FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2113261711> ?p ?o ?g. }

• W2113261711 endingPage "328" @default.
• W2113261711 startingPage "316" @default.
• W2113261711 abstract "Research Article| March 01, 1992 Origin and chemical evolution of the 1360 Ma San Isabel batholith, Wet Mountains, Colorado: A mid-crustal granite of anorogenic affinities ROBERT L. CULLERS; ROBERT L. CULLERS 1Department of Geology, Kansas State University, Manhattan, Kansas 66506 Search for other works by this author on: GSW Google Scholar TOM GRIFFIN; TOM GRIFFIN 1Department of Geology, Kansas State University, Manhattan, Kansas 66506 Search for other works by this author on: GSW Google Scholar M. E. BICKFORD; M. E. BICKFORD 2Department of Geology, University of Kansas, Lawrence, Kansas 66045 Search for other works by this author on: GSW Google Scholar J. LAWFORD ANDERSON J. LAWFORD ANDERSON 3Department of Geological Sciences, University of Southern California, Los Angeles, California 90089-0740 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1992) 104 (3): 316–328. https://doi.org/10.1130/0016-7606(1992)104<0316:OACEOT>2.3.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation ROBERT L. CULLERS, TOM GRIFFIN, M. E. BICKFORD, J. LAWFORD ANDERSON; Origin and chemical evolution of the 1360 Ma San Isabel batholith, Wet Mountains, Colorado: A mid-crustal granite of anorogenic affinities. GSA Bulletin 1992;; 104 (3): 316–328. doi: https://doi.org/10.1130/0016-7606(1992)104<0316:OACEOT>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The 1360 Ma San Isabel batholith is a weakly foliated hornblende-biotite-sphene monzogranite consisting predominantly of two variants: a coarse-grained facies and a medium-grained equigranular facies. It is a deeper-seated portion (mid-crustal; 5-7 kbar) of the extensive rhyolite and upper-crustal granite terrane that occurs in parts of Missouri, Oklahoma, Kansas, and Texas. Mafic minerals are abundant, variable in amount (to as high as 35%) and segregated into mafic-enriched zones.The San Isabel magma probably formed in an anorogenic setting, as suggested by (1) high total alkali and high FeO/(FeO + MgO) ratios, (2) relatively dry nature, (3) trace-element plots in tectonic discrimination diagrams, (4) similar composition of its leucogranite differentiates to shallower A-type granites, and (5) contemporaneity with other A-type granites.Compared to many granitic plutons, the batholith contains small, negative Eu anomalies, low SiO2 (56.1-72.0 wt%), moderate Sr, and high Fe, Ti, K, Mn, Ba, Sc, REE's, and FeO/(FeO + MgO). There are large and fairly linear ranges in the abundances of elements concentrated in mafic minerals (for example, Fe, Ti, Mg, and Ca) and smaller ranges (more scatter) in elements concentrated in the felsic minerals (for example, Eu anomaly size and Ba). The San Isabel magma is thus distinctly mafic in comparison with shallow A-type magmas.The San Isabel magma could have formed by >20% aggregate melting of a tonalite/andesite or by <10% melting of a calc-alkaline basalt. Mixing of the melts derived from the two sources might best explain the relatively low silica and high mafic-mineral content of the monzogranite. Accumulation or crystallization of the observed minerals from the magma could have produced the compositional variations in the batholith. The most silica-rich portions of the San Isabel are similar in composition to classic, shallower A-type granites. Thus, this may be one way in which the shallower and silica-rich A-type granites have formed. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2113261711 created "2016-06-24" @default.
• W2113261711 creator A5018137707 @default.
• W2113261711 creator A5026638700 @default.
• W2113261711 creator A5073107002 @default.
• W2113261711 creator A5081380902 @default.
• W2113261711 date "1992-03-01" @default.
• W2113261711 modified "2023-09-25" @default.
