„Periglaciális” változatai közötti eltérés
| [ellenőrzött változat] | [ellenőrzött változat] |
Tartalom törölve Tartalom hozzáadva
12. sor:
==Irodalom==
*J.S. Levy, J.W. Head, D.R. Marchant, G.A. Morgan, J.L. Dickson. (2007): Gully-polygon interactions and stratigraphy on Earth and Mars: Sand-wedge polygons as part of cold-desert, near-surface fluvial systems. The 46th Vernadsky-Brown Microsymposium on Comparative Planetology. V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry Russian Academy of Sciences, Moscow, Russia, October 2-3, 2007
*Levy, J.S., Head, J.W., Marchant, D.R., and *Kowalewski, D.E. (2008). Identification of sublimation-type thermal contraction crack polygons at the proposed NASA landing site: implications for substrate properties and climate-driven morphological evolution. Geophysical Research Letters, 35, L04202, doi:10.1029/2007GL032813.
*Krevslasky, M.A., Head, J.W. III, and Marchant, D.R. (2008). Periods of active permafrost layer formation during the geological history of Mars: implications for circum-polar and mid-latitude surface processes. Planetary and Space Sciences 56, 289-302 doi:10.1016/j.pss.2006.02.010.
==Külső hivatkozások==
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