Publications

 

Articles

Couvy H., Chen J., Drozd V.: Compressibility of nanaocrystalline forsterite. Physics and Chemistry of Minerals. in press, DOI: 10.1007/s00269-009-0337-8

Chen J., Couvy H., Liu H., Drozd V., Daemen L.L., Zhao Y., Kao C-C.: In situ x-ray study of ammonia borane at high pressure. International Journal of Hydrogen Energy, Submitted

Terry M.P., Heidelbach F., Couvy H., Bromiley G.D,: Deformation and metamorphism of the Kvalvika peridotite, Norway: Conditions and timing for olivine c-slip and exhumation at ultrahigh pressure. Journal of Metamorphic Geology. In revision

Rabier J., Renault P.O., Eyidi D., Demenet J.L., Chen J., Couvy H., Wang L. (2007) Plastic Deformation of Silicon Between 20 degrees C and 425 Degrees C.Phys. Status Solidi C, 4(8), 3110-3114.

Nyilas K., Couvy H., Cordier P., Ungar T. (2006): The Dislocation-Structure and Crystallite-Size in Forsterite (Olivine) Deformed at 1400°C by 11 GPa. Zeitschrift für Kristallographie Suppl., 23, 135-140.

Couvy H. (2005): Experimental deformation of forsterite, wadsleyite and ringwoodite: Implications for seismic anisotropy of the Earth's mantle. Ph.D Dissertation. Universitaet Bayreuth and Université des Sciences et Technologies de Lille, Bayreuth and Villeneuve d'Ascq.

Cordier P., Couvy H., Merkel S., Weidner D.J. (2005): Plastic deformation of minerals at high pressure: Experimental techniques. in "Mineral Behaviour at Extreme Conditions", R. Miletich, Ed. 339-355.

Mainprice D., Tommasi A., Couvy H., Cordier P., Frost D.J. (2004): Pressure sensitivity of olivine slip systems: implications for the interpretation of seismic anisotropy of the Earth's upper mantle. Nature, 433, 731-733.

Tommasi A., Mainprice D., Cordier P., Thoraval, C., Couvy H. (2004): Strain-induced seismic anisotropy of wadsleyite polycrystals and flow patterns in the mantle transition zone. Journal of Geophysical Research - Solid Earth.

Couvy H., Frost D.J., Heidelbach, F., Nyilas K., Ungár T., Mackwell S.J., Cordier P. (2004): Shear deformation experiments of forsterite at 11 GPa-1400°C in the multianvil apparatus. European Journal of Mineralogy, 16, 877-889.