FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2104314315> ?p ?o ?g. }

• W2104314315 endingPage "759" @default.
• W2104314315 startingPage "742" @default.
• W2104314315 abstract "Abstract Thirty-two heavy-mineral separates, each comprising approximately 2000 grains, were analyzed using the Automatic Geological Scanning Electron Microscope (AutoGeoSEM). This analysis was undertaken to study the influence of depositional environment on the distribution of heavy minerals throughout a regressive Pliocene coastal sequence. The majority of these heavy minerals were separated from the Loxton-Parilla sands, the host of the Bondi Main heavy-mineral beach placer deposit in the Murray Basin of southeastern Australia. The remaining heavy minerals were separated from a number of other Neogene units encountered at the deposit. The heavy-mineral suite is dominated by stable to ultrastable minerals such as zircon, rutile, and tourmaline, along with ilmenite, various intermediate titanates, and anatase. Sillimanite, andalusite, topaz, chrome spinel/chromite, monazite, and muscovite also occur. These heavy minerals are heterogeneously distributed throughout both the Loxton-Parilla sands and the remaining Neogene units. The main process controlling the heterogeneous distribution of these heavy minerals throughout the Loxton-Parilla sands appears to have been the hydraulic conditions, which are intimately linked with the environment of deposition. Consequently, the dense heavy minerals (density > ~ 3.5 g/cm3) are concentrated in relatively high-energy environments such as the breaker zone and swash zone. The less dense heavy minerals (density < ~ 3.5 g/cm3) are concentrated in the shoaling zone and shelf environments. The erratic distribution of the various heavy minerals in some of the other Neogene units is also apparently due to varying depositional conditions. Postdepositional weathering has altered the heavy-mineral assemblages in all units. Accordingly, some primary minerals, such as ilmenite, appear to have altered to secondary minerals, such as pseudorutile and anatase." @default.
• W2104314315 created "2016-06-24" @default.
• W2104314315 creator A5011320416 @default.
• W2104314315 creator A5014835659 @default.
• W2104314315 creator A5052720027 @default.
• W2104314315 creator A5072221751 @default.
• W2104314315 creator A5090395044 @default.
• W2104314315 date "2005-07-01" @default.
• W2104314315 modified "2023-10-18" @default.
• W2104314315 title "Quantitative Heavy-Mineral Analysis of a Pliocene Beach Placer Deposit in Southeastern Australia Using the AutoGeoSEM" @default.
• W2104314315 cites W1484111562 @default.
• W2104314315 cites W1598406615 @default.
• W2104314315 cites W1843117915 @default.
• W2104314315 cites W1981202614 @default.
• W2104314315 cites W1997252211 @default.
• W2104314315 cites W2043890424 @default.
• W2104314315 cites W2046851180 @default.
• W2104314315 cites W2053879970 @default.
• W2104314315 cites W2074686284 @default.
• W2104314315 cites W2089755508 @default.
• W2104314315 cites W2131647691 @default.
• W2104314315 cites W2142786232 @default.
• W2104314315 cites W2153796480 @default.
• W2104314315 cites W2157444311 @default.
• W2104314315 cites W2167897813 @default.
• W2104314315 cites W2173117288 @default.
• W2104314315 cites W2262186335 @default.
• W2104314315 cites W2327639685 @default.
• W2104314315 cites W2921789969 @default.
• W2104314315 cites W3119352019 @default.
• W2104314315 doi "https://doi.org/10.2110/jsr.2005.060" @default.
• W2104314315 hasPublicationYear "2005" @default.
• W2104314315 type Work @default.
• W2104314315 sameAs 2104314315 @default.
• W2104314315 citedByCount "10" @default.
• W2104314315 countsByYear W21043143152012 @default.
• W2104314315 countsByYear W21043143152013 @default.
• W2104314315 countsByYear W21043143152014 @default.
• W2104314315 countsByYear W21043143152021 @default.
• W2104314315 countsByYear W21043143152023 @default.
• W2104314315 crossrefType "journal-article" @default.
• W2104314315 hasAuthorship W2104314315A5011320416 @default.
• W2104314315 hasAuthorship W2104314315A5014835659 @default.
• W2104314315 hasAuthorship W2104314315A5052720027 @default.
• W2104314315 hasAuthorship W2104314315A5072221751 @default.
• W2104314315 hasAuthorship W2104314315A5090395044 @default.
• W2104314315 hasConcept C127313418 @default.
• W2104314315 hasConcept C145972909 @default.
• W2104314315 hasConcept C16674752 @default.
• W2104314315 hasConcept C17409809 @default.
• W2104314315 hasConcept C191897082 @default.
• W2104314315 hasConcept C192562407 @default.
• W2104314315 hasConcept C2776432453 @default.
• W2104314315 hasConcept C2780049196 @default.
• W2104314315 hasConcept C2781394513 @default.
• W2104314315 hasConcept C43592290 @default.
• W2104314315 hasConceptScore W2104314315C127313418 @default.
• W2104314315 hasConceptScore W2104314315C145972909 @default.
• W2104314315 hasConceptScore W2104314315C16674752 @default.
• W2104314315 hasConceptScore W2104314315C17409809 @default.
• W2104314315 hasConceptScore W2104314315C191897082 @default.
• W2104314315 hasConceptScore W2104314315C192562407 @default.
• W2104314315 hasConceptScore W2104314315C2776432453 @default.
• W2104314315 hasConceptScore W2104314315C2780049196 @default.
• W2104314315 hasConceptScore W2104314315C2781394513 @default.
• W2104314315 hasConceptScore W2104314315C43592290 @default.
• W2104314315 hasIssue "4" @default.
• W2104314315 hasLocation W21043143151 @default.
• W2104314315 hasOpenAccess W2104314315 @default.
• W2104314315 hasPrimaryLocation W21043143151 @default.
• W2104314315 hasRelatedWork W1507323463 @default.
• W2104314315 hasRelatedWork W1993146595 @default.
• W2104314315 hasRelatedWork W1993361411 @default.
• W2104314315 hasRelatedWork W2072043006 @default.
• W2104314315 hasRelatedWork W2252876390 @default.
• W2104314315 hasRelatedWork W2283524457 @default.
• W2104314315 hasRelatedWork W2920983306 @default.
• W2104314315 hasRelatedWork W3039738199 @default.
• W2104314315 hasRelatedWork W4293580930 @default.
• W2104314315 hasRelatedWork W4312853652 @default.
• W2104314315 hasVolume "75" @default.
• W2104314315 isParatext "false" @default.
• W2104314315 isRetracted "false" @default.
• W2104314315 magId "2104314315" @default.
• W2104314315 workType "article" @default.