FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2008765384> ?p ?o ?g. }

• W2008765384 endingPage "7556" @default.
• W2008765384 startingPage "7539" @default.
• W2008765384 abstract "Oceanic plateaus are major ocean features, yet their origins and development are poorly understood. Many are huge piles of basalt, and it is widely accepted that mantle plumes are their source, perhaps from eruptions of the voluminous head of an emerging plume. Shatsky Rise is a basaltic plateau that formed during a period of geomagnetic reversals, unlike many mid‐Cretaceous plateaus, so magnetic data can help us understand its tectonic history. In this study, we analyzed magnetic anomaly data from 131 cruises over and around Shatsky Rise and constructed a magnetic lineation chart for tectonic interpretation. A significant finding is that magnetic lineations are traceable through low parts of the rise between volcanic massifs, indicating nearly normal lithosphere, and between large volcanic edifices. Many lineations form bights near the rise axis and show former locations of the Pacific‐Izanagi‐Farallon triple junction. They indicate that the junction was in a ridge‐ridge‐ridge (RRR) configuration and closely followed the rise axis from chron M20 (146 Ma) to chron M4 (127 Ma). Lineation and bight geometries indicate that the triple junction jumped northeastward at least nine times, often apparently in response to volcanic activity from the mantle plume. Some jumps, however, appear related to ridge reorientations. Numerous features within the rise are parallel to lineations or lineation offsets, implying that the plateau formed near the triple junction and was modified by ridge faulting. Most of our observations support the hypothesis that Shatsky Rise was formed by a mantle plume that captured a triple junction." @default.
• W2008765384 created "2016-06-24" @default.
• W2008765384 creator A5054511541 @default.
• W2008765384 creator A5056216860 @default.
• W2008765384 creator A5078718326 @default.
• W2008765384 date "1999-04-10" @default.
• W2008765384 modified "2023-10-17" @default.
• W2008765384 title "Magnetic lineations within Shatsky Rise, northwest Pacific Ocean: Implications for hot spot‐triple junction interaction and oceanic plateau formation" @default.
• W2008765384 cites W1493328586 @default.
• W2008765384 cites W1510744043 @default.
• W2008765384 cites W1535589826 @default.
• W2008765384 cites W1600627284 @default.
• W2008765384 cites W1965522845 @default.
• W2008765384 cites W1966917681 @default.
• W2008765384 cites W1969955164 @default.
• W2008765384 cites W2002950669 @default.
• W2008765384 cites W2007613085 @default.
• W2008765384 cites W2017422309 @default.
• W2008765384 cites W2018396915 @default.
• W2008765384 cites W2020053214 @default.
• W2008765384 cites W2021959819 @default.
• W2008765384 cites W2023451840 @default.
• W2008765384 cites W2023781651 @default.
• W2008765384 cites W2026807252 @default.
• W2008765384 cites W2033223278 @default.
• W2008765384 cites W2039850020 @default.
• W2008765384 cites W2040430455 @default.
• W2008765384 cites W2041269880 @default.
• W2008765384 cites W2045826394 @default.
• W2008765384 cites W2047660088 @default.
• W2008765384 cites W2056668951 @default.
• W2008765384 cites W2057371440 @default.
• W2008765384 cites W2058884294 @default.
• W2008765384 cites W2059685173 @default.
• W2008765384 cites W2064674501 @default.
• W2008765384 cites W2065684465 @default.
• W2008765384 cites W2066176154 @default.
• W2008765384 cites W2074902400 @default.
• W2008765384 cites W2083420683 @default.
• W2008765384 cites W2083428579 @default.
• W2008765384 cites W2089962601 @default.
• W2008765384 cites W2090151175 @default.
• W2008765384 cites W2104938345 @default.
• W2008765384 cites W2124100891 @default.
• W2008765384 cites W2134798915 @default.
• W2008765384 cites W2153536201 @default.
• W2008765384 cites W2482414511 @default.
• W2008765384 cites W2542801869 @default.
• W2008765384 cites W3011093675 @default.
• W2008765384 doi "https://doi.org/10.1029/1999jb900002" @default.
• W2008765384 hasPublicationYear "1999" @default.
• W2008765384 type Work @default.
• W2008765384 sameAs 2008765384 @default.
• W2008765384 citedByCount "123" @default.
• W2008765384 countsByYear W20087653842012 @default.
• W2008765384 countsByYear W20087653842013 @default.
• W2008765384 countsByYear W20087653842014 @default.
• W2008765384 countsByYear W20087653842015 @default.
• W2008765384 countsByYear W20087653842016 @default.
• W2008765384 countsByYear W20087653842017 @default.
• W2008765384 countsByYear W20087653842018 @default.
• W2008765384 countsByYear W20087653842019 @default.
• W2008765384 countsByYear W20087653842020 @default.
• W2008765384 countsByYear W20087653842021 @default.
• W2008765384 countsByYear W20087653842022 @default.
• W2008765384 countsByYear W20087653842023 @default.
• W2008765384 crossrefType "journal-article" @default.
• W2008765384 hasAuthorship W2008765384A5054511541 @default.
• W2008765384 hasAuthorship W2008765384A5056216860 @default.
• W2008765384 hasAuthorship W2008765384A5078718326 @default.
• W2008765384 hasBestOaLocation W20087653841 @default.
• W2008765384 hasConcept C120806208 @default.
• W2008765384 hasConcept C121332964 @default.
• W2008765384 hasConcept C127313418 @default.
• W2008765384 hasConcept C146481406 @default.
• W2008765384 hasConcept C147894010 @default.
• W2008765384 hasConcept C151730666 @default.
• W2008765384 hasConcept C165205528 @default.
• W2008765384 hasConcept C16942324 @default.
• W2008765384 hasConcept C194482375 @default.
• W2008765384 hasConcept C2775840915 @default.
• W2008765384 hasConcept C2777994876 @default.
• W2008765384 hasConcept C2778282194 @default.
• W2008765384 hasConcept C32277403 @default.
• W2008765384 hasConcept C58097730 @default.
• W2008765384 hasConcept C77928131 @default.
• W2008765384 hasConcept C8058405 @default.
• W2008765384 hasConcept C97355855 @default.
• W2008765384 hasConcept C98742433 @default.
• W2008765384 hasConceptScore W2008765384C120806208 @default.
• W2008765384 hasConceptScore W2008765384C121332964 @default.
• W2008765384 hasConceptScore W2008765384C127313418 @default.
• W2008765384 hasConceptScore W2008765384C146481406 @default.
• W2008765384 hasConceptScore W2008765384C147894010 @default.
• W2008765384 hasConceptScore W2008765384C151730666 @default.
• W2008765384 hasConceptScore W2008765384C165205528 @default.
• W2008765384 hasConceptScore W2008765384C16942324 @default.
• W2008765384 hasConceptScore W2008765384C194482375 @default.

• next