中国地质大学(武汉)导师教师师资介绍简介-郭新转

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的个人主页 http://grzy.cug.edu.cn/guoxinzhuan
副教授博士生导师硕士生导师

性别 : 男
毕业院校 : 冈山大学
学历 : 博士研究生毕业
学位 : 博士学位
所在单位 : 地质过程与矿产资源国家重点实验室
学科 : 矿物学、岩石学、矿床学构造地质学
联系方式 : gxzhuan@cug.edu.cn
Email :

个人简介
简介
郭新转博士，男，汉族，中共党员，中国地质大学（武汉）地质过程与矿产资源国重点实验室副教授，博士生导师。2003年在吉林大学本科毕业，2012年在日本冈山大学行星物质科学研究所获博士学位。2012-2014年在日本冈山大学受地球流体学会资助，担任特别研究员（博士后）； 2014年至今在中国地质大学(武汉)任副研究员。2015年获评湖北省楚天学子。目前致力于壳幔物质在高温高压下的物性、相变、流变实验研究。主持国家自然科学基金面上项目1项、参于国家自然科学基金重大项目等多项。已在Geology、EPSL、GRL、Am. Miner.、PEPI、CMP等SCI杂志发表论文30余篇。
个人信息
地址：湖北省武汉市洪山区鲁磨路388号中国地质大学（武汉）
邮箱：gxzhuan@cug.edu.cn
电话：**
教育经历
2008/10-2012/3，日本冈山大学，惑星物质研究所，博士，导师：芳野极
2006/10-2008/9，日本岛根大学，地球科学系，硕士，导师：高须晃
2003/10-2006/7，吉林大学，地球科学学院，硕士，导师：刘永江
1999/9-2003/7，吉林大学，地球科学学院，学士，导师：刘永江
工作经历
1. 2014/04-至今，中国地质大学（武汉），地质过程与矿产资源国家重点实验室，副研究员
2. 2012/4-2014/4，日本冈山大学，惑星物质研究所，博士后，合作导师：芳野极
科研及人才项目
1. 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（排名第二）
2. 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，在研，主持
3. 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
4. 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
5. 湖北省“楚天****”（“楚天学子”），2015年，地质学
发表论文
(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 (Mg_0.92Fe_0.08)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 (Mg_0.83,Fe_0.17)O and (Mg_0.75,Fe_0.25)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 (Mg_0.83Fe_0.17)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 margin of the Qaidam basin.Geological Bulletin ofChina,23(9~10), 899-902.
招收硕士研究生方向：（1）矿物学、岩石学、矿床学，（2）构造地质学
招收博士研究生方向：高温高压矿物物理
学生科研、获奖情况： 所招研究生都积极参于了导师的科研项目，并取得了丰硕的科研成果。其中，硕士生陈思博获得2016国家奖学金，并以第一作者身份在国内外一流期刊《Geology》和《Science China Earth Science》各发表一篇；硕士生李平以第一作者身份在《Contributions to Mineralogy and Petrology》发表论文一篇。

中国地质大学(武汉)导师教师师资介绍简介-郭新转

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