FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2593117777> ?p ?o ?g. }

• W2593117777 endingPage "120" @default.
• W2593117777 startingPage "108" @default.
• W2593117777 abstract "The Walvis Ridge is one of the major hotspot trails in the South Atlantic and a classical example for volcanic island chains. Two models compete about the origin of the ridge: It is either the result of a deep mantle plume or active fracture zones above mantle inhomogeneities. Among other things crustal information is needed to constrain the models. Here, we provide such constraint with a 480 km long P-wave velocity model of the deep crustal structure of the eastern Walvis Ridge at 6° E. According to our data the Walvis Ridge stretches across the Florianopolis Fracture Zone into the Angola Basin. Here, we observe a basement high and thick basaltic layers covering the oceanic crust and the fracture zone. We found two crustal roots along the profile: one is located beneath the ridge crest, the other one beneath the northern basement high in the Angola Basin. The crustal thickness reaches 18 km and 12 km and the lower crustal velocities are 7.2 km/s and 7.4 km/s, respectively. The bathymetric expression of the ridge along the profile is less pronounced than closer to shore, which is mainly attributable to the absence of a thick layer of volcanic debris, rather than to reduced crustal thickness below the basement surface. Therefore, this part of the ridge was never or only briefly subaerially exposed. The crustal structure suggests that the ridge and the fracture zone formed independently of each other. The oceanic crust north of the fracture zone, which is buried underneath the basalt layer, is younger than the reconstructed age of hotspot volcanism of the Walvis Ridge. We interpret these structures north of the fracture zone to be at least partly a product of late stage volcanism." @default.
• W2593117777 created "2017-03-16" @default.
• W2593117777 creator A5007089586 @default.
• W2593117777 creator A5039996849 @default.
• W2593117777 creator A5075440066 @default.
• W2593117777 date "2017-10-01" @default.
• W2593117777 modified "2023-10-18" @default.
• W2593117777 title "Interaction between a hotspot and a fracture zone: The crustal structure of Walvis Ridge at 6° E" @default.
• W2593117777 cites W1480881588 @default.
• W2593117777 cites W1523067580 @default.
• W2593117777 cites W1533183184 @default.
• W2593117777 cites W1868360353 @default.
• W2593117777 cites W1896601192 @default.
• W2593117777 cites W1979170629 @default.
• W2593117777 cites W1979728158 @default.
• W2593117777 cites W1983086091 @default.
• W2593117777 cites W1992192773 @default.
• W2593117777 cites W1992390499 @default.
• W2593117777 cites W2006032174 @default.
• W2593117777 cites W2009046233 @default.
• W2593117777 cites W2025394267 @default.
• W2593117777 cites W2026818690 @default.
• W2593117777 cites W2031596985 @default.
• W2593117777 cites W2036853755 @default.
• W2593117777 cites W2039157170 @default.
• W2593117777 cites W2044690415 @default.
• W2593117777 cites W2047018904 @default.
• W2593117777 cites W2056848092 @default.
• W2593117777 cites W2056851935 @default.
• W2593117777 cites W2062677185 @default.
• W2593117777 cites W2070686596 @default.
• W2593117777 cites W2079851790 @default.
• W2593117777 cites W2081696323 @default.
• W2593117777 cites W2088715187 @default.
• W2593117777 cites W2091869523 @default.
• W2593117777 cites W2095950674 @default.
• W2593117777 cites W2102452791 @default.
• W2593117777 cites W2114660893 @default.
• W2593117777 cites W2120304236 @default.
• W2593117777 cites W2122856225 @default.
• W2593117777 cites W2137335718 @default.
• W2593117777 cites W2137978791 @default.
• W2593117777 cites W2151859611 @default.
• W2593117777 cites W2153846210 @default.
• W2593117777 cites W2154783705 @default.
• W2593117777 cites W2154861622 @default.
• W2593117777 cites W2159808525 @default.
• W2593117777 cites W2160431324 @default.
• W2593117777 cites W2168959606 @default.
• W2593117777 cites W2432609928 @default.
• W2593117777 cites W2471906810 @default.
• W2593117777 cites W2503837247 @default.
• W2593117777 cites W2562305412 @default.
• W2593117777 cites W4238075456 @default.
• W2593117777 cites W4244341864 @default.
• W2593117777 doi "https://doi.org/10.1016/j.tecto.2017.03.001" @default.
• W2593117777 hasPublicationYear "2017" @default.
• W2593117777 type Work @default.
• W2593117777 sameAs 2593117777 @default.
• W2593117777 citedByCount "15" @default.
• W2593117777 countsByYear W25931177772018 @default.
• W2593117777 countsByYear W25931177772019 @default.
• W2593117777 countsByYear W25931177772020 @default.
• W2593117777 countsByYear W25931177772021 @default.
• W2593117777 countsByYear W25931177772022 @default.
• W2593117777 countsByYear W25931177772023 @default.
• W2593117777 crossrefType "journal-article" @default.
• W2593117777 hasAuthorship W2593117777A5007089586 @default.
• W2593117777 hasAuthorship W2593117777A5039996849 @default.
• W2593117777 hasAuthorship W2593117777A5075440066 @default.
• W2593117777 hasBestOaLocation W25931177772 @default.
• W2593117777 hasConcept C117485682 @default.
• W2593117777 hasConcept C120806208 @default.
• W2593117777 hasConcept C127313418 @default.
• W2593117777 hasConcept C135559958 @default.
• W2593117777 hasConcept C146481406 @default.
• W2593117777 hasConcept C147894010 @default.
• W2593117777 hasConcept C151730666 @default.
• W2593117777 hasConcept C154200439 @default.
• W2593117777 hasConcept C161509811 @default.
• W2593117777 hasConcept C165205528 @default.
• W2593117777 hasConcept C16942324 @default.
• W2593117777 hasConcept C2776698055 @default.
• W2593117777 hasConcept C2778677506 @default.
• W2593117777 hasConcept C32277403 @default.
• W2593117777 hasConcept C51151373 @default.
• W2593117777 hasConcept C58097730 @default.
• W2593117777 hasConcept C5900021 @default.
• W2593117777 hasConcept C67236022 @default.
• W2593117777 hasConcept C77928131 @default.
• W2593117777 hasConceptScore W2593117777C117485682 @default.
• W2593117777 hasConceptScore W2593117777C120806208 @default.
• W2593117777 hasConceptScore W2593117777C127313418 @default.
• W2593117777 hasConceptScore W2593117777C135559958 @default.
• W2593117777 hasConceptScore W2593117777C146481406 @default.
• W2593117777 hasConceptScore W2593117777C147894010 @default.
• W2593117777 hasConceptScore W2593117777C151730666 @default.
• W2593117777 hasConceptScore W2593117777C154200439 @default.

• next