姓名： 郭新转 性别： 男

职称： 研究员 学历： 博士

电话： ** 传真： 无

Email： gxzhuan@mail.gyig.ac.cn 邮编： 550081

地址： 贵州省贵阳市观山湖区林城西路99号


简历：
学习经历：
1999.09—2003.07 吉林大学，固体矿产勘察专业，学士学位
2003.09—2006.12吉林大学，大地构造专业，硕士学位
2006.10—2008.09，日本岛根大学，变质岩石学专业，硕士学位
2008.10—2012.03，日本冈山大学，行星物质科学，博士学位
工作经历：
2012.04—2014.03，日本冈山大学，惑星物质研究所，博士后
2014.04—2019.05，中国地质大学（武汉），地质过程与矿产资源国家重点实验室，副教授
2019.06—现在，中国科学院地球化学研究所，地球内部物质高温高压重点实验室，研究员

研究方向：
高温高压实验技术、地球内部物质传输特性、变质岩石学

承担科研项目情况：
(1) 中央高校基本科研业务费, G，2014.1-2016.1, 主持
(2) 国家重大科研仪器研制项目，**，基于同步辐射X射线谱学的水热大腔体高温高压装置，2019/01/-2023/12，675万，在研，参加
(3) 国家自然科学基金重大项目，**, 水对壳幔矿物和岩石流变性质的影响与俯冲带地震成因， 2016/01-2020/12，422.5万元，在研，参加
(4) 国家重点研发计划，2016YFC**, 青藏高原碰撞造山成矿系统深部结构与成矿过程，2016/07-2020/12, 768万元，在研，参加
(5) 国家自然科学基金面上项目，**, 高温高压下含盐水岩石的电导率实验研究：对地壳中的高电导率异常的启示， 2015/01-2018/12, 98万元，结题，主持
(6) 湖北省“楚天****”（“楚天学子”），2015年，地质学
(7) 中国科学院“西部引进人才” (Y9CR026)，2019.01-2024.04，主持

