Steady-State Flow in Polycrystalline Halite at Pressure of 2 Kilobars

作者: Hugh C. Heard

DOI: 10.1029/GM016P0191

关键词: CrystalliteGeologyStress–strain curveMineralogyHalite

摘要: … In the region where steady-state flow prevails, all data are consistent with Weertman's models of creep by dislocation climb and well fit by ɛ' = A exp (-E/RT) σN , where A = 3 × 10 -6 sec …

参考文章(405)
George P. Rigsby, Crystal Orientation in Glacier and in Experimentally Deformed Ice Journal of Glaciology. ,vol. 3, pp. 589- 606 ,(1960) , 10.1017/S0022143000023716
W.F. Brace, James D. Byerlee, Recent Experimental Studies Of Brittle Fracture Of Rocks The 8th U.S. Symposium on Rock Mechanics (USRMS). ,(1966)
O.D. Sherby, M.T. Simnad, PREDICTION OF ATOMIC MOBILITY IN METALLIC SYSTEMS Trans. Am. Soc. Metals. ,(1961)
Ulf Dworak, Stoßwellenmetamorphose des Anorthosits vom Manicouagan Krater, Québec, Canada Contributions to Mineralogy and Petrology. ,vol. 24, pp. 306- 347 ,(1969) , 10.1007/BF00371273
N. J. Tighe, Microstructure of Fine-Grain Ceramics Springer, Boston, MA. pp. 109- 133 ,(1970) , 10.1007/978-1-4684-2643-4_7
Ekkehart Kr�ner, Berechnung der elastischen Konstanten des Vielkristalls aus den Konstanten des Einkristalls European Physical Journal. ,vol. 151, pp. 504- 518 ,(1958) , 10.1007/BF01337948
I. Y. Borg, H. C. Heard, Experimental Deformation Of Plagioclases Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung. pp. 375- 403 ,(1970) , 10.1007/978-3-642-95187-9_15