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王永锋
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的个人主页 http://grzy.cug.edu.cn/yongfeng
博士生导师 硕士生导师
性别 :
男
毕业院校 :
中国地质大学(武汉)
学历 :
博士研究生
学位 :
理学博士学位
所在单位 :
地球科学学院
学科 :
构造地质学
Email :
a559115223f0fdc3c7485fe19a84f3709356a43e682d8783b630a47601087dc01d0d51b396526d0c61e857ea1dd7e09952fdbbff5ce5a9206f5a803e8587782d74af5ad27b480a6ee427e0f18041114b13c0eabe3410eacc73f5db7f3abc5ac9639980dbb2084a99895a4be722c466ae47c4937edf1ffbd408ff075f77167f1c
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[1] Influence of melt-peridotite interactions on deformation and seismic properties of the upper mantle beneath a destroyed craton: A case study of the Damapong peridotites from the North China Craton. Journal of Geophysical Research: Solid Earth (128)
[2] Hydrostatic dehydration fabrics of antigorite at high pressure and high temperature: Implications for trench parallel seismic anisotropy at convergent plate boundaries. Journal of Geophysical Research: Solid Earth (126)
[3] Rheology of dry K-feldspar aggregates at high temperature and high pressure: An experimental study. Tectonophysics (817)
[4] Pyroxene does not always preserve its source hydrogen concentration: Clues from some peridotite xenoliths. Geochimica et Cosmochimica Acta,292 :382 ~ 408
[5] Rheology of felsic granulite at high temperature and high pressure. Journal of Geophysical Research: Solid Earth,126
[6] An investigation of dislocation in olivine phenocrysts from the Hawaiian basalts. Journal of Earth Science (30):1183 ~ 1189
[7] An FTIR study of kyanite in the Maobei kyanite-bearing eclogites from the Sulu orogenic belt, eastern China. Journal of Earth Science,29 :21 ~ 29
[8] Anisotropic growth of olivine during crystallization in basalts from Hawaii: Implications for olivine fabric development. American Mineralogist,103 :735 ~ 741
[9] Late Triassic alkaline complex in the Sulu UHP terrane: Implications for post-collisional magmatism and subsequent fractional crystallization. GONDWANA RESEARCH,35 :390 ~ 410
[10] Water and fabric in an ophiolitic peridotite from a supra-subduction zone. Contributions to Mineralogy and Petrology,171 (22)
[11] 西藏马攸木地区雅江南带方辉橄榄岩的显微构造特征及其矿物结构水的初步研究. 岩石学报,32 :1653 ~ 1662
[12] 斜方辉石筛状反应边的成因机制及其对岩石圈地幔性质转变的意义. 岩石矿物学杂志,32 :604 ~ 612
[13] The origin and geophysical implications of a weak C-type olivine fabric in the Xugou ultrahigh pressure garnet peridotite. Earth and Planetary Science Letters,376 :63 ~ 73
[14] Petrofabric and strength of SiO2 near the quartz-coesite phase boundary. JOURNAL OF METAMORPHIC GEOLOGY,31 :83 ~ 92
[15] Low oxygen fugacity dependency for the deformation of partially molten lherzolite. TECTONOPHYSICS,580 :114 ~ 123
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中国地质大学(武汉)校址:湖北省武汉市鲁磨路388号