於宋月，男，2003年本科畢業於吉林大學地球科學學院資源勘查專業，2003-2008年在中國科學院廣州地球化學研究所岩石地球化學專業碩博連讀，並於2008年獲得理學博士學位。2008-2018年，在中國科學院地球化學研究所礦床地球化學國家重點實驗室任助理研究員、副研究員；2019年至今在中國科學院地球化學研究所礦床地球化學國家重點實驗室任研究員，博士生導師
基本介紹
- 中文名：於宋月
- 國籍：中國
- 畢業院校：吉林大學
- 性別：男
人物經歷,研究方向,承擔項目情況,代表論著,
人物經歷
1999.09—2003.06：畢業於吉林大學地球科學學院資源勘查專業，
2003.09—2008.06：中國科學院廣州地球化學研究所碩博連讀，並獲碩士，博士學位
2008.06—2018.12：中國科學院地球化學研究所助理研究員、副研究員
2019.05至今：中國科學院地球化學研究所研究員
研究方向
地幔柱岩漿作用與成礦多樣性
西太平洋俯衝過程與中國東部岩石圈減薄
承擔項目情況
主持和參與多項國家自然科學基金、重點研發、“973項目”和中科院先導項目等
代表論著
代表著作I:（第一作者及通訊作者文章）
[1] Yu, S.-Y., Song, X.-Y. and Chen,L.-M., 2024. Interaction between mantle plume and subduction-modifiedlithospheric mantle: Geochemical evidence from the picritic lavas from theEmeishan large igneous province. Chemical Geology, 648: 121964.
[2] Chen, Q., Yu, S-Y., Chen, L-M.,Zhou, S-H., Kang, J., 2023. Textural and compositional zoning in plagioclasephenocrysts: implications for magma chamber processes in the Emeishan largeIgneous Province, SW China. Acta Geochimica. https://doi.org/10.1007/s11631-023-00601-1（通訊作者）
[3] Zhou, S.-H.,Yu, S.-Y., Shu, Q., Chen,L.-M. and Kang, J., 2023. Formation and evolution of lithospheric mantlebeneath the Yilan-Yitong Fault Zone, Northeast China: Constraints from theShangzhi peridotite xenoliths. Journal of Asian Earth Sciences: 105746. （通訊作者）
[4] Yu, S.-Y., Xu, Y.-G., Huang,K.-J., Lan, J.-B., Chen, L.-M. and Zhou, S.-H., 2021. Magnesium isotopeconstraints on contributions of recycled oceanic crust and lithospheric mantleto generation of intraplate basalts in a big mantle wedge. Lithos, 398-399:106327. https://doi.org/10.1016/j.lithos.2021.106327.（第一作者）
[5] Yu, S.-Y., Chen, L.-M., Lan, J.-B., He, Y.-S., Chen,Q. and Song, X.-Y., 2020. Controls of mantle source and condition of meltextraction on generation of the picritic lavas from the Emeishan large igneousprovince, SW China. Journal of Asian Earth Sciences, 203: 104534.https://doi.org/10.1016/j.jseaes.2020.104534.（第一作者）
[6] 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 Cenozoicbasaltic lavas from the Changbaishan-Baoqing Volcanic Belt, NE China: Productsof lithosphere-asthenosphere interaction induced by subduction of the Pacificplate. Journal of Asian Earth Sciences, 164: 260-273.（第一作者）
[7]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 peridotitexenoliths from Shangzhi, NE China: products of recent melt/fluid-peridotiteinteraction. Acta Geochimica.37(5): 769-789.（通訊作者）
[8] Yu, S.Y., Shen, N.P., Song,X.Y., Ripley, E.M., Li, C. and Chen, L.M., 2017. An integrated chemical andoxygen isotopic study of primitive olivine grains in picrites from the EmeishanLarge Igneous Province, SW China: Evidence for oxygen isotope heterogeneity inmantle sources. Geochimica et Cosmochimica Acta, 215: 263-276.（第一作者）
[9] Yu S.Y., Song X.Y., Ripley, E.M.,Chusi Li, Chen L.M., She Y.W., Luan Y. 2015. Integrated O–Sr–Nd isotopeconstraints on the evolution of four important Fe–Ti oxide ore-bearingmafic–ultramafic intrusions in the Emeishan large igneous province, SW China.Chemical Geology 401: 28-42. （第一作者）
[10] Yu, S.Y., Song, X.Y., Chen,L.M., Li, X.B. 2014. Postdated melting of subcontinental lithospheric mantle bythe Emeishan mantle plume: Evidence from the Anyi intrusion, Yunnan,SW China.Ore geology reviews, 2014, 57: 560-573.（第一作者）
[11] Yu, S.Y., Song, X.Y. Xu, Y.G.,Chen, L.M., Li, J. 2012. Effects of melt percolation on the Re-Os systematicsof continental mantle lithosphere: A case study of spinel peridotite xenolithsfrom Heilongjiang, NE China. Science in China Series D 55：869-1042. （第一作者）
[12] 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 ofoceanic lower crust in the subcontinental lithospheric mantle: Trace elementand Sr-Nd-O isotope evidence from aluminous garnet pyroxenite xenoliths fromJiaohe, Northeast China. Earth and Planetary Science Letters 297(3-4): 413-422.（第一作者）
[13] 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 incontinental mantle lithosphere beneath Northeast China: Effects of pervasivemantle metasomatism. Journal of Asian Earth Sciences 35: 554-570.（第一作者）.
