By Erich Gröner; Dieter Jung; Martin Maass

ISBN-10: 3763748091

ISBN-13: 9783763748099

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Space weathering from Mercury to the asteroid belt. : Effects of vapor-phase deposition processes on the optical, chemical, and magnetic properties of the lunar regolith. : Satellite-sized planetesimals and lunar origin. : Characterization of lunar ilmenite resources. In: Proceedings of the 20th Lunar and Planetary Science Conference, pp. : Lunar deposits of possible pyroclastic origin. : Lunar Sourcebook: A User’s Guide to the Moon, p. 736. : Origins of igneous rocks, p. 336. : Lunar surface processes.

Between the solidus and liquidus curves is a mixture of crystals and melt. A discussion of phase diagrams, tying melt composition to the composition of early- and late-forming crystals, as well as the temperature of melting and temperature of crystallization, can be found in Hess (1989). g. Papike et al. 1998; represented by the light gray area). However, some extremely Fe-rich olivines (0-10% Mg2SiO4, represented by the dark gray area) have been found in extremely late stage crystallization mineral assemblages (Papike et al.

Between the solidus and liquidus curves is a mixture of crystals and melt. A discussion of phase diagrams, tying melt composition to the composition of early- and late-forming crystals, as well as the temperature of melting and temperature of crystallization, can be found in Hess (1989). g. Papike et al. 1998; represented by the light gray area). However, some extremely Fe-rich olivines (0-10% Mg2SiO4, represented by the dark gray area) have been found in extremely late stage crystallization mineral assemblages (Papike et al.

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Die deutschen Kriegsschiffe 1815-1945 [Vol 2] by Erich Gröner; Dieter Jung; Martin Maass


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