FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1987643414> ?p ?o ?g. }

• W1987643414 endingPage "16015" @default.
• W1987643414 startingPage "15991" @default.
• W1987643414 abstract "Mylitta Fluctus is a volcanic flow field that covers approximately 300,000 km 2 in southern Lavinia Planitia. The flows are typically radar‐bright with uniform surface textures. Central channels are common. Maximum flow lengths range from 400 to 1000 km; flow widths range 30–100 km in the medial and distal portions of the flow field. The total volume of the flow field, based on estimates of flow thickness, is of the order of 2 × 10 4 km 3 . The flow field is composed of six smaller flow fields that are interpreted to represent major eruption events in the evolution of Mylitta. An asymmetric shield volcano 200 km in radius with a central caldera has been identified as the single major source. It is located along a possible rift zone at the northern edge of Lada Terra. No evidence for fissure‐fed eruptions is observed, although eruptions may have occurred along fissures within the rift before the main vent centralized. Mylitta is similar in scale to many terrestrial flood basalt provinces, although it is lower in total estimated volume and is distinguished by the presence of a central source edifice. The origin of Mylitta is proposed to be linked to regional extension and possible hotspot activity in a manner similar to that suggested for the origin of terrestrial flood basalts. The lower apparent volume of Mylitta relative to terrestrial flood basalts suggests that the amount of material upwelling from the mantle may have been lower in this case or that the formation of the flow field has not yet finished. Detailed studies of the morphology and distribution of flow fields similar to Mylitta should yield insight into the variation and evolution of hotspot‐related volcanism and the formation of possible flood basalts on Venus." @default.
• W1987643414 created "2016-06-24" @default.
• W1987643414 creator A5007250708 @default.
• W1987643414 creator A5023264421 @default.
• W1987643414 creator A5036972952 @default.
• W1987643414 creator A5080536069 @default.
• W1987643414 date "1992-10-25" @default.
• W1987643414 modified "2023-10-17" @default.
• W1987643414 title "Mylitta Fluctus, Venus: Rift‐related, centralized volcanism and the emplacement of large‐volume flow units" @default.
• W1987643414 cites W1855938585 @default.
• W1987643414 cites W1966917681 @default.
• W1987643414 cites W1982243468 @default.
• W1987643414 cites W1982299760 @default.
• W1987643414 cites W2004749421 @default.
• W1987643414 cites W2004795408 @default.
• W1987643414 cites W2007113613 @default.
• W1987643414 cites W2007123004 @default.
• W1987643414 cites W2009313161 @default.
• W1987643414 cites W2016418052 @default.
• W1987643414 cites W2017392760 @default.
• W1987643414 cites W2020913119 @default.
• W1987643414 cites W2022648729 @default.
• W1987643414 cites W2026650065 @default.
• W1987643414 cites W2030142526 @default.
• W1987643414 cites W2034299044 @default.
• W1987643414 cites W2034728404 @default.
• W1987643414 cites W2040421381 @default.
• W1987643414 cites W2042120195 @default.
• W1987643414 cites W2046426212 @default.
• W1987643414 cites W2056367705 @default.
• W1987643414 cites W2061688203 @default.
• W1987643414 cites W2064058802 @default.
• W1987643414 cites W2070736873 @default.
• W1987643414 cites W2074511800 @default.
• W1987643414 cites W2077151738 @default.
• W1987643414 cites W2079619279 @default.
• W1987643414 cites W2084388491 @default.
• W1987643414 cites W2086545252 @default.
• W1987643414 cites W2092345110 @default.
• W1987643414 cites W2093567690 @default.
• W1987643414 cites W2095574869 @default.
• W1987643414 cites W2131180775 @default.
• W1987643414 cites W2145975417 @default.
• W1987643414 cites W2169458059 @default.
• W1987643414 cites W2169783778 @default.
• W1987643414 cites W2307097205 @default.
• W1987643414 doi "https://doi.org/10.1029/92je01245" @default.
• W1987643414 hasPublicationYear "1992" @default.
• W1987643414 type Work @default.
• W1987643414 sameAs 1987643414 @default.
• W1987643414 citedByCount "59" @default.
• W1987643414 countsByYear W19876434142012 @default.
• W1987643414 countsByYear W19876434142013 @default.
• W1987643414 countsByYear W19876434142014 @default.
• W1987643414 countsByYear W19876434142015 @default.
• W1987643414 countsByYear W19876434142016 @default.
• W1987643414 countsByYear W19876434142017 @default.
• W1987643414 countsByYear W19876434142020 @default.
• W1987643414 countsByYear W19876434142021 @default.
• W1987643414 countsByYear W19876434142023 @default.
• W1987643414 crossrefType "journal-article" @default.
• W1987643414 hasAuthorship W1987643414A5007250708 @default.
• W1987643414 hasAuthorship W1987643414A5023264421 @default.
• W1987643414 hasAuthorship W1987643414A5036972952 @default.
• W1987643414 hasAuthorship W1987643414A5080536069 @default.
• W1987643414 hasConcept C109902934 @default.
• W1987643414 hasConcept C113754120 @default.
• W1987643414 hasConcept C120806208 @default.
• W1987643414 hasConcept C127313418 @default.
• W1987643414 hasConcept C158959774 @default.
• W1987643414 hasConcept C161509811 @default.
• W1987643414 hasConcept C165205528 @default.
• W1987643414 hasConcept C183222429 @default.
• W1987643414 hasConcept C2778471503 @default.
• W1987643414 hasConcept C32848823 @default.
• W1987643414 hasConcept C49708893 @default.
• W1987643414 hasConcept C50682988 @default.
• W1987643414 hasConcept C6363049 @default.
• W1987643414 hasConcept C67236022 @default.
• W1987643414 hasConcept C6787264 @default.
• W1987643414 hasConcept C77928131 @default.
• W1987643414 hasConcept C8058405 @default.
• W1987643414 hasConcept C9566828 @default.
• W1987643414 hasConceptScore W1987643414C109902934 @default.
• W1987643414 hasConceptScore W1987643414C113754120 @default.
• W1987643414 hasConceptScore W1987643414C120806208 @default.
• W1987643414 hasConceptScore W1987643414C127313418 @default.
• W1987643414 hasConceptScore W1987643414C158959774 @default.
• W1987643414 hasConceptScore W1987643414C161509811 @default.
• W1987643414 hasConceptScore W1987643414C165205528 @default.
• W1987643414 hasConceptScore W1987643414C183222429 @default.
• W1987643414 hasConceptScore W1987643414C2778471503 @default.
• W1987643414 hasConceptScore W1987643414C32848823 @default.
• W1987643414 hasConceptScore W1987643414C49708893 @default.
• W1987643414 hasConceptScore W1987643414C50682988 @default.
• W1987643414 hasConceptScore W1987643414C6363049 @default.
• W1987643414 hasConceptScore W1987643414C67236022 @default.
• W1987643414 hasConceptScore W1987643414C6787264 @default.

• next