FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3193873733> ?p ?o ?g. }

• W3193873733 abstract "Abstract The Australian‐Antarctic Ridge (AAR) is an intermediate‐spreading rate system located between the Southeast Indian Ridge and Macquarie Triple Junction of the Australian‐Antarctic‐Pacific plates. KR1 is the easternmost and longest AAR segment and exhibits unique axial morphology and various volcanic structures. We identified three asymmetric seamount chains positioned parallel to the seafloor spreading direction, which were indicative of prevalent off‐axis volcanism in the vicinity of segment KR1. Two‐dimensional magnetic modeling was used to predict the magnetization polarity of the seamounts, as well as to constrain their formation time and duration. The magnetic modeling revealed that the majority of the examined seamounts were formed over a period of less than ∼600 kyrs. The seamount formation primarily occurred during two distinct volcanic pulses from 0.16–1.14 to 1.58–2.69 Ma. A temporal gap of 200–650 kyrs between the formation time of the seamounts and seafloor was estimated for certain seamounts that were formed much later than their underlying seafloor and at a distance of 10–20 km from the KR1 axis. Typically, such off‐axis seamount activity is related to axial mantle convection caused by excessive magma supply near the ridge crest. Considering the scale of off‐axis volcanism and thickening lithosphere ∼20 km away from the axis with intermediate‐spreading rates, small‐scale upwelling made feasible by the fertile mantle heterogeneity is proposed as the mechanism for the seamount formations at off‐axis distances, and the geochemically enriched compositions of the seamounts support this alternative explanation." @default.
• W3193873733 created "2021-08-30" @default.
• W3193873733 creator A5033439167 @default.
• W3193873733 creator A5049875261 @default.
• W3193873733 creator A5069267886 @default.
• W3193873733 date "2021-09-01" @default.
• W3193873733 modified "2023-10-05" @default.
• W3193873733 title "Magnetic Constraints on Off‐Axis Seamount Volcanism in the Easternmost Segment of the Australian‐Antarctic Ridge" @default.
• W3193873733 cites W1533813737 @default.
• W3193873733 cites W1539311582 @default.
• W3193873733 cites W1586195761 @default.
• W3193873733 cites W1589201273 @default.
• W3193873733 cites W1624012152 @default.
• W3193873733 cites W1633323809 @default.
• W3193873733 cites W1862013975 @default.
• W3193873733 cites W1903208285 @default.
• W3193873733 cites W1951212893 @default.
• W3193873733 cites W1976608926 @default.
• W3193873733 cites W1978788058 @default.
• W3193873733 cites W1981030863 @default.
• W3193873733 cites W1982800323 @default.
• W3193873733 cites W1983520771 @default.
• W3193873733 cites W1989680157 @default.
• W3193873733 cites W1994977293 @default.
• W3193873733 cites W1997268075 @default.
• W3193873733 cites W2008712522 @default.
• W3193873733 cites W2009046233 @default.
• W3193873733 cites W2013495059 @default.
• W3193873733 cites W2015041730 @default.
• W3193873733 cites W2021959819 @default.
• W3193873733 cites W2023604492 @default.
• W3193873733 cites W2025061891 @default.
• W3193873733 cites W2027795135 @default.
• W3193873733 cites W2032033713 @default.
• W3193873733 cites W2034095102 @default.
• W3193873733 cites W2038338617 @default.
• W3193873733 cites W2041365719 @default.
• W3193873733 cites W2046266025 @default.
• W3193873733 cites W2048457570 @default.
• W3193873733 cites W2050022404 @default.
• W3193873733 cites W2055879106 @default.
• W3193873733 cites W2065167475 @default.
• W3193873733 cites W2068192866 @default.
• W3193873733 cites W2073730823 @default.
• W3193873733 cites W2076833330 @default.
• W3193873733 cites W2080234677 @default.
• W3193873733 cites W2083985973 @default.
• W3193873733 cites W2087239287 @default.
• W3193873733 cites W2090046792 @default.
• W3193873733 cites W2091646500 @default.
• W3193873733 cites W2097061955 @default.
• W3193873733 cites W2098813846 @default.
• W3193873733 cites W2098839042 @default.
• W3193873733 cites W2102234201 @default.
• W3193873733 cites W2108316127 @default.
• W3193873733 cites W2112194415 @default.
• W3193873733 cites W2115012406 @default.
• W3193873733 cites W2116593025 @default.
• W3193873733 cites W2123415250 @default.
• W3193873733 cites W2134423656 @default.
• W3193873733 cites W2139019018 @default.
• W3193873733 cites W2143254061 @default.
• W3193873733 cites W2146151718 @default.
• W3193873733 cites W2148281592 @default.
• W3193873733 cites W2150226675 @default.
• W3193873733 cites W2158583264 @default.
• W3193873733 cites W2166178563 @default.
• W3193873733 cites W2168976279 @default.
• W3193873733 cites W2257774785 @default.
• W3193873733 cites W2269655193 @default.
• W3193873733 cites W2327966818 @default.
• W3193873733 cites W2329232707 @default.
• W3193873733 cites W2480239077 @default.
• W3193873733 cites W2498330216 @default.
• W3193873733 cites W2755992464 @default.
• W3193873733 cites W2891086750 @default.
• W3193873733 cites W2914068391 @default.
• W3193873733 cites W3007220147 @default.
• W3193873733 cites W3111818795 @default.
• W3193873733 cites W3135346642 @default.
• W3193873733 cites W4230557738 @default.
• W3193873733 doi "https://doi.org/10.1029/2020gc009576" @default.
• W3193873733 hasPublicationYear "2021" @default.
• W3193873733 type Work @default.
• W3193873733 sameAs 3193873733 @default.
• W3193873733 citedByCount "3" @default.
• W3193873733 countsByYear W31938737332022 @default.
• W3193873733 countsByYear W31938737332023 @default.
• W3193873733 crossrefType "journal-article" @default.
• W3193873733 hasAuthorship W3193873733A5033439167 @default.
• W3193873733 hasAuthorship W3193873733A5049875261 @default.
• W3193873733 hasAuthorship W3193873733A5069267886 @default.
• W3193873733 hasBestOaLocation W31938737331 @default.
• W3193873733 hasConcept C117485682 @default.
• W3193873733 hasConcept C120806208 @default.
• W3193873733 hasConcept C127313418 @default.
• W3193873733 hasConcept C13495919 @default.
• W3193873733 hasConcept C135559958 @default.
• W3193873733 hasConcept C146481406 @default.
• W3193873733 hasConcept C151730666 @default.

• next