Yu, S.-Y, Ripley, E.M. and Bai, Z.-J., 2019. Olivine O isotope and trace element constraints on source variation of picrites in the Emeishan flood basalt province, SW China. Lithos, 338-339: 87-98.

[2] He, H.-L., Song, X.-Y., Zhai, M.-G., Yu, S.-Y. and Du, Z.-S., 2019. Lower crustal contribution to the magma formation of the Damiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes. Precambrian Research, 332: 105396.

[3] Hu, J.-H., Song, X.-Y., He, H.-L., Zheng, W.-Q., Yu, S.-Y., Chen, L.-M. and Lai, C.-K., 2018. Constraints of texture and composition of clinopyroxene phenocrysts of Holocene volcanic rocks on a magmatic plumbing system beneath Tengchong, SW China. Journal of Asian Earth Sciences, 154: 342-353.

[4] Chen, L.M., Teng, F.Z., Song, X.Y., Hu, R.Z., Yu, S.Y., Zhu, D. and Kang, J., 2018. Magnesium isotopic evidence for chemical disequilibrium among cumulus minerals in layered mafic intrusion. Earth and Planetary Science Letters, 487: 74-83.

[5] Chen, L.-M., Song, X.-Y., Hu, R.-Z., Yu, S.-Y., He, H.-L., Dai, Z.-H., She, Y.-W. and Xie, W., 2017. Controls on trace-element partitioning among co-crystallizing minerals: Evidence from the Panzhihua layered intrusion, SW China. American Mineralogist, 102(5): 1006-1020.

[6] She, Y.-W., Song, X.-Y., Chen, L.-M., Yu, S.-Y., Zhu, X.-K., Yi, J.-N. and Hu, J.-H., 2017. Platinum-group element geochemistry of the layered intrusions in the Emeishan large igneous province, SW China: Implications for the principal controls on magmatic sulfide immiscibility. American Journal of Science, 317(4): 483-513.

[7] He, H.L., Yu, S.Y., Song, X.Y., Du, Z.S., Dai, Z.H., Zhou, T. and Xie, W., 2016. Origin of nelsonite and Fe–Ti oxides ore of the Damiao anorthosite complex, NE China: Evidence from trace element geochemistry of apatite, plagioclase, magnetite and ilmenite. Ore Geology Reviews, 79: 367-381.

[8] She, Y.W., Song, X.Y., Yu, S.Y., Chen, L.M. and Zheng, W.-Q., 2016. Apatite geochemistry of the Taihe layered intrusion, SW China: Implications for the magmatic differentiation and the origin of apatite-rich Fe-Ti oxide ores. Ore Geology Reviews, 78: 151-165.

[9] Arguin, J.-P., Pagé, P., Barnes, S.-J., Yu, S.-Y. and Song, X.-Y., 2016. The Effect of Chromite Crystallization on the Distribution of Osmium, Iridium, Ruthenium and Rhodium in Picritic Magmas: an Example from the Emeishan Large Igneous Province, Southwestern China. Journal of Petrology, 57(5): 1019-1048.

[10] She, Y.W., Song, X.Y., Yu, S.Y., and He, H. L., 2015. Variations of trace element concentration of magnetite and ilmenite from the Taihe layered intrusion, Emeishan large igneous province, SW China: Implications for magmatic fractionation and origin of Fe–Ti–V oxide ore deposits. Journal of Asian Earth Sciences, 113: 1117-1131.

[11] She, Y.W., Yu, S.Y., Song, X.Y., Chen, L.M., Zheng, W.Q., Luan, Y. 2014. The formation of P-rich Fe-Ti oxide ore layers in the Taihe layered intrusion, SW China: Implications for magma-plumbing system process. Ore geology reviews, 57：539-559

[12] Chen, L.M., Song, X.Y., Zhu, X.K., Zhang, X.Q., Yu, S.Y., Yi, J.N. 2014. Iron isotope fractionation during crystallization and sub-solidus re-equilibration: Constraints from the Baima mafic layered intrusion, SW China. Chemical Geology, 380: 97-109.

