@article{fdi:010023227,
  title = {{F}acies y ambientes sedimentarios de la {F}ormacion {C}ancaniri ({S}ilurico inferior) en la cumbre de {L}a {P}az, norte de la {C}ordillera {O}riental de {B}olivia},
  author = {{D}iaz {M}artinez, {E}nrique},
  editor = {},
  language = {{SPA}},
  abstract = {{F}acies analysis of a continuous outcrop of the {C}ancañiri {F}ormation (latest {A}shgillian-{L}landoverina) at {L}a {C}umbre ({NE} of {L}a {P}az, {B}olivia) allowed for a thorough interpretation of sedimentary processes and environments envolved during its deposition. {D}istal 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. {O}utsized granite clasts indicate local glaciation of the source area. {T}ectonic deformation and the resulting reliefs may be identified as the origin for the instability and local glaciation, respectively ({R}{\'e}sum{\'e} d'auteur).},
  keywords = {{SEDIMENTATION} {MARINE} ; {SEDIMENTOLOGIE} ; {ORDOVICIEN} ; {FACIES} ; {TECTONIQUE} ; {OROGENESE} ; {SILURIEN} ; {BOLIVIE} ; {ANDES}},
  booktitle = {},
  journal = {{G}eogaceta (},
  numero = {22},
  pages = {55--57},
  ISSN = {0213-683{X}},
  year = {1997},
  URL = {https://www.documentation.ird.fr/hor/fdi:010023227},
}