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姓名 陈意 性别:
职称 副研究员 学位 博士
电话 010-82998534 传真: 010-62010846
Email: chenyi@mail.iggcas.ac.cn 邮编: 100029
地址 北京朝阳区北土城西路19号,中科院地质与地球物理研究所
更多信息:
 
简历:

陈意,男,1980年12月出生于湖北黄冈市。副研究员。

时间 学校/工作单位名称        专业        学位/职称
1999.09-2003.07  中国地质大学(武汉)  地质学      学士学位
2003.09-2008.07  中科院地质与地球物理研究所 矿物学、岩石学、矿床学 博士学位
2008.07-2010.12  中科院地质与地球物理研究所     变质岩石学     博士后
2011.02-现今   中科院地质与地球物理研究所     变质岩石学     副研究员

 
学科类别:
地质学
 
研究方向:
主要从事板块俯冲及其改造的变质岩石学研究。
目前主要研究方向:
1. 高压-超高压变质岩石学
2. 俯冲带壳幔物质循环
3. 高级变质岩热力学模拟
 
职务:
 
社会任职:
 
承担科研项目情况:
  1. 中国科学院知识创新工程青年人才领域前沿项目,造山带石榴橄榄岩中钛斜粒硅镁石的成因及其对俯冲带高场强元素活动性的指示,2007.10-2009.09
  2. 国家自然科学基金青年基金(40902023):毛屋基性-超基性岩的变质演化及其对俯冲地壳流体与地幔楔相互作用的启示,2010.01-2012.12
  3. 国家自然科学基金面上项目(41372078):低温地幔楔底部对重稀土和高场强元素的过滤作用:对岛弧岩浆成因的启示,2014.01-2017.12
  4. 中国科学院战略性先导科技专项(B类)子课题(XDB03010202):新特提斯洋俯冲过程变质和超基性岩成因研究,2012.07-2017.06
  5. 国家重点基础研究发展计划(973)子课题(2015CB856103),超深俯冲陆壳对地幔楔的改造,2015/01-2019/12
  6. 国家自然科学基金重大项目课题(41490614),东西构造结大陆岩石圈俯冲的变质响应,2015/01-2019/12
  7. 国家自然科学基金优秀青年基金项目(41822202),变质岩石学,2019/01-2021/12
 
获奖及荣誉:
  1. 2008年获中国科学院“王宽诚博士后工作奖”
  2. 2018年获“侯德封矿物岩石地球化学青年科学家奖”
 
代表论著:

ResearchGate 

第一/通讯作者论文

19. Chen, Y., Huang, F., Shi, G.H., Wu, F.Y., Chen, X., Jin, Q.Z., Su, B., Guo, S., Sein, K., Nyunt, T.T., 2018. Magnesium isotope composition of subduction zone fluids as constrained by jadeitites from Myanmar. Journal of Geophysical Research: Solid Earth, doi: 10.1029/2018JB015805.

18. Su, B., Chen, Y.*, 2018. Making Cratonic Lithospheric Mantle. Journal of Geophysical Research: Solid Earth, doi: 10.1029/2018JB016179. (通讯作者)

17. 陈意,陈思,苏斌,李仪兵,郭顺,2018。麻粒岩相金红石微量元素体系。地球科学,43(1),127–149.

16. Chen, Y., Su, B., Chu, Z.Y., 2017. Modification of an ancient subcontinental lithospheric mantle by continental subduction: Insight from the Maowu garnet peridotites in the Dabie UHP belt, eastern China. Lithos, 278-281, 54–71.

15. Su, B., Chen, Y.*, Guo, S., Liu, J.B., 2017. Dolomite dissociation indicates ultra-deep (>150 km) subduction of a garnet-bearing dunite block (the Sulu UHP terrane). American Mineralogist, 102, 2295–2306 (通讯作者).

14. 王娟,陈意*,毛骞,李秋立,马玉光,石永红,宋传中,2017。金红石微量元素电子探针分析。岩石学报,33(6): 1934–1946. (通讯作者)

13. Su, B., Chen, Y.*, Guo, S., Chu, Z. Y., Liu, J. B., Gao, Y. J., 2016. Carbonatitic metasomatism in orogenic dunites from Lijiatun in the Sulu UHP terrane, eastern China. Lithos, 262, 266–284 (通讯作者).

12. Su, B., Chen, Y.*, Guo, S., Liu, J.B., 2016. Origins of orogenic dunites: Petrology, geochemistry, and implications. Gondwana Research, 29, 41–59 (通讯作者).

11. Chen, Y., Su, B., Guo, S., 2015. The Dabie-Sulu orogenic peridotites: Progress and key issues. Science China Earth Science, 58, 1679–1699.

10. Chen, Y., Ye, K., Wu, T. F., Guo, S., 2013. Exhumation of oceanic eclogites: thermodynamic constraints on pressure, temperature, bulk composition and density: Journal of Metamorphic Geology, 31, 549–570.