[14] 於宋月，徐義剛，黃小龍，葛文春，程錦. 2007. 東北和華北地區上地幔成分和熱狀態對比及對中國東部岩石圈減薄的啟示. 岩石學報 23（6）：1252-1268. （第一作者）.
[15] 於宋月，徐義剛，黃小龍，葛文春，馬金龍. 2007.吉林雙遼地區橄欖岩包體中熔體-岩石作用特徵及其對地幔交代作用的啟示. 岩石礦物學雜誌 26（3）：213-222. （第一作者）.
[16] 於宋月; 宋謝炎; E.M.Ripley;Chusi Li; 陳列錳; 佘宇偉; 欒燕, 2015. O-Sr-Nd同位素對峨眉山大火成岩省中含釩鈦磁鐵礦岩體成因的制約, 礦物學報, S1：177. （第一作者）
[17] 於宋月，藍江波，陳琦，2020，峨眉山苦橄岩原始岩漿成分反演及對地幔熔融條件的評估，礦物岩石地球化學通報，39期，DOI：10.19658/j.issn.1007-2802.2020.39.068,（第一作者）
[18]陳琦，於宋月，溫漢捷，藍江波，羅重光，2020，滇東-黔西地區峨眉山玄武岩Nb-Ga-REE富集機制及賦存狀態初步研究，礦物岩石地球化學通報，39期，DOI：10.19658/j.issn.1007-2802.2020.39.069,（通訊作者）
[19] 陳琦，於宋月. 2021. 長白山新生代斜斑玄武岩的岩漿作用過程與岩石成因制約. 礦物岩石地球化學通報，40期，DOI：10.19658/j.issn.1007-2802.2022.40.107（通訊作者）
代表著作II:（共同作者文章）
[1] Liang, Q.-L., Song, X.-Y., Smolkin, V., Krivolutskaya, N.A., Yu,S.-Y. and Chen, L.-M., 2024. Mineralogy and geochemistry of magnetite in theZhdanov Ni-Cu-(PGE) deposit in the Pechenga ore field, Russia: Implications forthe formation of magmatic sulfide ores. Journal of Asian Earth Sciences, 259:105903.
[2] Chen, L.-M., Lightfoot, P.C., Zhu, J.-M., Teng, F.-Z., Duan, Q., Yin,R., Wu, G., Yu, S.-Y. and Hu, R.-Z., 2023. Nickel isotope ratios trace theprocess of sulfide-silicate liquid immiscibility during magmaticdifferentiation. Geochimica et Cosmochimica Acta, 353: 1-12.
[3] Deng, Y.-F., Song, X.-Y., Xie, W., Chen, L.-M., Yu, S.-Y., Yuan, F.,Hollings, P. and Wei, S., 2022. The Role of External Sulfur in TriggeringSulfide Immiscibility at Depth: Evidence from the Huangshan-Jingerquan Ni-CuMetallogenic Belt, NW China. Economic Geology, 117(8): 1867-1879.
[4] He, H.-L., Chen, L.-M., Song, X.-Y., Fu, B., Yi, J.-N., Yu, S.-Y. andDeng, Y.-F., 2022. Genesis of the Xiarihamu Magmatic Ni-Co Sulfide Deposit inthe East Kunlun Orogen, Northern Tibetan Plateau: In Situ Oxygen Isotope andGeochemical Perspectives. Economic Geology, 117(8): 1827-1844.