专家类别：
中国科学院“西部引进人才”
职务：

社会任职：
中国矿物岩石地球化学学会会员

获奖及荣誉：
亚洲高压联盟TANDEM国际会议，优秀青年科学家奖，2010

代表论著：
(1) Chen S., Guo* X., Yoshino T., Jin Z., Li P., 2018. Dehydration of phengite inferred by electrical conductivity measurements: Implication for the high conductivity anomalies relevant to the subduction zones. Geology, 46 (1): 11-14.
(2) Li P., Guo* X., Chen S., Wang C., Yang J., Zhou X., 2018. Electrical conductivity of the plagioclase-NaCl-water system and its implication for the high conductivity anomalies in the mid-lower crust of Tibet Plateau. Contributions to Mineralogy and Petrology, 173:16. https://doi.org/10.1007/s00410-018-1442-9
(3) Guo* X., 2016. Experimental study of the electrical conductivity of hydrous minerals in the crust and the mantle under high pressure and high temperature. Science China: Earth Sciences, 59:696-706.
(4) Chen S., Guo* X., Zhou C., Jin Z., 2016. Negative pressure effect on the electrical conductivity of San Carlos olivine and its implication to the electrical structure in the upper mantle. Science China: Earth Sciences, 59: 2078-2088.
(5) Guo X*., Yoshino T., Shimojuku A., 2015. Electrical conductivity of albite-(quartz)-water and albite-water-NaCl systems and its implication to the high conductivity anomalies in the continental crust. Earth and Planetary Science Letters, 412:1-9.
(6) Guo* X., 2015. Reply to comments on “Electrical conductivity of albite–(quartz)–water and albite–water–NaCl systems and its implication to the high conductivity anomalies in the continental crust” by Guo, X., Yoshino, T. & Shimojuku, A. Earth and Planetary Science Letters 423, 246-247.
(7) Guo* X., Yoshino T., 2014. Pressure-induced enhancement of proton conduction in brucite. Geophysical Research Letters, 41:813-819.
(8) Guo* X., Takasu A., Liu Y., Li W., 2014. Zn-rich spinel in association with quartz in the Al-rich metapelites from the Mashan khondalite series,NE China. Journal of Earth Science, 25(2):207-223.
(9) Guo* X., Yoshino T., 2013. Electrical conductivity of dense hydrous magnesium silicates with implication for conductivity in the stagnant slab.Earth and Planetary Science Letters, 369-370: 239-247.
(10) Guo* X., Yoshino T., Okuchi T., Tomioka N., 2013. H-D interdiffusion in brucite at pressures up to 15 GPa. American Mineralogist, 98: 1919-1929.
(11) Guo* X., Yoshino T., Katayama I., 2011. Electrical conductivity anisotropy of deformed talc rocks and serpentinites at 3 GPa. Physics Earth and Planetary Interiors, 188:69-81.
(12) 郭新转，刘永江*，葛肖虹，袁四化，孙知明，裴军令，李伟民. 2006. 柴西红三旱一号地区新生代砂岩成分分析及其区域构造意义.吉林大学学报（地球科学版），36（2）：194-201.
(13) Xu J., Zhang D., Fan* D., Zhang J., Hu Y., Guo X., Dera* P., Zhou W., 2018. Phase Transitions in Orthoenstatite and Subduction Zone Dynamics: Effects of Water and Transition Metal Ions. Journal of Geophysical Research: Solid Earth, 123: 2723-2737.
(14) Wu* X., Wu Y., Lin J., Liu J., Mao Z., Guo X., Yoshino T., McCammon C., Prakapenka V., Xiao Y., 2016. Two-stage spin transition of iron in FeAl-bearing phase D at lower mantle. Journal of Geophysical Research: Solid Earth, 121:6411-6420.
(15) Yamazaki* D., Ito E., Yoshino T., Tsujino N., Yoneda A., Guo X., Xu F., Higo Y., Funakoshi K., 2014. Over 1 Mbar generation in the Kawai-type multianvil apparatus and its application to compression of (Mg0.92Fe0.08)SiO3 perovskite and stishovite.Physics Earth and Planetary Interiors,228，262-267.
(16) Zhai* S., Yamazaki D., Xue W., Ye L., Wu C., Shan S., Ito E., Yoneda A., Yoshino T., Guo X., Shimojuku A., Tsujino N., Funakoshi K., 2013. P-V-T relations of gamma-Ca3(PO4)2tuite determined by in situ X-ray diffraction in a large-volume high-pressure apparatus.American Mineralogist,98: 1811-1816.
(17) Yoshino* T., Shimojuku A., Shan S., Guo X., Yamazaki D., Ito E., Higo Y., Funakoshi K., 2012. Effect of temperature, pressure and iron content on the electrical conductivity of olivine and its high-pressure polymorphs. Journal of Geophysical Research: Solid Earth,117, B08205.
(18) Yamazaki* D., Ito E., Yoshino T., Yoneda A., Guo X., Zhang B., Sun W, Shimojuku A., Tsujino N., Kunimoto T., Higo Y., Funakoshi K., 2012. P-V-T equation of state for ε-iron up to 80 GPa and 1900 K using the Kawai-type high pressure apparatus equipped with sintered diamond anvils.Geophysical Research Letters, 39, L20308.
(19) Li* W., Takasu A., Liu Y., Genser J., Zhao Y., Han G., Guo X., 2011. U-Pb and40Ar/39Ar age constrains on protolith and high-P/T type metamorphism of the Heilongjiang Complex in the Jiamusi Massif,NE China.Journal of Mineralogical and Petrological Sciences, 106: 326-331.
(20) Matsui* M., Ito E., Yamazaki D., Yoshino T., Guo X., Shan S., Higo Y., Funakoshi K., 2011. Static compression of (Mg0.83,Fe0.17)O and (Mg0.75,Fe0.25)O ferropericlase up to 58 GPa at 300, 700, and 1100 K. American Mineralogist,97: 176-183.
(21) Xu* J., Ito E., Yamazaki D., Guo X., Wu X., 2011. Synthesis and crystal chemical characterization of the pyrochlore type MgZrSi2O7.Materials Chemistry and Physics, 128: 410-412.
(22) Yamazaki* D., Ito E., Katsura T., Yoshino T., Zhai S., Fukui H., Shatskiy A., Guo, X., Shan S., Okuchi T., Tange Y., Higo Y., Funakoshi K., 2011. Phase boundary between perovskite and post-perovskite structures in MnGeO3determined by in situ X-ray diffraction measurements using sintered diamond anvils.American Mineralogist,96:89-92.
(23) Yoshino* T., Ito E., Katsura T., Yamazaki D., Shan S., Guo X., Nishi M., Higo Y., Funakoshi K., 2011. Effect of iron content on electrical conductivity of ferro-periclase with implications for the spin transition pressure. Journal of Geophysical Research: Solid Earth,116, B04202.
(24) Yamazaki* D., Ito E., Yoshino T., Guo X., Shan S., Nishi M., Higo Y., Funakoshi K., 2010. Preliminary reports on in situ X-ray observation of post-perovskite in CaRuO3.Journal of Physics: Conference series,215, 012096.
(25) Ito* E., Yoshino T., Yamazaki D., Shatskiy A., Shan S., Guo X., Katsura T., Higo Y., Funakoshi K., 2010. High pressure generation and investigation of the spin transition of ferropericlase (Mg0.83Fe0.17)O.Journal of Physics: Conference series,215 (1), 012099.
(26) Li* W., Takasu A., Liu Y., Guo X., 2010. Newly discovered garnet-barroisite schists from the Heilongjiang Complex in the Jiamusi Massif, northeasternChina.Journal of Mineralogical and Petrological Sciences, 105: 86-91.
(27) Pei* J., Sun Z., Wang X., Zhao Y., Ge X., Guo X., Li H., Si J., 2009. Evidence for Tibetan Plateau Uplift in Qaidam Basin before Eocene–Oligocene Boundary and Its Climatic Implications.Journal of Earth Science,2: 018.
(28) Li* W., Takasu A., Liu Y., Genser J., Neubauer F., Guo X., 2009.40Ar/39Ar ages of the high-P/T metamorphic rocks of the Heilongjiang Complex in the Jiamusi Massif, northeasternChina.Journal of Mineralogical and Petrological Sciences,104: 110-116.
(29) Yuan* S., Liu Y., Ge X., We G., Guo, X., Li W., 2008. Uplift time of the northern Qinghai-Xizang Plateau: The evidences from the Altyn Mountains and Qaidam Basi.Acta Petrologica et Mineralogica,27: 14-19.
(30) Yuan S., Liu* Y., Ge X., Ren S., Wu G., Li W., Liu H., Guo X., 2006. Advance in study of Mesozoic-Cenozoic uplift history of theAltynMountains.Global Geology,25(2), 164-171.
(31) Li W., Liu* Y., Sun Z., Ge X., Ren S., Pei J., Yuan S., Guo X., 2006. New paleomagnetic evidences of Paleogene tectonic rotation of theQaidamBasinand vicinity region: Mechanism and its tectonic implication.Global Geology, 9(1): 40-48.
(32) Sun* Z., Yang Z., Ge X., Pei J., Guo X., Li W., Ma Z., Xu S., 2004. Advances in the study of the Paleogene magnetostratigraphy on the northwestern ">Geological Bulletin ofChina,23(9~10), 899-902.