Stability region of K0.2Na0.8AlSi3O8 hollandite at 22 GPa and 2273 K
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W. Du | H. Ohfuji | T. Irifune | T. Shinmei | Youmo Zhou
[1] H. Kojitani,et al. High-pressure phase transitions and subduction behavior of continental crust at pressure–temperature conditions up to the upper part of the lower mantle , 2012 .
[2] R. Caracas,et al. Elasticity of (K,Na)AlSi3O8 hollandite from lattice dynamics calculations , 2010 .
[3] K. Nakanishi,et al. High-pressure phase relations in the system CaAl4Si2O11–NaAl3Si3O11 with implication for Na-rich CAS phase in shocked Martian meteorites , 2010 .
[4] L. Dubrovinsky,et al. High-pressure ferroelastic phase transition in aluminosilicate hollandite , 2009 .
[5] M. Miyahara,et al. Transformation textures, mechanisms of formation of high‐pressure minerals in shock melt veins of L6 chondrites, and pressure‐temperature conditions of the shock events , 2009 .
[6] Lin‐gun Liu,et al. High-Pressure Phase Transitions of the Feldspars, and Further Characterization of Lingunite , 2007 .
[7] F. Tutti. Formation of end-member NaAlSi3O8 hollandite-type structure (lingunite) in diamond anvil cell , 2007 .
[8] Xi Liu. Phase relations in the system KAlSi3O8–NaAlSi3O8 at high pressure–high temperature conditions and their implication for the petrogenesis of lingunite , 2006 .
[9] T. Ferroir,et al. Equation of state and phase transition in KAlSi3O8 hollandite at high pressure , 2006 .
[10] P. Decarli,et al. High-pressure phases in a shock-induced melt vein of the Tenham L6 chondrite: Constraints on shock pressure and duration , 2006 .
[11] D. Yamazaki,et al. Stability and P–V–T equation of state of KAlSi3O8-hollandite determined by in situ X-ray observations and implications for dynamics of subducted continental crust material , 2005 .
[12] T. Ferroir,et al. A new high‐pressure form of KAlSi3O8 under lower mantle conditions , 2004 .
[13] T. Kondo,et al. Formation of high-pressure minerals in shocked L6 chondrite Yamato 791384: constraints on shock conditions and parent body size , 2004 .
[14] K. Hirose,et al. Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications , 2004 .
[15] N. Tomioka,et al. Shock‐induced transition of NaAlSi3O8 feldspar into a hollandite structure in a L6 chondrite , 2000 .
[16] T. Kikegawa,et al. In situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg2SiO4 , 2000 .
[17] L. Dubrovinsky,et al. Natural NaAlSi(3)O(8)-hollandite in the shocked sixiangkou meteorite , 2000, Science.
[18] T. Sharp,et al. The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in Chondrites , 1996, Science.
[19] C. Agee,et al. Pressure‐temperature phase diagram for the Allende meteorite , 1995 .
[20] O. Shimomura,et al. Synchrotron radiation study on the high-pressure and high-temperature phase relations of KAlSi3O8 , 1994 .
[21] Jianzhong Zhang,et al. Melting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPa , 1994 .
[22] T. Kikegawa,et al. The Phase Boundary Between α- and β-Mg2SiO4 Determined by in Situ X-ray Observation , 1994, Science.
[23] A. Yagi,et al. High pressure transitions in the system KAlSi3O8-NaAlSi3O8 , 1994 .
[24] K. Keil,et al. Shock metamorphism of ordinary chondrites , 1991 .
[25] A. E. Ringwood,et al. High-pressure KAlSi3O8, an aluminosilicate with sixfold coordination , 1967 .
[26] Masashi Yamamoto,et al. EDS quantification of light elements using osmium surface coating , 2015 .
[27] K. Kawai,et al. First-principles study on the high-pressure phase transition and elasticity of KAlSi3O8 hollandite , 2013 .
[28] H. Kojitani,et al. High-pressure phase relations of hollandite in the system KAlSi3O8-NaAlSi3O8 , 2005 .
[29] E. Ito,et al. Crystal-chemical characterization of KAlSi3O8 with the hollandite structure , 1984 .
[30] Lin‐gun Liu. High-pressure phase transformations of albite, jadeite and nepheline , 1978 .