[5] Kang, J.,Chen, L.-M., Yu, S.-Y., Zheng, W.-Q., Dai, Z.-H., Zhou, S.-H. and Ai, Q.-X.,2022. Chromite geochemistry of the Jinchuan Ni-Cu sulfide-bearing ultramaficintrusion (NW China) and its petrogenetic implications. Ore Geology Reviews,141: 104644
[6] Liang,Q.-L., Song, X.-Y., Wirth, R., Chen, L.-M., Yu, S.-Y., Krivolutskaya, N.A. and Dai, Z.-H., 2022.Thermodynamic conditions control the valences state of semimetals thusaffecting the behavior of PGE in magmatic sulfide liquids. Geochimica etCosmochimica Acta, 321: 1-15.
[7] Yin, R.,Chen, D., Pan, X., Deng, C., Chen, L., Song, X., Yu, S-Y., Zhu, C., Wei, X., Xu, Y., Feng, X., Blum, J.D. andLehmann, B., 2022. Mantle Hg isotopic heterogeneity and evidence of oceanic Hgrecycling into the mantle. Nature Communications, 13(1).
[8] Song X-Y,Deng Y-F, Xie W, Yi J-N, Fu B, Chen L-M, YuS-Y, Zheng W-Q, Liang Q-L, 2021. Prolonged basaltic magmatism andshort-lived magmatic sulfide mineralization in orogenic belts. Lithos390-391:106114 doi:10.1016/j.lithos.2021.106114
[9] Chen, L.-M.,Teng, F.-Z., Song, X.-Y., Luan, Y., Yu,S.-Y. and Kang, J., 2021. Origins and implications of magnesiumisotopic heterogeneity in Fe–Ti oxides in layered mafic intrusions. Geochimicaet Cosmochimica Acta, 308: 273-290
[10] Chen L-M,Song X-Y, Hu R-Z, Yu S-Y, YiJ-N, Kang J, Huang K-J. 2021. Mg–Sr–Nd Isotopic Insights into Petrogenesis ofthe Xiarihamu Mafic–Ultramafic Intrusion, Northern Tibetan Plateau, China.Journal of Petrology 62(2) https://doi.org/10.1093/petrology/egaa113
[11] Yao, J.-H.,Zhu, W.-G., Li, C., Zhong, H., Yu,S., Ripley, E.M. and Bai, Z.-J., 2019. Olivine O isotope and traceelement constraints on source variation of picrites in the Emeishan floodbasalt province, SW China. Lithos, 338-339: 87-98.
[12] 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 theDamiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-Oisotopes. Precambrian Research, 332: 105396.
[13] 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 andcomposition of clinopyroxene phenocrysts of Holocene volcanic rocks on amagmatic plumbing system beneath Tengchong, SW China. Journal of Asian EarthSciences, 154: 342-353.（共同作者）
[14] Chen, L.M.,Teng, F.Z., Song, X.Y., Hu, R.Z., Yu,S.Y., Zhu, D. and Kang, J., 2018. Magnesium isotopic evidence forchemical disequilibrium among cumulus minerals in layered mafic intrusion.Earth and Planetary Science Letters, 487: 74-83. （共同作者）
[15]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 ontrace-element partitioning among co-crystallizing minerals: Evidence from thePanzhihua layered intrusion, SW China. American Mineralogist, 102(5):1006-1020. （共同作者）
[16] 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 geochemistryof 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. （共同作者）
[17] 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 oreof the Damiao anorthosite complex, NE China: Evidence from trace elementgeochemistry of apatite, plagioclase, magnetite and ilmenite. Ore GeologyReviews, 79: 367-381. （共同作者）
[18] She, Y.W.,Song, X.Y., Yu, S.Y., Chen,L.M. and Zheng, W.-Q., 2016. Apatite geochemistry of the Taihe layeredintrusion, SW China: Implications for the magmatic differentiation and theorigin of apatite-rich Fe-Ti oxide ores. Ore Geology Reviews, 78: 151-165.
