The chemical variability at the surface of Mars: implications for exogenic processes (2005)
Kolb, Christopher, Martín Fernández, Josep Antoni, Abart, R., Lammer, Helmut, Pawlowsky Glahn, Vera
The chemical composition of sediments and rocks, as well as their distribution at theMartian surface, represent a long term archive of processes, which have formed theplanetary surface. A survey of...
An ultraviolet simulator for the incident Martian surface radiation and its applications (2005)
Kolb, C., Abart, R., Bérces, A., Garry, J.R.C., Hansen, A.A., Hohenau, W., ...
Ultraviolet (UV) radiation can act on putative organic/biological matter at the Martian surface in several ways. Only absorbed, but not transmitted or reflected, radiation energy can be...
An ultraviolet simulator for the incident Martian surface radiation and its applications (2005)
Kolb, C., Abart, R., Berces, A., Garry, J. C., Hansen, A. A., Hohenau, W., ...
Ultraviolet (UV) radiation can act on putative organic/biological matter at the Martian surface in several ways. Only absorbed, but not transmitted or reflected, radiation energy can be...
KELLER, L. M., DE CAPITANI, C., ABART, R.
A thermodynamic model for the quaternary white mica solid solution with end-members muscovite–Mg-celadonite–paragonite–Fe-celadonite (Ms–MgCel–Pg–FeCel) is presented. The interaction...
KELLER, L. M., ABART, R., SCHMID, S. M., DE CAPITANI, C.
The metamorphic evolution of metapelites from the eastern part of the Monte Rosa nappe and the Camughera–Moncucco unit, both situated in the upper Penninic units SW of the Simplon line, were...
KELLER, L. M., DE CAPITANI, C., ABART, R.
A thermodynamic model for the quaternary white mica solid solution with end-members muscovite-Mg-celadonite-paragonite-Fe-celadonite (Ms-MgCel-Pg-FeCel) is presented. The interaction energies for the...
KELLER, L. M., ABART, R., SCHMID, S. M., DE CAPITANI, C.
The metamorphic evolution of metapelites from the eastern part of the Monte Rosa nappe and the Camughera-Moncucco unit, both situated in the upper Penninic units SW of the Simplon line, were...