9. Chen, Y., Ye, K., Wu, Y.W., Guo, S., Su, B., Liu, J.B., 2013. Hydration and Dehydration in the lower margin of a cold mantle wedge: implications for crust–mantle interactions and petrogeneses of arc magmas. International Geology Review, 55, 1506–1522.

8. Chen, Y., Ye, K., Guo, S., Wu, T.F., Liu, J.B., 2013, Multistage metamorphism of garnet orthopyroxenites from the Maowu mafic-ultramafic complex, Dabieshan UHP terrane, eastern China. International Geology Review, 55, 1239–1260.

7. 陈意,叶凯,苏斌,郭顺,刘景波。2013。大别-苏鲁造山带橄榄岩的变质和交代过程。科学通报,58(23):2294–2299.

6. 陈意,叶凯。2013。俯冲洋壳的折返及其相关问题讨论。岩石学报,29(5):1451–1478。

5. Chen, Y., Ye, K., Liu, J.B. & Sun, M., 2008. Quantitative P–T–X constraints on orthopyroxene-bearing high-pressure granulites in felsic-metapelitic rocks: evidence from the Huangtuling granulite, Dabieshan Orogen. Journal of Metamorphic Geology, 26, 1–15.

4. 陈意,叶凯,刘景波,孙敏。2007。斜方辉石高压麻粒岩的成因研究进展。科学通报,52 (22):2682。

3. Chen, Y., Ye, K., Liu, J.B. & Sun, M., 2006. Multistage metamorphism of the Huangtuling granulite, Northern Dabie Orogen, eastern China: implications for the tectonometamorphic evolution of subducted lower continental crust. Journal of Metamorphic Geology, 24, 633–654.

2. 陈意,叶凯,吴春明。2005。榴辉岩常用温压计在应用中应注意的问题。岩石学报,21:1067–1080。

1. 陈意,金振民,欧新功,金淑燕,徐海军。2004。韧性剪切带中片麻岩和超高压榴辉岩变形特征及其与地震波速各向异性的关系:来自中国大陆科学钻探(CCSD)680–1200米岩心的证据。岩石学报,20:97–108。

 

合作作者论文

25. Guo, S., Tang, P., Su, B., Chen, Y., Ye, K., Zhang, L.M., Gao, Y.J., Liu, J.B., Yang, Y.H., 2017. Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins (Dabie UHP terrane): A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs. American Mineralogist, 102, 2268–2283.

24. Xu, Y., Liu, C.Z., Chen, Y., Guo, S., Wang, J.G., Sein, K., 2017. Petrogenesis and tectonic implications of gabbro and plagiogranite intrusions in mantle peridotites of the Myitkyina ophiolite, Myanmar. Lithos, 284, 180–193.

23. Li, X.H., Chen, Y., Tchouankoue, J.P., Liu, C.Z., Li, J., Ling, X.X., Tang, G.Q., Liu, Y., 2017. Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints. Precambrian Research, 294, 307–321.

22. Guo, S., Yang, Y.H., Chen, Y., Su, B., Gao, Y.J., Zhang, L.M., Liu, J.B., Mao, Q., 2016. Grain-scale Sr isotope heterogeneity in amphibolite (retrograded UHP eclogite, Dabie terrane): Implications for the origin and flow behavior of retrograde fluids during slab exhumation. Lithos, 266, 383–405.

21. Liu, C.Z., Zhang, C., Xu, Y., Wang, J.G., Chen, Y., Guo, S., Wu, F.Y., Sein, K., 2016. Petrology and geochemistry of mantle peridotites from the Kalaymyo and Myitkyina ophiolites (Myanmar): Implications for tectonic settings. Lithos, 264, 495–508.

20. Li, X.H., Chen, Y., Li, J., Yang, C., Ling, X.X., Tchouankoue, J. P., 2016. New isotopic constraints on age and origin of Mesoarchean charnockite, trondhjemite and amphibolite in the Ntem Complex of NW Congo Craton, southern Cameroon. Precambrian Research, 276, 14–23.

19. Liu, C.Z., Chung, S.L., Wu, F.Y., Zhang, C., Xu, Y., Wang, J.G., Chen, Y., Guo, S., 2016. Tethyan suturing in Southeast Asia: Zircon U-Pb and Hf-O isotopic constraints from Myanmar ophiolites. Geology, 44, 311–318.

18. Guo, S., Chen, Y., Liu, C.Z., Wang, J.G., Su, B., Gao, Y.J., Wu, F.Y., Sein, K., Yang, Y.H., Mao, Q., 2016. Scheelite and coexisting F-rich zoned garnet, vesuvianite, fluorite, and apatite in calc-silicate rocks from the Mogok metamorphic belt, Myanmar: Implications for metasomatism in marble and the role of halogens in W mobilization and mineralization. Journal of Asian Earth Sciences, 117, 82–106.

