@article{10272/16338,
year = {1992},
url = {http://hdl.handle.net/10272/16338},
abstract = {In Majanillos Formation (middle -upper Ladinian age) of the Subbetic Zone, the bioturbate textures are related with deep ramp facies. F/ieTlialassinoides trace fossil is placed in the middle levels of the formation corresponding to lagoon facies (low energy). And the Diplocaaterion, Rhizocorallium and Chondrites trace fossils are related with the shallower facies of a restricted stone},
publisher = {Sociedad Geológica de España},
title = {Estructuras bioturbadas de las facies Muschelkalk de la Zona Subbética},
title = {Bioturbate structures of the Muschelka lk fades in the Subbetic Zone},
author = {Pérez López, Alberto},
}