FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2044610696> ?p ?o ?g. }

• W2044610696 endingPage "71" @default.
• W2044610696 startingPage "57" @default.
• W2044610696 abstract "Geochemical sampling of groundwater may be an effective tool in exploring for Au deposits in areas of transported overburden. However, to use hydrogeochemistry effectively, we need to understand which elements are useful pathfinders and how their distribution patterns are affected by groundwater flow and geochemistry, especially in areas that have hypersaline groundwater. A hydrogeochemical survey was completed over the strongly Au-endowed St. Ives area of the Eastern Goldfields of Western Australia. Extensive geochemical and hydrogeological data were measured from 80 holes drilled on a kilometre-spaced grid. A numerical model was developed to quantify the groundwater flow regime in the study area. Also, hydrogeological data in combination with the geochemistry of the waters were used to identify a complex flow regime adjacent to Lake Lefroy, a playa lake in the area. Regional brine flows towards the salt lake, evaporation occurs and hypersaline (playa) brines are formed that sink and flow away from Lake Lefroy and beneath the regional brines. Density-driven, convective mixing of these two brines is responsible for forming a zone of brines with transitional compositions located near the edge of Lake Lefroy. Knowledge of the groundwater flow regime was used to interpret the distribution of elements around bedrock Au mineralization. An Au-only groundwater anomaly (>10 ppt, maximum 52 ppt) is located downstream of the Junction Au ore body. No anomaly was identified in deep brines associated with the nearby Argo/Apollo Au ore body; however, shallow regional brines sampled in a previous survey showed elevated Au values overlying and downstream of the mineralization. The lack of elevated Au concentrations in deeper groundwater associated with Argo/Apollo is because the samples collected were hypersaline playa brines sourced from Lake Lefroy that had not flowed over the mineralization. Possible pathfinder elements, such as Sb, Bi and Te, were either present in concentrations too low to detect or showed no spatial pattern related to known mineralization; however, a strong correlation was noted between some of their concentrations and salinity. Evaluation of the groundwater anomalies observed in this study suggests that hydrogeochemical exploration is most effective at a resolution of 0.5–4 km spacing, and does not require fully cased and packed wells, at least in cases where no confined aquifers are intersected in drilling. The results of this study illustrate the importance of understanding groundwater flow regimes in planning and interpreting hydrogeochemical surveys." @default.
• W2044610696 created "2016-06-24" @default.
• W2044610696 creator A5033301986 @default.
• W2044610696 creator A5061572748 @default.
• W2044610696 creator A5072520088 @default.
• W2044610696 date "2003-02-01" @default.
• W2044610696 modified "2023-09-27" @default.
• W2044610696 title "Groundwater flow in playa lake environments: impact on gold and pathfinder element distributions in groundwaters surrounding mesothermal gold deposits, St. Ives area, Eastern Goldfields, Western Australia" @default.
• W2044610696 cites W1964233138 @default.
• W2044610696 cites W1974653212 @default.
• W2044610696 cites W1975320007 @default.
• W2044610696 cites W1980192365 @default.
• W2044610696 cites W2002586309 @default.
• W2044610696 cites W2014891531 @default.
• W2044610696 cites W2035271940 @default.
• W2044610696 cites W2035695555 @default.
• W2044610696 cites W2036959539 @default.
• W2044610696 cites W2040047684 @default.
• W2044610696 cites W2040403446 @default.
• W2044610696 cites W2042522600 @default.
• W2044610696 cites W2057079287 @default.
• W2044610696 cites W2057139065 @default.
• W2044610696 cites W2058832323 @default.
• W2044610696 cites W2066755254 @default.
• W2044610696 cites W2076207391 @default.
• W2044610696 cites W2078507095 @default.
• W2044610696 cites W2079725932 @default.
• W2044610696 cites W2132812062 @default.
• W2044610696 cites W2147690151 @default.
• W2044610696 cites W2150026431 @default.
• W2044610696 cites W2151379975 @default.
• W2044610696 cites W2155022123 @default.
