FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2009644474> ?p ?o ?g. }

• W2009644474 endingPage "4855" @default.
• W2009644474 startingPage "4833" @default.
• W2009644474 abstract "Sea surface, deep tow, and submersible magnetic surveys show that the spreading axis of the Cleft segment of the southern Juan de Fuca Ridge (SJDF) is overlain by a distinctive magnetic anomaly low in contrast to the more typical magnetic anomaly high found over the adjacent Vance segment and most mid‐ocean ridge spreading centers. Forward iterative thickness modeling, based on the near‐bottom magnetic data, shows that this axial magnetic low can be produced by a thin magnetic source layer beneath the Cleft axial valley. Thick crust is required to produce the magnetic anomaly high over the Vance axial valley. This magnetic modeling demonstrates that variations in the base of the magnetic source layer, which is assumed to be equivalent to the base of the extrusive lavas, can produce a significant proportion of the observed short‐wavelength magnetic anomaly signal. These magnetic layer thickness models also correlate quite well with nearby seismic results which show that seismic layer 2A thins beneath the axial valley of the Cleft and is thicker beneath the Vance axial valley. Recent seismic results over other fast and medium spreading rifts also show rapid changes in the thickness of the uppermost crust near the axis of spreading, which could produce significant magnetic contrasts. The results of this study and the correlation with independent seismic measurements suggest that while magnetization may vary due to geomagnetic behavior or because of petrology or alteration, first‐order change in upper crustal thickness is one of the most important variables to consider in the production of fine‐scale magnetic anomalies in young ocean crust." @default.
• W2009644474 created "2016-06-24" @default.
• W2009644474 creator A5020258837 @default.
• W2009644474 date "1994-03-10" @default.
• W2009644474 modified "2023-10-13" @default.
• W2009644474 title "Fine‐scale magnetic anomaly field over the southern Juan de Fuca Ridge: Axial magnetization low and implications for crustal structure" @default.
• W2009644474 cites W1562792385 @default.
• W2009644474 cites W1970187426 @default.
• W2009644474 cites W1973057777 @default.
• W2009644474 cites W1974027425 @default.
• W2009644474 cites W1974677732 @default.
• W2009644474 cites W1975833725 @default.
• W2009644474 cites W1977003666 @default.
• W2009644474 cites W1978185779 @default.
• W2009644474 cites W1983574415 @default.
• W2009644474 cites W1985999749 @default.
• W2009644474 cites W1991923137 @default.
• W2009644474 cites W1998139838 @default.
• W2009644474 cites W1999139618 @default.
• W2009644474 cites W2001873873 @default.
• W2009644474 cites W2002128134 @default.
• W2009644474 cites W2003807291 @default.
• W2009644474 cites W2005805533 @default.
• W2009644474 cites W2007901832 @default.
• W2009644474 cites W2010477797 @default.
• W2009644474 cites W2011369995 @default.
• W2009644474 cites W2011472004 @default.
• W2009644474 cites W2012864958 @default.
• W2009644474 cites W2013266297 @default.
• W2009644474 cites W2013841428 @default.
• W2009644474 cites W2015195100 @default.
• W2009644474 cites W2015673714 @default.
• W2009644474 cites W2017114107 @default.
• W2009644474 cites W2018967094 @default.
• W2009644474 cites W2019309644 @default.
• W2009644474 cites W2023476433 @default.
• W2009644474 cites W2023488081 @default.
• W2009644474 cites W2027457863 @default.
• W2009644474 cites W2033961403 @default.
• W2009644474 cites W2041379122 @default.
• W2009644474 cites W2048137911 @default.
• W2009644474 cites W2051173566 @default.
• W2009644474 cites W2054969778 @default.
• W2009644474 cites W2065167475 @default.
• W2009644474 cites W2066242967 @default.
• W2009644474 cites W2067689144 @default.
• W2009644474 cites W2068641796 @default.
• W2009644474 cites W2073082793 @default.
• W2009644474 cites W2075531765 @default.
• W2009644474 cites W2079035957 @default.
• W2009644474 cites W2081969960 @default.
• W2009644474 cites W2082720347 @default.
• W2009644474 cites W2090311769 @default.
• W2009644474 cites W2090971241 @default.
• W2009644474 cites W2099704063 @default.
• W2009644474 cites W2108511180 @default.
• W2009644474 cites W2108979485 @default.
• W2009644474 cites W2122671476 @default.
• W2009644474 cites W2134720473 @default.
• W2009644474 cites W2135716982 @default.
• W2009644474 cites W2141388451 @default.
• W2009644474 cites W2146162649 @default.
• W2009644474 cites W2148472374 @default.
• W2009644474 cites W2149988268 @default.
• W2009644474 cites W2153199248 @default.
• W2009644474 cites W2154082181 @default.
• W2009644474 cites W2160121796 @default.
• W2009644474 cites W2167696014 @default.
• W2009644474 cites W2170262481 @default.
• W2009644474 cites W2498860691 @default.
• W2009644474 cites W2917902622 @default.
• W2009644474 cites W966629307 @default.
• W2009644474 doi "https://doi.org/10.1029/93jb02110" @default.
• W2009644474 hasPublicationYear "1994" @default.
• W2009644474 type Work @default.
• W2009644474 sameAs 2009644474 @default.
• W2009644474 citedByCount "34" @default.
• W2009644474 countsByYear W20096444742014 @default.
• W2009644474 countsByYear W20096444742016 @default.
• W2009644474 countsByYear W20096444742022 @default.
• W2009644474 crossrefType "journal-article" @default.
• W2009644474 hasAuthorship W2009644474A5020258837 @default.
• W2009644474 hasConcept C115260700 @default.
• W2009644474 hasConcept C117485682 @default.
• W2009644474 hasConcept C121332964 @default.
• W2009644474 hasConcept C127313418 @default.
• W2009644474 hasConcept C12997251 @default.
• W2009644474 hasConcept C151730666 @default.
• W2009644474 hasConcept C165205528 @default.
• W2009644474 hasConcept C194482375 @default.
• W2009644474 hasConcept C199635899 @default.
• W2009644474 hasConcept C26873012 @default.
• W2009644474 hasConcept C2776698055 @default.
• W2009644474 hasConcept C32277403 @default.
• W2009644474 hasConcept C32546565 @default.
• W2009644474 hasConcept C51151373 @default.
• W2009644474 hasConcept C62520636 @default.
• W2009644474 hasConcept C8058405 @default.

• next