FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2145882925> ?p ?o ?g. }

• W2145882925 endingPage "771" @default.
• W2145882925 startingPage "749" @default.
• W2145882925 abstract "Geologic mapping in south-central Virginia demonstrates that the stratigraphy and structure of the Carolina slate belt extend northward across a steep thermal gradient into upper amphibolite-facies correlative gneiss and schist. The Neoproterozoic greenschist-facies Hyco, Aaron, and Virgilina Formations were traced northward from their type localities near Virgilina, Virginia, along a simple, upright, northeast-trending isoclinal syncline. This syncline is called the Dryburg syncline and is a northern extension of the more complex Virgilina synclinorium. Progressively higher-grade equivalents of the Hyco and Aaron Formations were mapped northward along the axial trace of the refolded and westwardly-overturned Dryburg syncline through the Keysville and Green Bay 7.5-minute quadrangles, and across the northern end of the Carolina slate belt as interpreted on previous geologic maps. Hyco rocks, including felsic metatuff, metawacke, and amphibolite, become gneisses upgrade with areas of local anatexis and the segregation of granitic melt into leucosomes with biotite selvages. Phyllite of the Aaron Formation becomes garnet-bearing mica schist. Aaron Formation rocks disconformably overlie the primarily felsic volcanic and volcaniclastic rocks of the Hyco Formation as evidenced by repeated truncation of internal contacts within the Hyco on both limbs of the Dryburg syncline at the Aaron-Hyco contact. East-northeast-trending isograds, defined successively by the first appearance of garnet, then kyanite ± staurolite in sufficiently aluminous rocks, are superposed on the stratigraphic units and synclinal structure at moderate to high angles to strike. The textural distinction between gneisses and identifiable sedimentary structures occurs near the kyanite ± staurolite-in isograd. Development of the steep thermal gradient and regional penetrative fabric is interpreted to result from emplacement of the Goochland terrane adjacent to the northern end of the slate belt during Alleghanian orogenesis. This mapping study indicates that the Carolina slate belt does not terminate on the north against through-going faults or rest on higher-grade basement as previously suggested." @default.
• W2145882925 created "2016-06-24" @default.
• W2145882925 creator A5001272365 @default.
• W2145882925 creator A5021242854 @default.
• W2145882925 creator A5044117230 @default.
• W2145882925 creator A5072767035 @default.
• W2145882925 date "2007-04-01" @default.
• W2145882925 modified "2023-10-16" @default.
• W2145882925 title "Northward extension of carolina slate belt stratigraphy and structure, south-central virginia: Results from geologic mapping" @default.
• W2145882925 cites W11414049 @default.
• W2145882925 cites W1512020177 @default.
• W2145882925 cites W1544335146 @default.
• W2145882925 cites W1967742585 @default.
• W2145882925 cites W2010579216 @default.
• W2145882925 cites W2018487270 @default.
• W2145882925 cites W2021472427 @default.
• W2145882925 cites W2035151649 @default.
• W2145882925 cites W2064941535 @default.
• W2145882925 cites W2075825313 @default.
• W2145882925 cites W2078027909 @default.
• W2145882925 cites W2079677010 @default.
• W2145882925 cites W2094551879 @default.
• W2145882925 cites W2127665746 @default.
• W2145882925 cites W2137995554 @default.
• W2145882925 cites W2162711786 @default.
• W2145882925 cites W2312666490 @default.
• W2145882925 cites W2325183290 @default.
• W2145882925 cites W2334389109 @default.
• W2145882925 cites W2486687458 @default.
• W2145882925 cites W2589206132 @default.
• W2145882925 cites W582241888 @default.
• W2145882925 cites W609326478 @default.
• W2145882925 cites W3033574335 @default.
• W2145882925 doi "https://doi.org/10.2475/04.2007.04" @default.
• W2145882925 hasPublicationYear "2007" @default.
• W2145882925 type Work @default.
• W2145882925 sameAs 2145882925 @default.
• W2145882925 citedByCount "0" @default.
• W2145882925 crossrefType "journal-article" @default.
• W2145882925 hasAuthorship W2145882925A5001272365 @default.
• W2145882925 hasAuthorship W2145882925A5021242854 @default.
• W2145882925 hasAuthorship W2145882925A5044117230 @default.
• W2145882925 hasAuthorship W2145882925A5072767035 @default.
• W2145882925 hasBestOaLocation W21458829251 @default.
• W2145882925 hasConcept C101139013 @default.
• W2145882925 hasConcept C109007969 @default.
• W2145882925 hasConcept C112764850 @default.
• W2145882925 hasConcept C127313418 @default.
• W2145882925 hasConcept C146588470 @default.
• W2145882925 hasConcept C149465734 @default.
• W2145882925 hasConcept C151730666 @default.
• W2145882925 hasConcept C167284885 @default.
• W2145882925 hasConcept C171701179 @default.
• W2145882925 hasConcept C17409809 @default.
• W2145882925 hasConcept C193429443 @default.
• W2145882925 hasConcept C26687426 @default.
• W2145882925 hasConcept C26815474 @default.
• W2145882925 hasConcept C2778250313 @default.
• W2145882925 hasConcept C2779362224 @default.
• W2145882925 hasConcept C37045145 @default.
• W2145882925 hasConcept C77928131 @default.
• W2145882925 hasConcept C79927612 @default.
• W2145882925 hasConceptScore W2145882925C101139013 @default.
• W2145882925 hasConceptScore W2145882925C109007969 @default.
• W2145882925 hasConceptScore W2145882925C112764850 @default.
• W2145882925 hasConceptScore W2145882925C127313418 @default.
• W2145882925 hasConceptScore W2145882925C146588470 @default.
• W2145882925 hasConceptScore W2145882925C149465734 @default.
• W2145882925 hasConceptScore W2145882925C151730666 @default.
• W2145882925 hasConceptScore W2145882925C167284885 @default.
• W2145882925 hasConceptScore W2145882925C171701179 @default.
• W2145882925 hasConceptScore W2145882925C17409809 @default.
• W2145882925 hasConceptScore W2145882925C193429443 @default.
• W2145882925 hasConceptScore W2145882925C26687426 @default.
• W2145882925 hasConceptScore W2145882925C26815474 @default.
• W2145882925 hasConceptScore W2145882925C2778250313 @default.
• W2145882925 hasConceptScore W2145882925C2779362224 @default.
• W2145882925 hasConceptScore W2145882925C37045145 @default.
• W2145882925 hasConceptScore W2145882925C77928131 @default.
• W2145882925 hasConceptScore W2145882925C79927612 @default.
• W2145882925 hasIssue "4" @default.
• W2145882925 hasLocation W21458829251 @default.
• W2145882925 hasOpenAccess W2145882925 @default.
• W2145882925 hasPrimaryLocation W21458829251 @default.
• W2145882925 hasRelatedWork W1565044853 @default.
• W2145882925 hasRelatedWork W2029349985 @default.
• W2145882925 hasRelatedWork W2040834967 @default.
• W2145882925 hasRelatedWork W2145882925 @default.
• W2145882925 hasRelatedWork W2160618206 @default.
• W2145882925 hasRelatedWork W2308236690 @default.
• W2145882925 hasRelatedWork W2349947565 @default.
• W2145882925 hasRelatedWork W2586729066 @default.
• W2145882925 hasRelatedWork W56719329 @default.
• W2145882925 hasRelatedWork W838758648 @default.
• W2145882925 hasVolume "307" @default.
• W2145882925 isParatext "false" @default.
• W2145882925 isRetracted "false" @default.
• W2145882925 magId "2145882925" @default.

• next