郭顺

中国科学院地质与地球物理研究所

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  • 郭顺
  • 副研究员
  • 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
简历:
郭顺,男,1982年9月生于辽宁鞍山,中国科学院地质与地球物理研究所副研究员 教育经历:2001/09-2005/07 中国地质大学(北京),宝石与材料工艺学,学士2005/09-2010/06 中国科学院地质与地球物理研究所 矿物学、岩石学、矿床学,博士工作经历:2010/06-2013/01 中国科学院地质与地球物理研究所 矿物学、岩石学、矿床学,博士后2013/01-至今 中国科学院地质与地球物理研究所 副研究员
学科类别:
变质岩石学
研究方向:
超高压变质作用和大陆深俯冲俯冲带深部流体活动和元素迁移变质矿物原位地球化学分析缅甸抹谷变质带演化和宝石成因
职务:
社会任职:
承担科研项目情况:
国家自然基金委面上基金项目两项(41372079、41672059)国家自然基金委青年基金项目一项(41102034)博士后科学基金面上资助一项(2011M500384)
获奖及荣誉:
2017年入选中国科学院青年创新促进会2010年获中国科学院优秀毕业生2009年获中国科学院“科教结合”教育创新项目优秀学生奖
代表论著:
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, 266-267: 383-405.Guo, S., Chen, Y., Liu, C.Z., Wang, J.G., Su, B., Gao, Y.J., Wu, F.Y., Kyaing, Sein, 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.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.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 eclogite from the Dabie terrane: insights from key mineral compositional zonations. International Geology Review, 57, 1077-1102. 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. DOI: 10.1007/s00410-014-0975-9.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 multi-stage epidote (Ganghe, Dabie UHP terrane). Journal of Metamorphic Geology, 31, 415-435.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, 136–139, 145–167. 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. 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,57(22),2186-2191.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(5), 1486-1498.