• W2113261711 title "Origin and chemical evolution of the 1360 Ma San Isabel batholith, Wet Mountains, Colorado: A mid-crustal granite of anorogenic affinities" @default.
• W2113261711 doi "https://doi.org/10.1130/0016-7606(1992)104<0316:oaceot>2.3.co;2" @default.
• W2113261711 hasPublicationYear "1992" @default.
• W2113261711 type Work @default.
• W2113261711 sameAs 2113261711 @default.
• W2113261711 citedByCount "33" @default.
• W2113261711 countsByYear W21132617112012 @default.
• W2113261711 countsByYear W21132617112013 @default.
• W2113261711 countsByYear W21132617112015 @default.
• W2113261711 countsByYear W21132617112017 @default.
• W2113261711 countsByYear W21132617112018 @default.
• W2113261711 countsByYear W21132617112019 @default.
• W2113261711 countsByYear W21132617112022 @default.
• W2113261711 countsByYear W21132617112023 @default.
• W2113261711 crossrefType "journal-article" @default.
• W2113261711 hasAuthorship W2113261711A5018137707 @default.
• W2113261711 hasAuthorship W2113261711A5026638700 @default.
• W2113261711 hasAuthorship W2113261711A5073107002 @default.
• W2113261711 hasAuthorship W2113261711A5081380902 @default.
• W2113261711 hasConcept C127313418 @default.
• W2113261711 hasConcept C151730666 @default.
• W2113261711 hasConcept C161191863 @default.
• W2113261711 hasConcept C166957645 @default.
• W2113261711 hasConcept C172660882 @default.
• W2113261711 hasConcept C199360897 @default.
• W2113261711 hasConcept C2775969163 @default.
• W2113261711 hasConcept C2778447006 @default.
• W2113261711 hasConcept C2778805511 @default.
• W2113261711 hasConcept C41008148 @default.
• W2113261711 hasConcept C77928131 @default.
• W2113261711 hasConcept C95457728 @default.
• W2113261711 hasConceptScore W2113261711C127313418 @default.
• W2113261711 hasConceptScore W2113261711C151730666 @default.
• W2113261711 hasConceptScore W2113261711C161191863 @default.
• W2113261711 hasConceptScore W2113261711C166957645 @default.
• W2113261711 hasConceptScore W2113261711C172660882 @default.
• W2113261711 hasConceptScore W2113261711C199360897 @default.
• W2113261711 hasConceptScore W2113261711C2775969163 @default.
• W2113261711 hasConceptScore W2113261711C2778447006 @default.
• W2113261711 hasConceptScore W2113261711C2778805511 @default.
• W2113261711 hasConceptScore W2113261711C41008148 @default.
• W2113261711 hasConceptScore W2113261711C77928131 @default.
• W2113261711 hasConceptScore W2113261711C95457728 @default.
• W2113261711 hasIssue "3" @default.
• W2113261711 hasLocation W21132617111 @default.
• W2113261711 hasOpenAccess W2113261711 @default.
• W2113261711 hasPrimaryLocation W21132617111 @default.
• W2113261711 hasRelatedWork W2007662642 @default.
• W2113261711 hasRelatedWork W2017250477 @default.
• W2113261711 hasRelatedWork W2033475216 @default.
• W2113261711 hasRelatedWork W2038530868 @default.
• W2113261711 hasRelatedWork W2057655526 @default.
• W2113261711 hasRelatedWork W2059015916 @default.
• W2113261711 hasRelatedWork W2745843255 @default.
• W2113261711 hasRelatedWork W4221134017 @default.
• W2113261711 hasRelatedWork W4302332348 @default.
• W2113261711 hasRelatedWork W4380320271 @default.
• W2113261711 hasVolume "104" @default.
• W2113261711 isParatext "false" @default.
• W2113261711 isRetracted "false" @default.
• W2113261711 magId "2113261711" @default.
• W2113261711 workType "article" @default.