FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000404423> ?p ?o ?g. }

• W2000404423 endingPage "263" @default.
• W2000404423 startingPage "239" @default.
• W2000404423 abstract "The Snake Range décollement (SRD) in east‐central Nevada separates supracrustal rocks extended by normal faulting from ductilely deformed igneous and metamorphic rocks. A well‐known stratigraphy unaffected by earlier faulting permits analysis of both upper and lower plate strain leading to a better understanding of how vastly different rock types and deformational styles are juxtaposed along low‐angle faults in metamorphic core complexes. Middle Cambrian to Permian upper plate rocks are cut by two generations of NE trending, east directed normal faults. Both generations were initiated as high‐angle (60°) planar faults that flattened abruptly into the SRD and rotated domino style to low angles, yielding a total rotation of bedding of about 80–90°. Faulting is Tertiary in age as 35‐m.y.‐old volcanic rocks are involved and resulted in about 450–500% extension in a N55W‐;S55E direction. The SRD developed as a subhorizontal surface 6–7 km deep at the top of the Cambrian Pioche Shale. Lower plate granitic rocks and their late Precambrian‐Cambrian metamorphic country rocks were involved in progressive ductile to brittle extension at low greenschist grade, forming a penetrative subhorizontal foliation and N55–70W lineation that increases in intensity eastward and upward toward the SRD. Stretching and thinning in the lower plate is coaxial and comparable in magnitude to upper plate extension, and is interpreted as synchronous. K‐Ar ages ranging from 20 to 40 m.y. in the lower plate suggests the N. Snake Range represents a Tertiary thermal anomaly. We conclude that the SRD developed as a ductile‐brittle transition zone at 6–7 km depth. Gravity data suggests that the gently domed SRD is cut by younger Basin and Range faults, but the geology of adjacent ranges suggests that the SRD does not continue more than 60 km in any given direction. The lack of stratigraphic omission across the SRD rules out large amounts of movement on a surface that originally cut downsection, and we suggest that extensional detachment faults such as the SRD can be developed locally as boundaries between brittlely extended rocks and underlying ductile extension and intrusion." @default.
• W2000404423 created "2016-06-24" @default.
• W2000404423 creator A5005431172 @default.
• W2000404423 creator A5016640393 @default.
• W2000404423 creator A5026577031 @default.
• W2000404423 date "1983-06-01" @default.
• W2000404423 modified "2023-10-17" @default.
• W2000404423 title "The Snake Range Décollement: An exhumed Mid-Tertiary ductile-brittle transition" @default.
• W2000404423 cites W1518416130 @default.
• W2000404423 cites W155336274 @default.
• W2000404423 cites W1903458979 @default.
• W2000404423 cites W1924569715 @default.
• W2000404423 cites W1972167093 @default.
• W2000404423 cites W1973328624 @default.
• W2000404423 cites W2001882191 @default.
• W2000404423 cites W2019642854 @default.
• W2000404423 cites W2037522282 @default.
• W2000404423 cites W2068106790 @default.
• W2000404423 cites W2070465804 @default.
• W2000404423 cites W2071793309 @default.
• W2000404423 cites W2076224916 @default.
• W2000404423 cites W2092118088 @default.
• W2000404423 cites W2099512080 @default.
• W2000404423 cites W2155500845 @default.
• W2000404423 cites W2257165051 @default.
• W2000404423 cites W22920472 @default.
• W2000404423 cites W2340347543 @default.
• W2000404423 cites W2343214232 @default.
• W2000404423 cites W2400278868 @default.
• W2000404423 cites W4298420999 @default.
• W2000404423 doi "https://doi.org/10.1029/tc002i003p00239" @default.
• W2000404423 hasPublicationYear "1983" @default.
• W2000404423 type Work @default.
• W2000404423 sameAs 2000404423 @default.
• W2000404423 citedByCount "238" @default.
• W2000404423 countsByYear W20004044232012 @default.
• W2000404423 countsByYear W20004044232013 @default.
• W2000404423 countsByYear W20004044232014 @default.
• W2000404423 countsByYear W20004044232015 @default.
• W2000404423 countsByYear W20004044232016 @default.
• W2000404423 countsByYear W20004044232017 @default.
• W2000404423 countsByYear W20004044232018 @default.
• W2000404423 countsByYear W20004044232019 @default.
• W2000404423 countsByYear W20004044232020 @default.
• W2000404423 countsByYear W20004044232021 @default.
• W2000404423 countsByYear W20004044232022 @default.
• W2000404423 countsByYear W20004044232023 @default.
• W2000404423 crossrefType "journal-article" @default.
• W2000404423 hasAuthorship W2000404423A5005431172 @default.
• W2000404423 hasAuthorship W2000404423A5016640393 @default.
• W2000404423 hasAuthorship W2000404423A5026577031 @default.
• W2000404423 hasConcept C120806208 @default.
• W2000404423 hasConcept C127313418 @default.
• W2000404423 hasConcept C136137745 @default.
• W2000404423 hasConcept C151730666 @default.
• W2000404423 hasConcept C155627805 @default.
• W2000404423 hasConcept C165205528 @default.
• W2000404423 hasConcept C17409809 @default.
• W2000404423 hasConcept C185339796 @default.
• W2000404423 hasConcept C192241223 @default.
• W2000404423 hasConcept C26687426 @default.
• W2000404423 hasConcept C37045145 @default.
• W2000404423 hasConcept C42787717 @default.
• W2000404423 hasConcept C5900021 @default.
• W2000404423 hasConcept C63014310 @default.
• W2000404423 hasConcept C77928131 @default.
• W2000404423 hasConcept C98742433 @default.
• W2000404423 hasConceptScore W2000404423C120806208 @default.
• W2000404423 hasConceptScore W2000404423C127313418 @default.
• W2000404423 hasConceptScore W2000404423C136137745 @default.
• W2000404423 hasConceptScore W2000404423C151730666 @default.
• W2000404423 hasConceptScore W2000404423C155627805 @default.
• W2000404423 hasConceptScore W2000404423C165205528 @default.
• W2000404423 hasConceptScore W2000404423C17409809 @default.
• W2000404423 hasConceptScore W2000404423C185339796 @default.
• W2000404423 hasConceptScore W2000404423C192241223 @default.
• W2000404423 hasConceptScore W2000404423C26687426 @default.
• W2000404423 hasConceptScore W2000404423C37045145 @default.
• W2000404423 hasConceptScore W2000404423C42787717 @default.
• W2000404423 hasConceptScore W2000404423C5900021 @default.
• W2000404423 hasConceptScore W2000404423C63014310 @default.
• W2000404423 hasConceptScore W2000404423C77928131 @default.
• W2000404423 hasConceptScore W2000404423C98742433 @default.
• W2000404423 hasIssue "3" @default.
• W2000404423 hasLocation W20004044231 @default.
• W2000404423 hasOpenAccess W2000404423 @default.
• W2000404423 hasPrimaryLocation W20004044231 @default.
• W2000404423 hasRelatedWork W1495254432 @default.
• W2000404423 hasRelatedWork W2038989614 @default.
• W2000404423 hasRelatedWork W2086225853 @default.
• W2000404423 hasRelatedWork W2164643951 @default.
• W2000404423 hasRelatedWork W2283064580 @default.
• W2000404423 hasRelatedWork W2418700872 @default.
• W2000404423 hasRelatedWork W293705820 @default.
• W2000404423 hasRelatedWork W3018358708 @default.
• W2000404423 hasRelatedWork W3056175676 @default.
• W2000404423 hasRelatedWork W1672251905 @default.
• W2000404423 hasVolume "2" @default.

• next