FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1515076096> ?p ?o ?g. }

• W1515076096 abstract "The southwestern part of the Challis volcanic field occupies the valley of the Little Wood River and its tributaries in the Hailey and Idaho Falls 1??2? quadrangles of south-central Idaho. The Little Wood River area is a structurally controlled topographic basin that is partly filled by Eocene Challis Volcanic Group and younger rocks. Rock types in the Challis Volcanic Group of the Little Wood River area include, in order of decreasing abundance, andesite lava flows and tuff breccia, dacite lava flows and flow breccia, volcaniclastic sedimentary rocks, lithic tuff, nonvolcanic conglomerate, and rhyolite dikes. A basal nonvolcanic conglomerate, that locally rests on upper Paleozoic sedimentary rocks at a regional unconformity, was deposited prior to eruption of volcanic rocks. Andesite was the first volcanic rock erupted and is a voluminous sequence as thick as 3,000 ft (1,000 m). Locally thick volcaniclastic sedimentary rocks accumulated in topographic lows. A sharp transition marks the beginning of dacite eruption from fissures and flow-dome complexes. Dacite flows and breccias are as thick as 2,000 ft (600 m). An upper volcaniclastic unit was deposited in paleotopographic lows following emplacement of the main dacite unit. Next, a widespread, distinctive, lithic rich ash flow tuff, correlated with the tuff of Stoddard Gulch, was deposited over much of the area. Deposition of the tuff was followed by eruption of thin andesite and dacite lava flows and deposition of conglomeratic sedimentary rocks. The entire sequence was then intruded by a dacite flow-dome complex composed of at least three separate intrusions. The Challis Volcanic Group in the study area is calcalkaline. Andesitic rocks are typically high potassium basaltic andesite, high potassium andesite, shoshonite, and banakite (latite). Dacitic rocks are high potassium dacite and trachyte. Tuffs and vitrophyres range in composition from basaltic andesite to trachyte. The paleotopographic basin in which the Challis Volcanic Group accumulated was in part structurally controlled by preexisting west and northwest trending normal faults. Paleorelief was probably more than 2,000 ft (600 m). Rocks of the Challis Volcanic Group typically dip about 36? E., probably owing to Eocene extension and (or)basin-and-range faulting and tilting. Some potential forprecious and base metal hydrothermal deposits isassociated with northeast trending lineaments, argillicalteration, and rhyolite dikes." @default.
• W1515076096 created "2016-06-24" @default.
• W1515076096 creator A5019831015 @default.
• W1515076096 creator A5087817219 @default.
• W1515076096 date "2005-01-01" @default.
• W1515076096 modified "2023-09-27" @default.
• W1515076096 title "Geology and stratigraphy of the Challis Volcanic Group and related rocks, Little Wood River area, south-central Idaho" @default.
• W1515076096 cites W1506015560 @default.
• W1515076096 cites W1524976375 @default.
• W1515076096 cites W1557201645 @default.
• W1515076096 cites W1586071180 @default.
• W1515076096 cites W186912107 @default.
• W1515076096 cites W188968803 @default.
• W1515076096 cites W1966819178 @default.
• W1515076096 cites W1971572144 @default.
• W1515076096 cites W1979350315 @default.
• W1515076096 cites W1991887373 @default.
• W1515076096 cites W1991964389 @default.
• W1515076096 cites W2010028923 @default.
• W1515076096 cites W2013501420 @default.
• W1515076096 cites W2041681251 @default.
• W1515076096 cites W2048266370 @default.
• W1515076096 cites W2051955054 @default.
• W1515076096 cites W2053442410 @default.
• W1515076096 cites W2053573746 @default.
• W1515076096 cites W2065490300 @default.
• W1515076096 cites W2076543693 @default.
• W1515076096 cites W2081673195 @default.
• W1515076096 cites W2084475519 @default.
• W1515076096 cites W2087888055 @default.
