[en] The Saarland impact (Fig. 1) [1-5] has been an established event for several years with the existence of two craters with diameters of about 200 m (Nalbach) and Saarlouis (2.3 km). Finds of rocks and glasses in a strewn field (Fig. 1) with typical impact features (e.g. suevites) strengthened the impact hypothesis and initiated comprehensive mineralogical SEM-EDS and thin section analyses establishing strong shock metamorphism. Here we report on recent finds of shatter cone fracture markings diagnostic of meteorite impact shock.
Disciplines :
Earth sciences & physical geography
Author, co-author :
SIEGEL, Ulrich ; University of Luxembourg > Faculty of Science, Technology and Medicine (FSTM) > Department of Physics and Materials Science (DPHYMS)
ROMMELFANGEN, Jonathan ; University of Luxembourg > Faculty of Science, Technology and Medicine (FSTM) > Department of Physics and Materials Science (DPHYMS)
Müller, Werner
Michelbacher, Stefan
Ernstson, Kord; Universitity of Würzburg, 97074 Würzburg, Germany