TY - JOUR
T1 - Experimental impact cratering
T2 - A summary of the major results of the MEMIN research unit
AU - Kenkmann, Thomas
AU - Deutsch, Alex
AU - Thoma, Klaus
AU - Ebert, Matthias
AU - Poelchau, Michael H.
AU - Buhl, Elmar
AU - Carl, Eva Regine
AU - Danilewsky, Andreas N.
AU - Dresen, Georg
AU - Dufresne, Anja
AU - Durr, Nathanaël
AU - Ehm, Lars
AU - Grosse, Christian
AU - Gulde, Max
AU - Güldemeister, Nicole
AU - Hamann, Christopher
AU - Hecht, Lutz
AU - Hiermaier, Stefan
AU - Hoerth, Tobias
AU - Kowitz, Astrid
AU - Langenhorst, Falko
AU - Lexow, Bernd
AU - Liermann, Hanns Peter
AU - Luther, Robert
AU - Mansfeld, Ulrich
AU - Moser, Dorothee
AU - Raith, Manuel
AU - Reimold, Wolf Uwe
AU - Sauer, Martin
AU - Schäfer, Frank
AU - Schmitt, Ralf Thomas
AU - Sommer, Frank
AU - Wilk, Jakob
AU - Winkler, Rebecca
AU - Wünnemann, Kai
N1 - Publisher Copyright:
© The Meteoritical Society, 2018.
PY - 2018/8
Y1 - 2018/8
N2 - This paper reviews major findings of the Multidisciplinary Experimental and Modeling Impact Crater Research Network (MEMIN). MEMIN is a consortium, funded from 2009 till 2017 by the German Research Foundation, and is aimed at investigating impact cratering processes by experimental and modeling approaches. The vision of this network has been to comprehensively quantify impact processes by conducting a strictly controlled experimental campaign at the laboratory scale, together with a multidisciplinary analytical approach. Central to MEMIN has been the use of powerful two-stage light-gas accelerators capable of producing impact craters in the decimeter size range in solid rocks that allowed detailed spatial analyses of petrophysical, structural, and geochemical changes in target rocks and ejecta. In addition, explosive setups, membrane-driven diamond anvil cells, as well as laser irradiation and split Hopkinson pressure bar technologies have been used to study the response of minerals and rocks to shock and dynamic loading as well as high-temperature conditions. We used Seeberger sandstone, Taunus quartzite, Carrara marble, and Weibern tuff as major target rock types. In concert with the experiments we conducted mesoscale numerical simulations of shock wave propagation in heterogeneous rocks resolving the complex response of grains and pores to compressive, shear, and tensile loading and macroscale modeling of crater formation and fracturing. Major results comprise (1) projectile–target interaction, (2) various aspects of shock metamorphism with special focus on low shock pressures and effects of target porosity and water saturation, (3) crater morphologies and cratering efficiencies in various nonporous and porous lithologies, (4) in situ target damage, (5) ejecta dynamics, and (6) geophysical survey of experimental craters.
AB - This paper reviews major findings of the Multidisciplinary Experimental and Modeling Impact Crater Research Network (MEMIN). MEMIN is a consortium, funded from 2009 till 2017 by the German Research Foundation, and is aimed at investigating impact cratering processes by experimental and modeling approaches. The vision of this network has been to comprehensively quantify impact processes by conducting a strictly controlled experimental campaign at the laboratory scale, together with a multidisciplinary analytical approach. Central to MEMIN has been the use of powerful two-stage light-gas accelerators capable of producing impact craters in the decimeter size range in solid rocks that allowed detailed spatial analyses of petrophysical, structural, and geochemical changes in target rocks and ejecta. In addition, explosive setups, membrane-driven diamond anvil cells, as well as laser irradiation and split Hopkinson pressure bar technologies have been used to study the response of minerals and rocks to shock and dynamic loading as well as high-temperature conditions. We used Seeberger sandstone, Taunus quartzite, Carrara marble, and Weibern tuff as major target rock types. In concert with the experiments we conducted mesoscale numerical simulations of shock wave propagation in heterogeneous rocks resolving the complex response of grains and pores to compressive, shear, and tensile loading and macroscale modeling of crater formation and fracturing. Major results comprise (1) projectile–target interaction, (2) various aspects of shock metamorphism with special focus on low shock pressures and effects of target porosity and water saturation, (3) crater morphologies and cratering efficiencies in various nonporous and porous lithologies, (4) in situ target damage, (5) ejecta dynamics, and (6) geophysical survey of experimental craters.
UR - https://www.scopus.com/pages/publications/85050927308
U2 - 10.1111/maps.13048
DO - 10.1111/maps.13048
M3 - Article
AN - SCOPUS:85050927308
SN - 1086-9379
VL - 53
SP - 1543
EP - 1568
JO - Meteoritics and Planetary Science
JF - Meteoritics and Planetary Science
IS - 8
ER -