• W1515076096 cites W2089317477 @default.
• W1515076096 cites W2107006157 @default.
• W1515076096 cites W2108641227 @default.
• W1515076096 cites W2129952316 @default.
• W1515076096 cites W2130945854 @default.
• W1515076096 cites W2224833853 @default.
• W1515076096 cites W616560559 @default.
• W1515076096 cites W6183916 @default.
• W1515076096 cites W84604607 @default.
• W1515076096 cites W991100066 @default.
• W1515076096 doi "https://doi.org/10.3133/b2064ii" @default.
• W1515076096 hasPublicationYear "2005" @default.
• W1515076096 type Work @default.
• W1515076096 sameAs 1515076096 @default.
• W1515076096 citedByCount "4" @default.
• W1515076096 crossrefType "report" @default.
• W1515076096 hasAuthorship W1515076096A5019831015 @default.
• W1515076096 hasAuthorship W1515076096A5087817219 @default.
• W1515076096 hasConcept C106804226 @default.
• W1515076096 hasConcept C107504934 @default.
• W1515076096 hasConcept C113754120 @default.
• W1515076096 hasConcept C114793014 @default.
• W1515076096 hasConcept C120806208 @default.
• W1515076096 hasConcept C127313418 @default.
• W1515076096 hasConcept C138170599 @default.
• W1515076096 hasConcept C17409809 @default.
• W1515076096 hasConcept C192241223 @default.
• W1515076096 hasConcept C24343810 @default.
• W1515076096 hasConcept C25822816 @default.
• W1515076096 hasConcept C36986328 @default.
• W1515076096 hasConcept C5900021 @default.
• W1515076096 hasConcept C62074269 @default.
• W1515076096 hasConcept C6494504 @default.
• W1515076096 hasConcept C95869378 @default.
• W1515076096 hasConceptScore W1515076096C106804226 @default.
• W1515076096 hasConceptScore W1515076096C107504934 @default.
• W1515076096 hasConceptScore W1515076096C113754120 @default.
• W1515076096 hasConceptScore W1515076096C114793014 @default.
• W1515076096 hasConceptScore W1515076096C120806208 @default.
• W1515076096 hasConceptScore W1515076096C127313418 @default.
• W1515076096 hasConceptScore W1515076096C138170599 @default.
• W1515076096 hasConceptScore W1515076096C17409809 @default.
• W1515076096 hasConceptScore W1515076096C192241223 @default.
• W1515076096 hasConceptScore W1515076096C24343810 @default.
• W1515076096 hasConceptScore W1515076096C25822816 @default.
• W1515076096 hasConceptScore W1515076096C36986328 @default.
• W1515076096 hasConceptScore W1515076096C5900021 @default.
• W1515076096 hasConceptScore W1515076096C62074269 @default.
• W1515076096 hasConceptScore W1515076096C6494504 @default.
• W1515076096 hasConceptScore W1515076096C95869378 @default.
• W1515076096 hasLocation W15150760961 @default.
• W1515076096 hasOpenAccess W1515076096 @default.
• W1515076096 hasPrimaryLocation W15150760961 @default.
• W1515076096 hasRelatedWork W1491073723 @default.
• W1515076096 hasRelatedWork W1492294012 @default.
• W1515076096 hasRelatedWork W1515076096 @default.
• W1515076096 hasRelatedWork W2035268287 @default.
• W1515076096 hasRelatedWork W2066751852 @default.
• W1515076096 hasRelatedWork W2080245506 @default.
• W1515076096 hasRelatedWork W2156068745 @default.
• W1515076096 hasRelatedWork W2336169866 @default.
• W1515076096 hasRelatedWork W2356925304 @default.
• W1515076096 hasRelatedWork W3011672864 @default.
• W1515076096 isParatext "false" @default.
• W1515076096 isRetracted "false" @default.
• W1515076096 magId "1515076096" @default.
• W1515076096 workType "report" @default.