RT Journal Article
T1 Facies y ambientes sedimentarios de la Formación Cancañiri (Silúrico inferior) en La Cumbre de La Paz, norte de la Cordillera Oriental de Bolivia
T1 Facies and sedimentary environments of the Cancañiri Formation (Lower Silurian) at La Cumbre of La Paz, northern Eastern Cordillera of Bolivia
A1 Díaz Martínez, Enrique
AB Fades analysis of a continuous outcrop of the Cancaniri Formation (latest Ashgillian-Llandoverian) at La Cumbre (I<IE of La Paz, Bolivia) allowed for a thorough interpretation of sedimentary 'processes and environments envolved during its deposition. Distal turbidites and dark shales indicate a deep marine (offshore) environment, whereas interbedded mud flows, debris flows and deformed slided slabs provide evidence for sediment instability and resedimentation. Outsized granite clasts indicate local glaciation of the source area. Tectonic deformation and the resulting: reliefs may be identified, as the . origin for the instability and local glaciation, respectively
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10558
UL http://hdl.handle.net/10272/10558
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026