FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1988469968> ?p ?o ?g. }

• W1988469968 endingPage "236" @default.
• W1988469968 startingPage "223" @default.
• W1988469968 abstract "The Mesozoic Nevadan orogeny in the northern Sierra Nevada metamorphic belt, California, may be attributed to arc-continent collision, stratigraphic data and macroscopic cross cutting relations suggest successive accretion of two arcs along an active continental margin. The younger accretion event involved the Early Jurassic Slate Creek terrane, which is a 3–5 km thick pseudostratigraphic arc fragment. The Slate Creek thrust, an isoclinally folded fault with a subhorizontal median surface, carries the Slate Creek terrane at least 40 km eastward (continentward) over the pre-existing continental margin terrane amalgam. No rock units can be correlated across the Slate Creek thrust which is thus interpreted as an arc-continent suture. In addition to the Slate Creek thrust, the Nevadan orogen includes a major east-vergent imbricate thrust set east of and beneath the Slate Creek thrust, and steep west-vergent reverse shear zones, macroscopic upright folds, and steep foliations that overprint and cut the east-vergent structures. These data suggest a model for the relationships between the kinematics of arc collision and Nevadan orogenic structures. The Slate Creek arc terrane accreted by westward partial subduction of the continental margin along the east-vergent Slate Creek thrust. The continental margin was imbricated along an east-vergent thrust set. The structurally higher, inactive Slate Creek thrust-suture was deformed by steep west-vergent shear zones, folds, and foliations which may have accommodated shortening of the east-vergent thrust sheet. This deformation occurred within an active, continental margin arc that probably initiated by subduction flip after collision of the Slate Creek arc. This kinematic model is consistent with the structural geometry and chronology of the Nevadan orogen while qualitatively maintaining lithosphere-scale strain compatibility. This model has implications for problems related to emplacement of large crystalline thrust sheets, displacements beneath and at the margins of shortened crustal segments, and interaction of oppositely-verging structures. The Nevadan orogen is a slate belt, and the structural-plate tectonic model presented for the Nevadan orogeny may be testable in slate belts of other orogens." @default.
• W1988469968 created "2016-06-24" @default.
• W1988469968 creator A5083098593 @default.
• W1988469968 date "1991-06-01" @default.
• W1988469968 modified "2023-09-26" @default.
• W1988469968 title "Relationships between kinematics of arc-continent collision and kinematics of thrust faults, folds, shear zones, and foliations in the Nevadan orogen, northern Sierra Nevada, California" @default.
• W1988469968 cites W1482208893 @default.
• W1988469968 cites W1491817880 @default.
• W1988469968 cites W1508508756 @default.
• W1988469968 cites W1537503551 @default.
• W1988469968 cites W1964369447 @default.
• W1988469968 cites W1964697893 @default.
• W1988469968 cites W1964776185 @default.
• W1988469968 cites W1968546289 @default.
• W1988469968 cites W1968794798 @default.
• W1988469968 cites W1973989349 @default.
• W1988469968 cites W1974767724 @default.
• W1988469968 cites W1982248208 @default.
• W1988469968 cites W1983889008 @default.
• W1988469968 cites W1994596740 @default.
• W1988469968 cites W2011112180 @default.
• W1988469968 cites W2015515830 @default.
• W1988469968 cites W2016512270 @default.
• W1988469968 cites W2029114766 @default.
• W1988469968 cites W2033097432 @default.
• W1988469968 cites W2034472821 @default.
• W1988469968 cites W2056090805 @default.
• W1988469968 cites W2060888748 @default.
• W1988469968 cites W2077635133 @default.
• W1988469968 cites W2081344495 @default.
• W1988469968 cites W2087807772 @default.
• W1988469968 cites W2092489160 @default.
• W1988469968 cites W2095114392 @default.
• W1988469968 cites W2098817166 @default.
• W1988469968 cites W2101373275 @default.
• W1988469968 cites W2103684543 @default.
• W1988469968 cites W2111416196 @default.
• W1988469968 cites W2111555634 @default.
• W1988469968 cites W2116474531 @default.
• W1988469968 cites W2129826503 @default.
• W1988469968 cites W2133444858 @default.
• W1988469968 cites W2143501565 @default.
• W1988469968 cites W2151683179 @default.
• W1988469968 cites W2151790874 @default.
• W1988469968 cites W2162689360 @default.
• W1988469968 cites W2221232656 @default.
• W1988469968 cites W2242121529 @default.
• W1988469968 cites W2268315494 @default.
• W1988469968 cites W2331716385 @default.
• W1988469968 cites W2739230933 @default.
• W1988469968 cites W2772384892 @default.
• W1988469968 cites W3155294389 @default.
• W1988469968 cites W68009034 @default.
• W1988469968 cites W8595611 @default.
• W1988469968 doi "https://doi.org/10.1016/0040-1951(91)90058-z" @default.
• W1988469968 hasPublicationYear "1991" @default.
• W1988469968 type Work @default.
• W1988469968 sameAs 1988469968 @default.
• W1988469968 citedByCount "6" @default.
• W1988469968 countsByYear W19884699682013 @default.
• W1988469968 crossrefType "journal-article" @default.
• W1988469968 hasAuthorship W1988469968A5083098593 @default.
• W1988469968 hasConcept C105702510 @default.
• W1988469968 hasConcept C110041135 @default.
• W1988469968 hasConcept C114793014 @default.
• W1988469968 hasConcept C121332964 @default.
• W1988469968 hasConcept C127313418 @default.
• W1988469968 hasConcept C150999391 @default.
• W1988469968 hasConcept C151730666 @default.
• W1988469968 hasConcept C153220577 @default.
• W1988469968 hasConcept C165205528 @default.
• W1988469968 hasConcept C175551986 @default.
• W1988469968 hasConcept C201867031 @default.
• W1988469968 hasConcept C23295444 @default.
• W1988469968 hasConcept C2776401274 @default.
• W1988469968 hasConcept C2777327002 @default.
• W1988469968 hasConcept C44870925 @default.
• W1988469968 hasConcept C58097730 @default.
• W1988469968 hasConcept C71924100 @default.
• W1988469968 hasConcept C77928131 @default.
• W1988469968 hasConcept C79420006 @default.
• W1988469968 hasConcept C96035792 @default.
• W1988469968 hasConcept C97355855 @default.
• W1988469968 hasConceptScore W1988469968C105702510 @default.
• W1988469968 hasConceptScore W1988469968C110041135 @default.
• W1988469968 hasConceptScore W1988469968C114793014 @default.
• W1988469968 hasConceptScore W1988469968C121332964 @default.
• W1988469968 hasConceptScore W1988469968C127313418 @default.
• W1988469968 hasConceptScore W1988469968C150999391 @default.
• W1988469968 hasConceptScore W1988469968C151730666 @default.
• W1988469968 hasConceptScore W1988469968C153220577 @default.
• W1988469968 hasConceptScore W1988469968C165205528 @default.
• W1988469968 hasConceptScore W1988469968C175551986 @default.
• W1988469968 hasConceptScore W1988469968C201867031 @default.
• W1988469968 hasConceptScore W1988469968C23295444 @default.
• W1988469968 hasConceptScore W1988469968C2776401274 @default.
• W1988469968 hasConceptScore W1988469968C2777327002 @default.
• W1988469968 hasConceptScore W1988469968C44870925 @default.

• next