Pub-Nr. Information about Publication

Bischoff A., Schleiting M., Wieler R. and Patzek M. (2018): Brecciation among 2280 ordinary chondrites – Constraints on the evolution of their parent bodies. Volume 238, 516–541 Geochimica et Cosmochimica Acta, 10.1016/j.gca.2018.07.020


Schollenberger Q.R., Borg L.E., Render J., Ebert S., Bischoff A., S.S. Russell, Brennecka G.A. (2018): Isotopic coherence of refractory inclusions from CV and CK meteorites: Evidence from multiple isotope systems Volume 228, 62-80; Geochimica et Cosmochimica Acta, 10.1016/j.gca.2018.02.006


Zhu M.-H.,  Wünnemann K., and N. Artemieva (2018): Effects of Moon’s thermal state on the impact basin ejecta distribution. Geophysical Research Letters, 10.1002/2017GL075405


Patzek M., Bischoff A., Visser R. and John T. (2018). Mineralogy of volatile-rich clasts in brecciated meteorites Meteoritics & Planetary Science 1–22, 10.1111/maps.13175


Orgel C., Michael G., Fassett C.I., van der Bogert C.H.,Riedel C., Kneissl T., Hiesinger H. (2018): Ancient Bombardment of the Inner Solar System: Reinvestigation of the “Fingerprints” of Different Impactor Populations on the Lunar Surface, Journal of Geophysical Research: Planets, 123, 10.1002/2017JE005451


Ebert S., Render J., Brenneck A., Burkhardt C., Bischoff A., Gerber S., Kleine T. (2018). Ti isotopic evidence for a non-CAI refractory component in the inner Solar System. EPSL, Volume 498,Pages 257-265, 10.1016/j.epsl.2018.06.040


Steenstra ES, Seegers AX, Eisinga J, Tomassen BGJ, Webers FPF, Berndt J, Klemme S, Matveev S, van Westrenen W  (2018). Evidence for a sulfur-undersaturated lunar interior from the solubility of sulfur in lunar melts and sulfide-silicate partitioning of siderophile elements. Geochimica et Cosmochimica Acta, 231, 130-156,10.1016/j.gca.2018.04.008.


Steenstra E.S., Agmon N., Berndt J., Klemme S., Matveev S. and van Westrenen W.(2018) Depletion of potassium and sodium in mantles of Mars, Moon and Vesta by core formation, Scientific Reports, Volume 8, Article number: 7053, 10.1038/s41598-018-25505-6


Ruedas, T. and Breuer, D. (2017): On the relative importance of thermal and chemical buoyancy in regular and impact-induced melting in a Mars-like planet; Journal of Geophysical Research - Planets, 122(7), 1554-1579, 10.1002/2016JE005221.


Ballhaus C, Fonseca ROC, Münker, C, Rohrbach A, Nagel T, Speelmanns IM, Helmy HM, Zirner A, Vogel AK, and A. Heuser (2017): The great sulfur depletion of Earth's mantle is not a signature of mantle–core equilibration. 172, 68.Contributions to Mineraloly and Petrology, 10.1007/s00410-017-1388-3


Grützner T., Klemme S., Rohrbach A., Gervasoni F., Berndt J. (2018). The effect of fluorine on the stability of wadsleyite: Implications for the nature and depths of the transition zone in the Earth’s mantle. EPSL, 482, 236-244, 10.1016/j.epsl.2017.11.011


Kruijer T., Kleine T., Borg L. E. ,Brennecka G., Irving J. A., Bischoff A., Carl B. Ageed (2017) The early differentiation of Mars inferred from Hf–W chronometry. EPSL10.1016/j.epsl.2017.06.047


Bischoff A., Barrat J.-A.,Bauer K., Burkhardt C., Busemann H., Ebert S.,Gonsior M., Hakenmüller J.,Haloda J., Harries D., Heinlein D., Hiesinger H., Hochleitner R., Hoffmann V., Kaliwoda M., Laubenstein M., Maden C., Meier M. M. M., Morlok A., Pack A., Ruf A., Schmitt-Kopplin P., Schönbächler M., Steele R. C. J., Spurny P., and Wimmer K. 2017. The Stubenberg meteorite - an LL6 chondrite fragmental breccia recovered soon after precise prediction of the strewn field. Meteoritics & Planetary Science, 10.1111/maps.12883/pdf.


Render J. , Burkhardt T., Fischer-Gödde M., Kleine T. (2017) The cosmic molybdenum-neodymium isotope correlation and the building material of the Earth. Geochemical Perspective Letters, 10.7185/geochemlet.1720


Prieur N.C., Rolf T., Luther R., Wünnemann K., Xiao, Z., Werner S.C. (2017) Simple craters: Influence of target properties and crater
scaling relationships
. JGR Planets. 10.1002/2017JE005283


Padovan S., Tosi N., Plesa  A., Ruedas T. (2017). Impact-induced changes in source depth and volume of magmatism on Mercury and their observational signatures. Nature Communications 8, Article No. 1945, 10.1038/s41467-017-01692-0


Grützner T., Kohn S.C., Bromiley D.W., Rohrbach A., Berndt J., Klemme S. (2017). The storage capacity of fluorine in olivine and pyroxene under Upper Mantle conditions. Geochimica et Cosmochimica Acta, 208, 160, 10.1002/2016JE005221.


