摘要
The Casablanca region is world famous for its fossil sites,ranging from the Mio-Pliocene to the Holocene. The"gazelles cave"at Tamaris I in the region of Casablanca(Morocco),was recently discovered during construction work.It forms a pocket,cut into the marine calcarenite of the A(i|¨)n Roumman Member and is filled with continental sediments(Lahlalfa member) of Upper Pleistocene age.The fauna is largely dominated by gazelles,hence the name given to this locality.Ankle bones discovered at the
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期304-305,共2页
Earth Science Frontiers