Author/Authors :
Schmedemann، نويسنده , , N. and Kneissl، نويسنده , , T. and Ivanov، نويسنده , , B.A. and Michael، نويسنده , , G.G. and Wagner، نويسنده , , R.J. and Neukum، نويسنده , , G. and Ruesch، نويسنده , , O. and Hiesinger، نويسنده , , H. and Krohn، نويسنده , , K. and Roatsch، نويسنده , , T. and Preusker، نويسنده , , F. and Sierks، نويسنده , , H. and Jaumann، نويسنده , , R. and Reddy، نويسنده , , V. and Nathues، نويسنده , , A. and Walter، نويسنده , , S.H، نويسنده ,
Abstract :
We derived model functions for the crater production size-frequency distribution and chronology of the asteroids 951 Gaspra, 243 Ida, 21 Lutetia and 4 Vesta, based on a lunar-like crater production function and a lunar-like chronology with a smooth exponential decay in impact rate for the first ~1 Ga of Solar System history. For Gaspra, Ida and Lutetia we find surface ages roughly in agreement with published data. Using the same approach for Vesta leads to results with high correlation to Ar–Ar reset ages of HED meteorites, for which a strong dynamical and spectroscopic connection to Vesta has been found. In contrast to recently published young formation ages of the Rheasilvia and Veneneia basins of about 1 and 2 Ga, respectively, we find for Rheasilvia a formation age of 3.5±0.1 Ga and for the Veneneia formation a lower limit of 3.7±0.1 Ga. For comparison we also give surface model ages for a preliminary version of a chronology (pers. comm. D.P. O׳Brien) based on the Late Heavy Bombardment theory. Error bars presented in our work stem only from statistical analysis of measured crater distributions and do not include the uncertainty of the used chronology model.
Keywords :
Crater retention ages , Crater scaling , Cratering chronology , Rheasilvia , Veneneia , Vesta