Titre de série :	US Geological Survey Water-Supply Paper, 2326 -B
Titre :	Sedimentary structures and textures of Rio Orinocom channel sands, Venezuela and Colombia
Type de document :	texte imprimé
Auteurs :	Kee, E. D.
Mention d'édition :	US Geological survey
Editeur :	US Geological Survey
Année de publication :	1989
ISBN/ISSN/EAN :	CI-04250
Note générale :	Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...
Langues :	Anglais (eng)
Mots-clés :	Sédimentation  Hydrologie fluviale  Terminologie
Index. décimale :	551.48 Hydrologie :
Résumé :	Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...
Note de contenu :	Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...

US Geological Survey Water-Supply Paper, 2326 -B. Sedimentary structures and textures of Rio Orinocom channel sands, Venezuela and Colombia [texte imprimé] / Kee, E. D.  . -  US Geological survey . - US Geological Survey, 1989.
ISSN : CI-04250
Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...
Langues : Anglais (eng)

Mots-clés :	Sédimentation  Hydrologie fluviale  Terminologie
Index. décimale :	551.48 Hydrologie :
Résumé :	Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...
Note de contenu :	Most sedimentary structures represented in sand bodies of the Rio Orinoco are tabular-planar cross-strata which, together with some wedge-planar cross-strata, are the products of sand-wave deposition. Locally, in areas of river meander where point bars characteristically from, through structures forming festoon patterns are numerous. At a few localities, sets of nearly horizontal strata occur between babular-planar sets and are interpreted to be the deposits of very fast currents of the upper flow regime/ elswhere/ ...