Grützner T., Klemme S., Rohrbach A., Gervasoni F., Berndt J. (2017). The role of F-clinohumite in volatile recycling processes in subduction zones. Geology, 45, 10.1130/G38788.1


Maurice M. ,Tosi N., Samuel H ., Plesa A.C.,Hüttig C., and Doris Breuer (2017): Onset of solid-state mantle convection and mixing during magma ocean solidification, 122, 3, J. Geophys. R. Planets, 10.1002/2016JE005250


Bischoff A., Wurm G., Chaussidon M., Horstmann M., Metzler K., Weyrauch M., Weinauer J. (2017): The Allende multi-compound chondrule (ACC) – chondrule formation in a local super-dense region of the early Solar System, 1-19, Meteoritics & Planetary Science, 10.1111/maps.12833 


Morlok, A., Bischoff A., Patzek M., Sohn M. und H. Hiesinger (2017): Chelyabinsk - a rock with many different (stony) faces: An infrared study. Icarus 284, 431-442, 10.1016/j.icarus.2016.11.030


Budde G., Kruijer T.S. , and Th. Kleine (2018): Hf-W chronology of CR chondrites: implications for the timescale of chondrule formation and the distribution of 26Al in the solar nebula. 222, 284-304, Geochimica et Cosmochimica Acta. 10.1016/j.gca.2017.10.014


Kruijer T. and Kleine T. (2016) Tungsten isotopes and the origin of the Moon. EPSL, 0.1016/j.epsl.2017.07.021


Kleine T. and R. Walker (2017): Tungsten Isotopes in Planets, Annual Reviews of Earth and Planetary Sciences, 45; doi: 10.1146/annurev-earth-063016-020037, 10.1146/annurev-earth-063016-020037


Fischer-Gödde M. and Kleine T. (2017): Ruthenium isotopic evidence for an inner Solar System origin of the late veneer541, 468-470, Nature. doi:10.1038/541468a.

Data: Fischer-Goedde, M., et al., (2016), Ruthenium isotopic composition of chondrites, iron meteorites and terrestrial chromitites. Integrated Earth Data Applications (IEDA). doi:10.1594/IEDA/100622.


Kruijer T., Burkhardt C., Budde G., Kleine T.(2017). Age of Jupiter inferred from the distinct genetics and formation times of meteorites. PNAS, 10.1073/pnas.1704461114


Wang Z. and Becker H. (2016) Silver contents and Cu/Ag ratios in Martian meteorites and the implications for planetary differentiation. Geochimica et Cosmochimica Acta, 10.1016/j.gca.2017.05.024


Bellucci J. J., Whitehouse M.J., John T., Nemchin A.A., Snape J. F., Bland P. A., Benedix G.K. (2016) Halogen and Cl isotopic systematics in Martian phosphates: Implications for the Cl cycle and surface halogen reservoirs on Mars. EPSL, 10.1016/j.epsl.2016.10.028


Sarafian A. R., John T., Roszjar J., Whitehouse M. J. (2016) Chlorine and hydrogen degassing in Vesta’s magma ocean. EPSL, 10.1016/j.epsl.2016.10.029


Rolf T., Zhub M.-H., Wünnemann K., Werner S.C. (2016): The role of impact bombardment history in lunar evolution, 286, 138–152, Icarus, 10.1016/j.icarus.2016.10.007


Wang Z. and Becker H. (2016) Chalcophile elements in Martian meteorites indicate low sulfur content in the Martian interior and a volatile element-depleted late veneer. EPSL, 10.1016/j.epsl.2017.01.023


Gleißner P. and Becker H. (2017): Formation of Apollo 16 impactites and the composition of late accreted material: constraints from Os isotopes, highly siderophile elements and sulfur abundances, 200, 1-24, Geochimica et Cosmochimica Acta, 10.1016/j.gca.2016.12.017 


Kneissl T., Michael G.G., Schmedemann N. (2016): Treatment of non-sparse cratering in planetary surface dating277187-195; Icarus. 10.1016/j.icarus.2016.05.015

Michael G., Basilevsky A., Neukum G. (2018) On the history of the early meteoritic bombardment of the Moon: Was there a terminal lunar cataclysm? Icarus, 10.1016/j.icarus.2017.10.046

Yue Z., Michael G.G., Di K., Liu J. (2017) Global survey of lunar wrinkle ridge formation times. EPSL, 10.1016/j.epsl.2017.07.048