[19] Arguin,J.-P., Pagé, P., Barnes, S.-J., Yu,S.-Y. and Song, X.-Y., 2016. The Effect of Chromite Crystallization onthe 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. （共同作者）
[20] She, Y.W.,Song, X.Y., Yu, S.Y., and He,H. L., 2015. Variations of trace element concentration of magnetite andilmenite from the Taihe layered intrusion, Emeishan large igneous province, SWChina: Implications for magmatic fractionation and origin of Fe–Ti–V oxide oredeposits. Journal of Asian Earth Sciences, 113: 1117-1131. （共同作者）
[21] 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 orelayers in the Taihe layered intrusion, SW China: Implications formagma-plumbing system process. Ore geology reviews, 57：539-559（共同作者）
[22] Chen, L.M.,Song, X.Y., Zhu, X.K., Zhang, X.Q., Yu,S.Y., Yi, J.N. 2014. Iron isotope fractionation during crystallizationand sub-solidus re-equilibration: Constraints from the Baima mafic layeredintrusion, SW China. Chemical Geology, 380: 97-109. （共同作者）
[23] 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 oxidelayers in layered intrusion and frequent replenishment of fractionated maficmagma: evidence from the Panzhihua intrusion, SW China. Geochemistry,Geophysics, Geosystems, 2013, 14(3): 712-732（共同作者）
[24] 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. Keyfactors controlling the accumulation of the Fe–Ti oxides in the Hongge layered intrusion in theEmeishan Large Igneous Province, SW China，Ore Geology Reviews. 57: 518-538（共同作者）
[25] Zhang,X.Q., Song, X.Y., Chen, L.M., Yu,S.Y., Xie, W., Deng, Y.F., Zhang, J.F., Gui, S.G. 2013. Chalcophileelement geochemistry of the Baima layered intrusion, Emeishan Large IgneousProvince, SW China: implications for sulfur saturation history and geneticrelationship with high-Ti basalts. Contributions to Mineralogy and Petrology.166, 193-209（共同作者）
[26] 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. Fractionalcrystallization and the formation of thick Fe–Ti–V oxide layers in the Baimalayered intrusion, SW China. Ore Geology Reviews. 49: 96-108（共同作者）
[27] He, B., Xu,Y.G.，Huang,X.L.，Luo,Z.Y.，Shi,Y.R.，Yang,Q.J., Yu, S.Y. 2007. Age andduration of the Emeishan flood volcanism, SW China: Geochemistry and SHRIMPzircon U-Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation andclay tuff at the Chaotian section. Earth and Planetary Science Letters 255:306-323. （共同作者）
[28] 朱飛霖，陶琰，胡瑞忠，於宋月，屈文俊，杜安道. 2011. 四川省會理縣青礦山Ni-Cu-PGE礦床成因機制的Re-Os同位素證據. 岩石學報，27 (9): 2655-2664（共同作者）
[29] 秦秀峰, 徐義剛，張輝煌，於宋月，邱華寧, 2008. 大陸亞鹼性火山岩的成因多樣性：以敦化-密山和東寧火山岩帶為例. 岩石學報24（11）： 2501-2514（共同作者）
[30] 陳列錳，易俊年，宋謝炎，於宋月，佘宇偉，頡煒，欒燕，向建新. 2014. 峨眉山大火成岩省內帶黑谷田含釩鈦磁鐵礦層狀岩體成因. 岩石學報 30（5）：1415-1431（共同作者）
[31] 鄭文勤，鄧宇峰，宋謝炎，陳列錳，於宋月，周國富，劉世榮，向建新. 2014. 攀枝花岩體鈦鐵礦成分特徵及其成因意義. 岩石學報 30（5）：1432-1442（共同作者）
[32] 佘宇偉，宋謝炎，於宋月，陳列錳，魏宇，鄭文勤. 2014. 磁鐵礦和鈦鐵礦成分對四川太和富磷灰石釩鈦磁鐵礦床成因的約束. 岩石學報 30（5）：1443-1456
[33] 胥應紅，王京彬，宋謝炎，王向蘭，陳列錳，於宋月.2015.加拿大奈恩地球鎂鐵-超鎂鐵岩體稀土元素地球化學特徵及其意義.24(S2): 135-142（共同作者）
[34] 宋謝炎，鄧宇峰，頡煒，陳列錳，於宋月，梁慶林，2018.新疆黃山-鏡兒泉銅鎳成礦帶岩漿作用與區域走滑構造的關係. 地球科學與環境學報，40(5):505-519. （共同作者）
[35]宋謝炎，陳列錳，於宋月，陶琰等，2018，峨眉大火成岩省釩鈦磁鐵礦礦床地質特徵及成因，礦物岩石地球化學通報，37（6），1003-1018.
[36]鄧宇峰，宋謝炎，頡煒，袁峰，趙照明，韋帥，祝近近，康健，王開元，梁慶林，陳列錳，於宋月，2021，黃山-鏡兒泉銅鎳成礦帶地層時代的厘定及其地質意義探討，95（2）362-376
