Matches in SemOpenAlex for { <https://semopenalex.org/work/W2116760736> ?p ?o ?g. }
Showing items 1 to 84 of
84
with 100 items per page.
- W2116760736 endingPage "802" @default.
- W2116760736 startingPage "802" @default.
- W2116760736 abstract "The New Madrid seismic zone of the central Mississippi River valley has been interpreted to be a right-lateral strike-slip fault zone with a left stepover restraining bend (Reelfoot reverse fault). This model is overly simplistic because New Madrid seismicity continues 30 km southeast of the stepover. In this study we have analyzed 1704 earthquake hypocenters obtained between 1995 and 2006 in three-dimensional (3-D) space to more accurately map fault geometry in the New Madrid seismic zone. Most of the earthquakes appear to align along fault planes. The faults identified include the New Madrid North (29°, 72° SE), Risco (92°, 82° N), Axial (46°, 90°), Reelfoot North (167°, 30° SW), and Reelfoot South (150°, 44° SW) faults. A diffuse zone of earthquakes exists where the Axial fault divides the Reelfoot fault into the Reelfoot North and Reelfoot South faults. Regional mapping of the top of the Precambrian crystalline basement indicates that the Reelfoot North fault has an average of 500 m and the Reelfoot South fault 1200 m of down-to-the-southwest normal displacement. Since previously published seismic reflection profiles reveal reverse displacement on top of the Paleozoic and younger strata, the Reelfoot North and South faults are herein interpreted to be inverted basement normal faults. The Reelfoot North and Reelfoot South faults differ in strike, dip, depth, and displacement, and only the Reelfoot North fault has a surface scarp (monocline). Thus, the Reelfoot fault is actually composed of two left-stepping restraining bends and two faults that together extend across the entire width of the Reelfoot rift." @default.
- W2116760736 created "2016-06-24" @default.
- W2116760736 creator A5044776219 @default.
- W2116760736 creator A5048681211 @default.
- W2116760736 date "2008-01-01" @default.
- W2116760736 modified "2023-09-29" @default.
- W2116760736 title "New Madrid seismic zone fault geometry" @default.
- W2116760736 cites W1879613374 @default.
- W2116760736 cites W1964442736 @default.
- W2116760736 cites W1987356278 @default.
- W2116760736 cites W2153814770 @default.
- W2116760736 cites W2157764718 @default.
- W2116760736 cites W2171131956 @default.
- W2116760736 cites W2174868752 @default.
- W2116760736 cites W2272970159 @default.
- W2116760736 cites W2478068577 @default.
- W2116760736 doi "https://doi.org/10.1130/ges00141.1" @default.
- W2116760736 hasPublicationYear "2008" @default.
- W2116760736 type Work @default.
- W2116760736 sameAs 2116760736 @default.
- W2116760736 citedByCount "52" @default.
- W2116760736 countsByYear W21167607362012 @default.
- W2116760736 countsByYear W21167607362013 @default.
- W2116760736 countsByYear W21167607362014 @default.
- W2116760736 countsByYear W21167607362015 @default.
- W2116760736 countsByYear W21167607362016 @default.
- W2116760736 countsByYear W21167607362017 @default.
- W2116760736 countsByYear W21167607362018 @default.
- W2116760736 countsByYear W21167607362019 @default.
- W2116760736 countsByYear W21167607362020 @default.
- W2116760736 countsByYear W21167607362021 @default.
- W2116760736 countsByYear W21167607362022 @default.
- W2116760736 countsByYear W21167607362023 @default.
- W2116760736 crossrefType "journal-article" @default.
- W2116760736 hasAuthorship W2116760736A5044776219 @default.
- W2116760736 hasAuthorship W2116760736A5048681211 @default.
- W2116760736 hasBestOaLocation W21167607361 @default.
- W2116760736 hasConcept C114679195 @default.
- W2116760736 hasConcept C127203543 @default.
- W2116760736 hasConcept C127313418 @default.
- W2116760736 hasConcept C127413603 @default.
- W2116760736 hasConcept C13106087 @default.
- W2116760736 hasConcept C147176958 @default.
- W2116760736 hasConcept C151730666 @default.
- W2116760736 hasConcept C165205528 @default.
- W2116760736 hasConcept C173776410 @default.
- W2116760736 hasConcept C175551986 @default.
- W2116760736 hasConcept C2781297371 @default.
- W2116760736 hasConcept C77928131 @default.
- W2116760736 hasConcept C83176761 @default.
- W2116760736 hasConceptScore W2116760736C114679195 @default.
- W2116760736 hasConceptScore W2116760736C127203543 @default.
- W2116760736 hasConceptScore W2116760736C127313418 @default.
- W2116760736 hasConceptScore W2116760736C127413603 @default.
- W2116760736 hasConceptScore W2116760736C13106087 @default.
- W2116760736 hasConceptScore W2116760736C147176958 @default.
- W2116760736 hasConceptScore W2116760736C151730666 @default.
- W2116760736 hasConceptScore W2116760736C165205528 @default.
- W2116760736 hasConceptScore W2116760736C173776410 @default.
- W2116760736 hasConceptScore W2116760736C175551986 @default.
- W2116760736 hasConceptScore W2116760736C2781297371 @default.
- W2116760736 hasConceptScore W2116760736C77928131 @default.
- W2116760736 hasConceptScore W2116760736C83176761 @default.
- W2116760736 hasIssue "5" @default.
- W2116760736 hasLocation W21167607361 @default.
- W2116760736 hasOpenAccess W2116760736 @default.
- W2116760736 hasPrimaryLocation W21167607361 @default.
- W2116760736 hasRelatedWork W1944877252 @default.
- W2116760736 hasRelatedWork W1976317616 @default.
- W2116760736 hasRelatedWork W2043407093 @default.
- W2116760736 hasRelatedWork W2070847651 @default.
- W2116760736 hasRelatedWork W2073444015 @default.
- W2116760736 hasRelatedWork W2095757660 @default.
- W2116760736 hasRelatedWork W2315129140 @default.
- W2116760736 hasRelatedWork W2315696278 @default.
- W2116760736 hasRelatedWork W2591832703 @default.
- W2116760736 hasRelatedWork W3112501696 @default.
- W2116760736 hasVolume "4" @default.
- W2116760736 isParatext "false" @default.
- W2116760736 isRetracted "false" @default.
- W2116760736 magId "2116760736" @default.
- W2116760736 workType "article" @default.