Matches in SemOpenAlex for { <https://semopenalex.org/work/W2156841402> ?p ?o ?g. }
Showing items 1 to 98 of
98
with 100 items per page.
- W2156841402 endingPage "297" @default.
- W2156841402 startingPage "267" @default.
- W2156841402 abstract "The matrix (< 40 μ) of turbidites forms a possible clue to the density of turbidity currents and the origin of the graywacke matrix. Experiments in a circular flume provide a mechanism to study the relation between composition of suspensions at various speeds and their deposits. There is a close analogy to the lower part of turbidity currents. The lutum content of samples with median diameters greater than 400 or 500 μ is found to correspond to the suspended load of the pore water. The higher value for finer deposits can be recalculated to suspension concentration by use of the “sedimentation factor”. Hence, each turbidite carries, as it were, a sample of its depositing current. The lutum content depends not on the ratio of sand to lutum in the current, as tacitly assumed by many authors, but mainly on the ratio lutum to water, although also influenced by velocity. The average lutum density of coarser recent deep-sea sands is 1-2%. This indicates turbidity currents with 5-10% lutum by weight (density 1.03–1.07). The sand must be added to ascertain the current density. In first approximation turbidity currents tend to have densities at their nose of 1.1–1.2, but higher and much lower values also occur. The maximum original lutum percentage of coarse turbidites is below 10%. Higher values are very scarce and are due to post-depositional mixing, or we are dealing with slides. However, in fine-grained turbidites there is more matrix up to 20% for a median of 100 p. Hence, coarse graded marine graywackes with 20 or more per cent matrix are presumably weakly metamorphic turbidites, that originally held the same modest amount of lutum as recent turbidites of the same grain size. The Trask sorting of the experimental deposits is very good, like the average of natural turbidites. Most cumulative curves of turbidite grain-size analyses on arithmetic probability paper show a characteristic bend in fine sand or silt sizes." @default.
- W2156841402 created "2016-06-24" @default.
- W2156841402 creator A5029539631 @default.
- W2156841402 date "1966-12-01" @default.
- W2156841402 modified "2023-10-16" @default.
- W2156841402 title "MATRIX OF TURBIDITES: EXPERIMENTAL APPROACH" @default.
- W2156841402 cites W129245147 @default.
- W2156841402 cites W1446330235 @default.
- W2156841402 cites W1978543444 @default.
- W2156841402 cites W1997858267 @default.
- W2156841402 cites W1998806015 @default.
- W2156841402 cites W2003083792 @default.
- W2156841402 cites W2022387031 @default.
- W2156841402 cites W2027568591 @default.
- W2156841402 cites W2054284399 @default.
- W2156841402 cites W2065452157 @default.
- W2156841402 cites W2089013720 @default.
- W2156841402 cites W2560277103 @default.
- W2156841402 cites W2784288298 @default.
- W2156841402 cites W4248881934 @default.
- W2156841402 doi "https://doi.org/10.1111/j.1365-3091.1966.tb01295.x" @default.
- W2156841402 hasPublicationYear "1966" @default.
- W2156841402 type Work @default.
- W2156841402 sameAs 2156841402 @default.
- W2156841402 citedByCount "79" @default.
- W2156841402 countsByYear W21568414022012 @default.
- W2156841402 countsByYear W21568414022013 @default.
- W2156841402 countsByYear W21568414022014 @default.
- W2156841402 countsByYear W21568414022015 @default.
- W2156841402 countsByYear W21568414022016 @default.
- W2156841402 countsByYear W21568414022017 @default.
- W2156841402 countsByYear W21568414022018 @default.
- W2156841402 countsByYear W21568414022019 @default.
- W2156841402 countsByYear W21568414022020 @default.
- W2156841402 countsByYear W21568414022023 @default.
- W2156841402 crossrefType "journal-article" @default.
- W2156841402 hasAuthorship W2156841402A5029539631 @default.
- W2156841402 hasConcept C106487976 @default.
- W2156841402 hasConcept C109007969 @default.
- W2156841402 hasConcept C111368507 @default.
- W2156841402 hasConcept C114793014 @default.
- W2156841402 hasConcept C126753816 @default.
- W2156841402 hasConcept C127313418 @default.
- W2156841402 hasConcept C148043351 @default.
- W2156841402 hasConcept C157954998 @default.
- W2156841402 hasConcept C159390177 @default.
- W2156841402 hasConcept C159985019 @default.
- W2156841402 hasConcept C192562407 @default.
- W2156841402 hasConcept C199289684 @default.
- W2156841402 hasConcept C2524010 @default.
- W2156841402 hasConcept C2778320725 @default.
- W2156841402 hasConcept C2816523 @default.
- W2156841402 hasConcept C29941650 @default.
- W2156841402 hasConcept C33923547 @default.
- W2156841402 hasConcept C38349280 @default.
- W2156841402 hasConcept C64016661 @default.
- W2156841402 hasConcept C70004062 @default.
- W2156841402 hasConceptScore W2156841402C106487976 @default.
- W2156841402 hasConceptScore W2156841402C109007969 @default.
- W2156841402 hasConceptScore W2156841402C111368507 @default.
- W2156841402 hasConceptScore W2156841402C114793014 @default.
- W2156841402 hasConceptScore W2156841402C126753816 @default.
- W2156841402 hasConceptScore W2156841402C127313418 @default.
- W2156841402 hasConceptScore W2156841402C148043351 @default.
- W2156841402 hasConceptScore W2156841402C157954998 @default.
- W2156841402 hasConceptScore W2156841402C159390177 @default.
- W2156841402 hasConceptScore W2156841402C159985019 @default.
- W2156841402 hasConceptScore W2156841402C192562407 @default.
- W2156841402 hasConceptScore W2156841402C199289684 @default.
- W2156841402 hasConceptScore W2156841402C2524010 @default.
- W2156841402 hasConceptScore W2156841402C2778320725 @default.
- W2156841402 hasConceptScore W2156841402C2816523 @default.
- W2156841402 hasConceptScore W2156841402C29941650 @default.
- W2156841402 hasConceptScore W2156841402C33923547 @default.
- W2156841402 hasConceptScore W2156841402C38349280 @default.
- W2156841402 hasConceptScore W2156841402C64016661 @default.
- W2156841402 hasConceptScore W2156841402C70004062 @default.
- W2156841402 hasIssue "4" @default.
- W2156841402 hasLocation W21568414021 @default.
- W2156841402 hasOpenAccess W2156841402 @default.
- W2156841402 hasPrimaryLocation W21568414021 @default.
- W2156841402 hasRelatedWork W1502884667 @default.
- W2156841402 hasRelatedWork W2095226357 @default.
- W2156841402 hasRelatedWork W2108744423 @default.
- W2156841402 hasRelatedWork W2239015172 @default.
- W2156841402 hasRelatedWork W2326945182 @default.
- W2156841402 hasRelatedWork W2386036462 @default.
- W2156841402 hasRelatedWork W2768420214 @default.
- W2156841402 hasRelatedWork W2900616946 @default.
- W2156841402 hasRelatedWork W4253501567 @default.
- W2156841402 hasRelatedWork W2741962369 @default.
- W2156841402 hasVolume "7" @default.
- W2156841402 isParatext "false" @default.
- W2156841402 isRetracted "false" @default.
- W2156841402 magId "2156841402" @default.
- W2156841402 workType "article" @default.