FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W236017434> ?p ?o ?g. }

• W236017434 abstract "Numerous hot springs occur in a variety of geologic provinces in central and western Alaska. Granitic plutons are common to all the provinces and the hot springs are spatially associated with the contacts of these plutons. Of 23 hot springs whose bedrock geology is known, all occur within 3 miles of a granitic pluton. Preliminary chemical and isotopic analyses suggest the hot springs waters below to two groups. Most of the analyzed hot springs appear to have chemical and isotopic compositions indicating they were derived from deeply circulating meteoric water. About 25 percent of the analyzed hot springs show a distinct saline character with high concentrations of chloride, sodium, potassium, and calcium indicating either much more complex water-rock reactions than occurred in the other hot springs or the addition of another type of water. The present chemical and isotopic data are insufficient to determine the source of the constituents of the saline hot springs. Chemical geothermometers suggest subsurface temperatures in the general range of 100/sup 0/C to 160/sup 0/C. If the hot spring waters have derived their heat solely from deep circulation, the waters must have reached depths of 9,000 to 15,000 feet, assuming geothermal gradients of 30/sup 0/C tomore » 50/sup 0/C/km. If hot magmatic water has been added to the geothermal systems or if dilution or mixing has occurred, temperatures of 100/sup 0/C to 160/sup 0/Cmay be reached at shallower depths. The geologic and chemical data are too preliminary to make an estimate of the potential of the hot springs as a geothermal resource. The data suggest, however, that most of the hot springs of central and western Alaska have relatively low subsurface temperatures and limited reservoir capacities in comparison with geothermal areas presently being utilized for electrical power generation.« less" @default.
• W236017434 created "2016-06-24" @default.
• W236017434 creator A5009883349 @default.
• W236017434 creator A5038672329 @default.
• W236017434 creator A5073799377 @default.
• W236017434 date "1973-01-01" @default.
• W236017434 modified "2023-09-27" @default.
• W236017434 title "Geologic setting and chemical characteristics of hot springs in central and western Alaska. [Subsurface temperature of 100/sup 0/C to 160/sup 0/C]" @default.
• W236017434 hasPublicationYear "1973" @default.
• W236017434 type Work @default.
• W236017434 sameAs 236017434 @default.
• W236017434 citedByCount "0" @default.
• W236017434 crossrefType "journal-article" @default.
• W236017434 hasAuthorship W236017434A5009883349 @default.
• W236017434 hasAuthorship W236017434A5038672329 @default.
• W236017434 hasAuthorship W236017434A5073799377 @default.
• W236017434 hasConcept C111766609 @default.
• W236017434 hasConcept C127313418 @default.
• W236017434 hasConcept C127413603 @default.
• W236017434 hasConcept C149849071 @default.
• W236017434 hasConcept C151730666 @default.
• W236017434 hasConcept C17409809 @default.
• W236017434 hasConcept C178790620 @default.
• W236017434 hasConcept C185592680 @default.
• W236017434 hasConcept C187320778 @default.
• W236017434 hasConcept C199289684 @default.
• W236017434 hasConcept C2778131859 @default.
• W236017434 hasConcept C2778712887 @default.
• W236017434 hasConcept C34122518 @default.
• W236017434 hasConcept C76177295 @default.
• W236017434 hasConcept C76886044 @default.
• W236017434 hasConcept C77928131 @default.
• W236017434 hasConcept C78519656 @default.
• W236017434 hasConcept C8058405 @default.
• W236017434 hasConcept C92720285 @default.
• W236017434 hasConceptScore W236017434C111766609 @default.
• W236017434 hasConceptScore W236017434C127313418 @default.
• W236017434 hasConceptScore W236017434C127413603 @default.
• W236017434 hasConceptScore W236017434C149849071 @default.
• W236017434 hasConceptScore W236017434C151730666 @default.
• W236017434 hasConceptScore W236017434C17409809 @default.
• W236017434 hasConceptScore W236017434C178790620 @default.
• W236017434 hasConceptScore W236017434C185592680 @default.
• W236017434 hasConceptScore W236017434C187320778 @default.
• W236017434 hasConceptScore W236017434C199289684 @default.
• W236017434 hasConceptScore W236017434C2778131859 @default.
• W236017434 hasConceptScore W236017434C2778712887 @default.
• W236017434 hasConceptScore W236017434C34122518 @default.
• W236017434 hasConceptScore W236017434C76177295 @default.
• W236017434 hasConceptScore W236017434C76886044 @default.
• W236017434 hasConceptScore W236017434C77928131 @default.
• W236017434 hasConceptScore W236017434C78519656 @default.
• W236017434 hasConceptScore W236017434C8058405 @default.
• W236017434 hasConceptScore W236017434C92720285 @default.
• W236017434 hasLocation W2360174341 @default.
• W236017434 hasOpenAccess W236017434 @default.
• W236017434 hasPrimaryLocation W2360174341 @default.
• W236017434 hasRelatedWork W1363915 @default.
• W236017434 hasRelatedWork W1526100701 @default.
• W236017434 hasRelatedWork W1590060292 @default.
• W236017434 hasRelatedWork W1591297333 @default.
• W236017434 hasRelatedWork W1621958716 @default.
• W236017434 hasRelatedWork W1981249056 @default.
• W236017434 hasRelatedWork W1983429848 @default.
• W236017434 hasRelatedWork W1990543954 @default.
• W236017434 hasRelatedWork W1994093489 @default.
• W236017434 hasRelatedWork W2021039407 @default.
• W236017434 hasRelatedWork W2074920451 @default.
• W236017434 hasRelatedWork W2299918138 @default.
• W236017434 hasRelatedWork W2802342122 @default.
• W236017434 hasRelatedWork W2917394878 @default.
• W236017434 hasRelatedWork W2923984281 @default.
• W236017434 hasRelatedWork W2962578234 @default.
• W236017434 hasRelatedWork W3169552776 @default.
• W236017434 hasRelatedWork W3206422223 @default.
• W236017434 hasRelatedWork W91977908 @default.
• W236017434 hasRelatedWork W2338861751 @default.
• W236017434 isParatext "false" @default.
• W236017434 isRetracted "false" @default.
• W236017434 magId "236017434" @default.
• W236017434 workType "article" @default.