RT Journal Article
T1 Estructuración y significado tectonoestratigráfico de la formación calizas de panda (moscoviense superior, zona cantábrica)
T1 Structure and tectonostratigraphic signficance of Panda limestone Fm. (Upper Moscovian, Cantabrian Zone)
A1 Motis, K.
A1 Fernández, Luis R.
A1 Heredia, N.
AB The Panda Limestone Formation (upper Podolsky to Podolsky-Myachkovsky boundary, Pisuerga-Carrión Province, Cantabrian Zone) forms part of the Pando Group, the syn-orogenic wedge related to the emplacement of the Esla Unit. The formation has been divided into three informal members. Fades analysis suggests that the Panda limestones were deposited in a ramp-like platform, in which subtidal carbonate platform (lower or Cosoya member) and deep platform with mud mounds (upper or Valcarque member) settings can be recognised. Locally, a destructive slope (Casasuertes breccia member) developed. The Panda Formation and the upper part of the underlying Vega cerneja Formation form a depositional sequence recording a deepening upward trend. Also, the platform seems to have developed on an E-W trending arc, which is thought to be due to a blind thrust related to the Esla Unit emplacement
PB Sociedad Geológica de España
YR 2002
FD 2002
LK http://hdl.handle.net/10272/9313
UL http://hdl.handle.net/10272/9313
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026