[13] Song, X.Y., Qi, H.W., Hu, R.Z., Chen, L.M., Yu, S.Y. , Zhang, J.F. 2013. Formation of thick stratiform Fe-Ti oxide layers in layered intrusion and frequent replenishment of fractionated mafic magma: evidence from the Panzhihua intrusion, SW China. Geochemistry, Geophysics, Geosystems, 2013, 14(3): 712-732

[14] Luan, Y., Song, X.Y., Chen, L.M., Zheng, W.Q., Zhang, X.Q., Yu, S.Y. , She, Y.W., Tiao, X.L., Ran, Q.Y. 2013. Key factors controlling the accumulation of the Fe–Ti oxides in the Hongge layered intrusion in the Emeishan Large Igneous Province, SW China，Ore Geology Reviews. 57: 518-538

[15] Zhang, X.Q., Song, X.Y., Chen, L.M., Yu, S.Y., Xie, W., Deng, Y.F., Zhang, J.F., Gui, S.G. 2013. Chalcophile element geochemistry of the Baima layered intrusion, Emeishan Large Igneous Province, SW China: implications for sulfur saturation history and genetic relationship with high-Ti basalts. Contributions to Mineralogy and Petrology. 166, 193-209

[16] Zhang, X.Q., Song, X.Y., Chen, L.M., Xie, W., Yu, S.Y., Zheng, W.Q., Deng, Y.F., Zhang, J.F., Gui, S.G. 2012. Fractional crystallization and the formation of thick Fe–Ti–V oxide layers in the Baima layered intrusion, SW China. Ore Geology Reviews. 49: 96-108

[17] He, B., Xu, Y.G.，Huang, X.L.，Luo, Z.Y.，Shi, Y.R.，Yang, Q.J., Yu, S.Y. 2007. Age and duration of the Emeishan flood volcanism, SW China: Geochemistry and SHRIMP zircon U-Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation and clay tuff at the Chaotian section. Earth and Planetary Science Letters 255: 306-323.

[18] 朱飞霖，陶琰，胡瑞忠，于宋月，屈文俊，杜安道. 2011. 四川省会理县青矿山Ni-Cu-PGE矿床成因机制的Re-Os同位素证据. 岩石学报，27 (9): 2655-2664

[19] 秦秀峰, 徐义刚，张辉煌，于宋月，邱华宁, 2008. 大陆亚碱性火山岩的成因多样性：以敦化-密山和东宁火山岩带为例. 岩石学报24（11）： 2501-2514

[20] 陈列锰，易俊年，宋谢炎，于宋月，佘宇伟，颉炜，栾燕，向建新. 2014. 峨眉山大火成岩省内带黑谷田含钒钛磁铁矿层状岩体成因. 岩石学报 30（5）：1415-1431

[21] 郑文勤，邓宇峰，宋谢炎，陈列锰，于宋月，周国富，刘世荣，向建新. 2014. 攀枝花岩体钛铁矿成分特征及其成因意义. 岩石学报 30（5）：1432-1442

[22] 佘宇伟，宋谢炎，于宋月，陈列锰，魏宇，郑文勤. 2014. 磁铁矿和钛铁矿成分对四川太和富磷灰石钒钛磁铁矿床成因的约束. 岩石学报 30（5）：1443-1456

[23] 宋谢炎，邓宇峰，颉炜，陈列锰，于宋月，梁庆林，2018. 新疆黄山-镜儿泉铜镍成矿带岩浆作用与区域走滑构造的关系. 地球科学与环境学报，40(5):505-519.

[24] 胥应红，王京彬，宋谢炎，王向兰，陈列锰，于宋月. 2015.加拿大奈恩地球镁铁-超镁铁岩体稀土元素地球化学特征及其意义. 24(S2): 135-142