17. Guo, S., Chen, Y., Ye, K., Su, B., Yang, Y.H., Zhang, L.M., Liu, J.B., Mao, Q., 2015. Formation of multiple high-pressure veins in ultrahigh-pressure eclogite (Hualiangting, Dabie terrane, China): Fluid source, element transfer, and closed-system metamorphic veining. Chemical Geology, 417, 238–260.

16. Liu, S.A., Huang, J., Liu, J.G., Woerner, G., Yang, W., Tang, Y.J., Chen, Y., Tang, L.M., Zheng, J.P., Li, S.G., 2015. Copper isotopic composition of the silicate Earth. Earth and Planetary Science Letters, 427, 95–103.

15. Guo, S., Ye, K., Cheng, N.F., Chen, Y., Su, B., Liu, J.B., 2015. Metamorphic P-T trajectory and multi-stage fluid events of vein-bearing UHP eclogites from the Dabie terrane: insights from compositional zonations of key minerals. International Geology Review, 57, 1077–1102.

14. Liu, P.L., Wu, Y., Chen, Y., Zhang, J.F., Jin, Z.M., 2014. UHP impure marbles from the Dabie Mountains: Metamorphic evolution and carbon cycling in continental subduction zones. Lithos, 212, 280–297.

13. Xiao, L.L., Liu, F.L., Chen, Y., 2014. Metamorphic P-T-t paths of the Zanhuang metamorphic complex: Implications for the Paleoproterozoic evolution of the Trans-North China Orogen. Precambrian Research, 255, 216–235.

12. Guo, S., Ye, K., Yang, Y.H., Chen, Y., Zhang, L.M., Liu, J.B., Mao, Q., Ma, Y.G., 2014. In situ Sr isotopic analyses of epidote: tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite (Ganghe, Dabie terrane). Contributions to Mineralogy and Petrology, 167, DOI: 10.1007/s00410-014-0975-9.

11. Guo S., Ye K., Wu T.F., Chen Y., Yang Y.H., Zhang L.M., Liu J.B., Mao Q., Ma Y.G., 2013. A potential method to confirm the previous existence of lawsonite in eclogite: the mass imbalance of Sr and LREEs in multistage epidote (Ganghe, Dabie UHP terrane), Journal of Metamorphic Geology, 31(4), 415–435.

10. Xu, H.J., Ye, K., Song, Y.R., Chen, Y., Zhang, J.F., Liu, Q., Guo, S., 2013. Prograde metamorphism, decompressional partial melting and subsequent melt fractional crystallization in the Weihai migmatitic gneisses, Sulu. Chemical Geology, 341, 16–37.

9. 郭顺,叶凯,陈意,刘景波,毛骞, 2013。大别山榴辉岩中超高压硬柱石脱水分解及其对俯冲带深部流体活动的制约。科学通报,58(22): 2186–2191。

8. 刘景波,张灵敏,陈意,郭顺,程南飞,2013。大别-苏鲁造山带超高压榴辉岩和脉体磷灰石含氯特征与变质流体演化。科学通报,58(22): 2165–2168.

7. 郭顺,叶凯,陈意,刘景波,张灵敏,2013。开放地质体系中物质迁移质量平衡计算方法介绍。岩石学报,29,1486–1498.

6. 张灵敏,刘景波,程南飞,叶凯,郭顺,陈意,毛骞, 2013。大别-苏鲁高压-超高压变质带榴辉岩和脉体中磷灰石氯含量和流体盐度关系的研究。岩石学报,29,1525–1539.

5. Guo, J.H., Peng, P., Chen, Y., Jiao, S.J., Windley, B.F., 2012. UHT sapphirine granulite metamorphism at 1.93-1.92 Ga caused by gabbronorite intrusions: Implications for tectonic evolution of the northern margin of the North China Craton. Precambrian Research, 222, 124–142.

4. Guo, S., Ye, K., Chen, Y., Liu, J.B., Mao, Q., Ma, Y.G., 2012. Fluid-rock interaction and element mobilization in UHP metabasalt: Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen. Lithos, 136, 145–167.

3. Ye, K., Song, Y.R., Chen, Y., Xu, H.J., Liu, J.B., Sun, M., 2009. Multistage metamorphism of orogenic garnet-lherzolite from Zhimafang, Sulu UHP terrane, E. China: Implications for mantle wedge convection during progressive oceanic and continental subduction. Lithos, 109, 155–175.

2. Guo, S., Ye, K., Chen, Y., Liu, J.B., 2009. A normalization solution to mass transfer illustration of multiple progressively altered samples using the isocon diagram. Economic Geology, 104, 881–886.

1. Sun, M., Chen, N.S., Zhao, G.C., Wilde, S.A., Ye, K., Guo, J.H., Chen, Y., Yuan, C., 2008. U-Pb zircon and Sm-Nd isotopic study of the Huangtuling granulite, Dabie-Sulu belt, China: Implication for the paleoproterozoic tectonic history of the Yangtze Craton. American Journal of Science, 308, 469–483.

 

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