• W2044610696 cites W2315892471 @default.
• W2044610696 cites W2323636345 @default.
• W2044610696 cites W2404597426 @default.
• W2044610696 cites W4236138975 @default.
• W2044610696 cites W4236905269 @default.
• W2044610696 doi "https://doi.org/10.1144/1467-787302-045" @default.
• W2044610696 hasPublicationYear "2003" @default.
• W2044610696 type Work @default.
• W2044610696 sameAs 2044610696 @default.
• W2044610696 citedByCount "16" @default.
• W2044610696 countsByYear W20446106962013 @default.
• W2044610696 countsByYear W20446106962017 @default.
• W2044610696 countsByYear W20446106962018 @default.
• W2044610696 countsByYear W20446106962019 @default.
• W2044610696 countsByYear W20446106962021 @default.
• W2044610696 countsByYear W20446106962022 @default.
• W2044610696 countsByYear W20446106962023 @default.
• W2044610696 crossrefType "journal-article" @default.
• W2044610696 hasAuthorship W2044610696A5033301986 @default.
• W2044610696 hasAuthorship W2044610696A5061572748 @default.
• W2044610696 hasAuthorship W2044610696A5072520088 @default.
• W2044610696 hasConcept C127313418 @default.
• W2044610696 hasConcept C131227075 @default.
• W2044610696 hasConcept C151730666 @default.
• W2044610696 hasConcept C156622251 @default.
• W2044610696 hasConcept C159055055 @default.
• W2044610696 hasConcept C161191863 @default.
• W2044610696 hasConcept C166957645 @default.
• W2044610696 hasConcept C187320778 @default.
• W2044610696 hasConcept C205649164 @default.
• W2044610696 hasConcept C2776152364 @default.
• W2044610696 hasConcept C2778940482 @default.
• W2044610696 hasConcept C41008148 @default.
• W2044610696 hasConcept C75622301 @default.
• W2044610696 hasConcept C76177295 @default.
• W2044610696 hasConcept C76886044 @default.
• W2044610696 hasConceptScore W2044610696C127313418 @default.
• W2044610696 hasConceptScore W2044610696C131227075 @default.
• W2044610696 hasConceptScore W2044610696C151730666 @default.
• W2044610696 hasConceptScore W2044610696C156622251 @default.
• W2044610696 hasConceptScore W2044610696C159055055 @default.
• W2044610696 hasConceptScore W2044610696C161191863 @default.
• W2044610696 hasConceptScore W2044610696C166957645 @default.
• W2044610696 hasConceptScore W2044610696C187320778 @default.
• W2044610696 hasConceptScore W2044610696C205649164 @default.
• W2044610696 hasConceptScore W2044610696C2776152364 @default.
• W2044610696 hasConceptScore W2044610696C2778940482 @default.
• W2044610696 hasConceptScore W2044610696C41008148 @default.
• W2044610696 hasConceptScore W2044610696C75622301 @default.
• W2044610696 hasConceptScore W2044610696C76177295 @default.
• W2044610696 hasConceptScore W2044610696C76886044 @default.
• W2044610696 hasIssue "1" @default.
• W2044610696 hasLocation W20446106961 @default.
• W2044610696 hasOpenAccess W2044610696 @default.
• W2044610696 hasPrimaryLocation W20446106961 @default.
• W2044610696 hasRelatedWork W1267230520 @default.
• W2044610696 hasRelatedWork W126960246 @default.
• W2044610696 hasRelatedWork W1974058957 @default.
• W2044610696 hasRelatedWork W2051969510 @default.
• W2044610696 hasRelatedWork W2357547782 @default.
• W2044610696 hasRelatedWork W2775390275 @default.
• W2044610696 hasRelatedWork W2802620913 @default.
• W2044610696 hasRelatedWork W2889484933 @default.
• W2044610696 hasRelatedWork W4225388847 @default.
• W2044610696 hasRelatedWork W2909715836 @default.
• W2044610696 hasVolume "3" @default.

• next