Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006020120> ?p ?o ?g. }
Showing items 1 to 88 of
88
with 100 items per page.
- W2006020120 endingPage "678" @default.
- W2006020120 startingPage "659" @default.
- W2006020120 abstract "The Rio Grande Rift and the Salton Trough are the best developed rift systems in the United States and both share many features common to rifts in general, including geothermal resources. These two rifts have different tectonic and magmatic histories, however, and these differences are reflected in the nature of their geothermal resources. The Salton Trough is a well developed and successful rift. It is the landward extension of the Gulf of California spreading center, which has separated Baja, California, from the remainder of Mexico. Quaternary silicic magmatization has occurred and several of the geothermal resources are associated with recent rhyolitic intrusions. Such resources tend to be high temperature (> 200°C). Greenschist facies metamorphism has been observed in several of the geothermal wells. Localized upper crustal melting is a distinct possibility and there is increasing speculation that very high temperature (> 300°C) geothermal fluids may underlie a large portion of the central trough at depths in excess of 4 km. Low temperature geothermal resources associated with shallow hydrothermal convection are less common and tend to be located on the flanks of the trough or in the Coachella Valley to the north of the zone of active rifting. In contrast, the Rio Grande Rift is less well developed. Recent volcanism consists primarily of mantle-derived basalts, which have not had sufficient residence time within the crust to generate significant crustal melting. The geothermal resources within the Rio Grande Rift do not correlate well with these young basalts. Rather, the quantity of geothermal resources are low temperature (< 100°C) and result from forced hydrothermal convection which discharges at constrictions within or at the end of the major sedimentary basins. High temperature resources are less common and the only discovered example is the Valles Caldera of northern New Mexico (T = 250–300°C). The deep interiors of the sedimentary basins of the Rio Grande Rift do not appear to be major geothermal exploration targets." @default.
- W2006020120 created "2016-06-24" @default.
- W2006020120 creator A5013364548 @default.
- W2006020120 date "1983-05-01" @default.
- W2006020120 modified "2023-10-18" @default.
- W2006020120 title "Geothermal resources of rifts: A comparison of the rio grande rift and the salton trough" @default.
- W2006020120 cites W126241347 @default.
- W2006020120 cites W1483093968 @default.
- W2006020120 cites W154529801 @default.
- W2006020120 cites W1545567492 @default.
- W2006020120 cites W1547934844 @default.
- W2006020120 cites W1570499846 @default.
- W2006020120 cites W1575435123 @default.
- W2006020120 cites W1677257252 @default.
- W2006020120 cites W2030511518 @default.
- W2006020120 cites W2033580029 @default.
- W2006020120 cites W2120746470 @default.
- W2006020120 cites W2334266388 @default.
- W2006020120 cites W2339506802 @default.
- W2006020120 cites W592197537 @default.
- W2006020120 doi "https://doi.org/10.1016/0040-1951(83)90039-2" @default.
- W2006020120 hasPublicationYear "1983" @default.
- W2006020120 type Work @default.
- W2006020120 sameAs 2006020120 @default.
- W2006020120 citedByCount "16" @default.
- W2006020120 crossrefType "journal-article" @default.
- W2006020120 hasAuthorship W2006020120A5013364548 @default.
- W2006020120 hasConcept C104962623 @default.
- W2006020120 hasConcept C111766609 @default.
- W2006020120 hasConcept C120806208 @default.
- W2006020120 hasConcept C127313418 @default.
- W2006020120 hasConcept C139719470 @default.
- W2006020120 hasConcept C151730666 @default.
- W2006020120 hasConcept C161509811 @default.
- W2006020120 hasConcept C162324750 @default.
- W2006020120 hasConcept C165205528 @default.
- W2006020120 hasConcept C17409809 @default.
- W2006020120 hasConcept C192241223 @default.
- W2006020120 hasConcept C25822816 @default.
- W2006020120 hasConcept C2776698055 @default.
- W2006020120 hasConcept C2778471503 @default.
- W2006020120 hasConcept C2778697265 @default.
- W2006020120 hasConcept C32239851 @default.
- W2006020120 hasConcept C50682988 @default.
- W2006020120 hasConcept C5900021 @default.
- W2006020120 hasConcept C6363049 @default.
- W2006020120 hasConcept C77928131 @default.
- W2006020120 hasConceptScore W2006020120C104962623 @default.
- W2006020120 hasConceptScore W2006020120C111766609 @default.
- W2006020120 hasConceptScore W2006020120C120806208 @default.
- W2006020120 hasConceptScore W2006020120C127313418 @default.
- W2006020120 hasConceptScore W2006020120C139719470 @default.
- W2006020120 hasConceptScore W2006020120C151730666 @default.
- W2006020120 hasConceptScore W2006020120C161509811 @default.
- W2006020120 hasConceptScore W2006020120C162324750 @default.
- W2006020120 hasConceptScore W2006020120C165205528 @default.
- W2006020120 hasConceptScore W2006020120C17409809 @default.
- W2006020120 hasConceptScore W2006020120C192241223 @default.
- W2006020120 hasConceptScore W2006020120C25822816 @default.
- W2006020120 hasConceptScore W2006020120C2776698055 @default.
- W2006020120 hasConceptScore W2006020120C2778471503 @default.
- W2006020120 hasConceptScore W2006020120C2778697265 @default.
- W2006020120 hasConceptScore W2006020120C32239851 @default.
- W2006020120 hasConceptScore W2006020120C50682988 @default.
- W2006020120 hasConceptScore W2006020120C5900021 @default.
- W2006020120 hasConceptScore W2006020120C6363049 @default.
- W2006020120 hasConceptScore W2006020120C77928131 @default.
- W2006020120 hasIssue "1-4" @default.
- W2006020120 hasLocation W20060201201 @default.
- W2006020120 hasOpenAccess W2006020120 @default.
- W2006020120 hasPrimaryLocation W20060201201 @default.
- W2006020120 hasRelatedWork W1986578617 @default.
- W2006020120 hasRelatedWork W2006020120 @default.
- W2006020120 hasRelatedWork W2019021775 @default.
- W2006020120 hasRelatedWork W2064145068 @default.
- W2006020120 hasRelatedWork W2092119312 @default.
- W2006020120 hasRelatedWork W2156877751 @default.
- W2006020120 hasRelatedWork W2493384121 @default.
- W2006020120 hasRelatedWork W2885906625 @default.
- W2006020120 hasRelatedWork W3041234357 @default.
- W2006020120 hasRelatedWork W4206399890 @default.
- W2006020120 hasVolume "94" @default.
- W2006020120 isParatext "false" @default.
- W2006020120 isRetracted "false" @default.
- W2006020120 magId "2006020120" @default.
- W2006020120 workType "article" @default.