Timing of crystallisation of the Lunar Magma Ocean constrained by the oldest zircon 1 2 3 4
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S. Reddy | N. Timms | T. Geisler | R. Pidgeon | A. Nemchin | C. Meyer
[1] D. Prior,et al. Some garnet microstructures: an illustration of the potential of orientation maps and misorientation analysis in microstructural studies , 2002 .
[2] A. V. Chichagov,et al. MINCRYST: A crystallographic database for minerals, local and network (WWW) versions , 2001 .
[3] H. Leroux,et al. Experimental shock deformation in zircon: a transmission electron microscopic study , 1999 .
[4] A. Boyle,et al. Plastic deformation of metamorphic pyrite: new evidence from electron-backscatter diffraction and forescatter orientation-contrast imaging , 1998 .
[5] D. Mainprice,et al. Misorientation analysis and the formation and orientation of subgrain and grain boundaries , 1997 .
[6] W. Compston,et al. Uranium‐lead ages for lunar zircons: Evidence for a prolonged period of granophyre formation from 4.32 to 3.88 Ga , 1996 .
[7] J. Kramers,et al. Approximation of terrestrial lead isotope evolution by a two-stage model , 1975 .
[8] N. Gale. Uranium--lead systematics in lunar basalts. , 1972 .
[9] G. Wasserburg,et al. U-Th-Pb systematics in three Apollo 14 basalts and the problem of initial Pb in lunar rocks , 1972 .
[10] S. Reddy,et al. Electron backscatter diffraction analysis of zircon: A systematic assessment of match unit characteristics and pattern indexing optimization , 2008 .
[11] Rossnr M. HezrN,et al. Crystal structure and compressibility of zircon at high pressure , 1979 .