RT Journal Article
T1 La glaciación del límite Ordovícico-Silúrico en el Altiplano de Perú: evidencias e implicaciones tectónicas
T1 Latest Ordovician-Early Silurian glaciation in the Peruvian Altiplano: evidence and tectonic implications
A1 Díaz Martínez, Enrique
A1 Acosta, H.
A1 Rodríguez, R.
A1 Carlotto, V.
A1 Cárdenas, J.
AB The Lower Paleozoic strati graphic sequence cropping out immediately to the north of Ayaviri (Peruvian Altiplano) belongs to the Eastern Cordillera tectonostratigraphic domain, and includes the Sandia, San Gabán and Ananea formations. Clacially-striated and faceted clasts found within the diamictites of the San Gabán Formation provide the first evidence for the late Ashgill-Llandovery glaciation in the Peruvian Altiplano, an area where this unit was previously considered not to be deposited. The marked difference between the Lower Paleozoic sequences of the Altiplano and Eastern Cordillera tectonostratigraphic domains suggests important tectonic shortening along the boundary fault zone
PB Sociedad Geológica de España
YR 1999
FD 1999
LK http://hdl.handle.net/10272/10091
UL http://hdl.handle.net/10272/10091
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026