FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000367104> ?p ?o ?g. }

• W2000367104 endingPage "4884" @default.
• W2000367104 startingPage "4875" @default.
• W2000367104 abstract "The magnetic basement topography and associated magnetic anomaly lineation pattern in an area north of the New England seamounts lying between anomaly 31 and the continental margin were examined in light of the Mesozoic sea floor spreading history of the northwest Atlantic. Within the magnetic quiet zone the crust is typically oceanic as far landward as the slope anomaly and exhibits a normally polarized magnetism in the inner quiet zone. Magnetic lineations have been correlated with the Keathley sequence near Bermuda, and, based upon best estimates of the reversal time scale, cross-strike spreading rates are found to be about 1.7 cm yr−1 from −172 m.y. to −136 m.y. and between 0.9 and 1.0 cm yr−1 from −136 m.y. to −72 m.y. Landward of the Keathley sequence, magnetic anomalies decrease in amplitude, although the intensity of magnetization of the normally polarized crust exhibits average values. Magnetic observations within a large area of the quiet zone surveyed in detail can be fitted to the basement topography if a Jurassic pole position of normal polarity is assumed. However, three zones trending subparallel to the Keathley lineations require a weak reversely polarized magnetism. These low values of remanent magnetization are attributed to either viscous remanence or contamination of the original crust by widespread volcanic flows or intrusives during periods of predominantly normal magnetic polarity. The normal and reversed polarity sequence resulting from this study is correlated with the sequence obtained from paleomagnetic measurements on land. Trends of isochrons within this relatively limited oceanic area necessitate an alteration in the shape of the ridge axis. A difference in spreading rate and direction is obvious on either side of the New England seamount chain and is discussed with respect to the history of early plate motions in the northwest Atlantic." @default.
• W2000367104 created "2016-06-24" @default.
• W2000367104 creator A5062911352 @default.
• W2000367104 creator A5086312204 @default.
• W2000367104 date "1976-09-10" @default.
• W2000367104 modified "2023-10-18" @default.
• W2000367104 title "Mesozoic magnetic lineations, the magnetic quiet zone, and sea floor spreading in the northwest Atlantic" @default.
• W2000367104 cites W152287421 @default.
• W2000367104 cites W1978185779 @default.
• W2000367104 cites W2001197696 @default.
• W2000367104 cites W2002137158 @default.
• W2000367104 cites W2015876749 @default.
• W2000367104 cites W2027477351 @default.
• W2000367104 cites W2032937009 @default.
• W2000367104 cites W2035504541 @default.
• W2000367104 cites W2036066930 @default.
• W2000367104 cites W2037560001 @default.
• W2000367104 cites W2040272748 @default.
• W2000367104 cites W2046075128 @default.
• W2000367104 cites W2049218281 @default.
• W2000367104 cites W2056861878 @default.
• W2000367104 cites W2070941721 @default.
• W2000367104 cites W2076514905 @default.
• W2000367104 cites W2081371532 @default.
• W2000367104 cites W2120954655 @default.
• W2000367104 cites W2131279760 @default.
• W2000367104 cites W2136629436 @default.
• W2000367104 cites W2158710069 @default.
• W2000367104 cites W2163871679 @default.
• W2000367104 cites W2170386708 @default.
• W2000367104 cites W2487169387 @default.
• W2000367104 cites W990867378 @default.
• W2000367104 doi "https://doi.org/10.1029/jb081i026p04875" @default.
• W2000367104 hasPublicationYear "1976" @default.
• W2000367104 type Work @default.
• W2000367104 sameAs 2000367104 @default.
• W2000367104 citedByCount "65" @default.
• W2000367104 countsByYear W20003671042012 @default.
• W2000367104 countsByYear W20003671042015 @default.
• W2000367104 countsByYear W20003671042016 @default.
• W2000367104 countsByYear W20003671042017 @default.
• W2000367104 countsByYear W20003671042021 @default.
• W2000367104 countsByYear W20003671042023 @default.
• W2000367104 crossrefType "journal-article" @default.
• W2000367104 hasAuthorship W2000367104A5062911352 @default.
• W2000367104 hasAuthorship W2000367104A5086312204 @default.
• W2000367104 hasConcept C115260700 @default.
• W2000367104 hasConcept C121332964 @default.
• W2000367104 hasConcept C127313418 @default.
• W2000367104 hasConcept C141646446 @default.
• W2000367104 hasConcept C151730666 @default.
• W2000367104 hasConcept C152406496 @default.
• W2000367104 hasConcept C154200439 @default.
• W2000367104 hasConcept C155058782 @default.
• W2000367104 hasConcept C165205528 @default.
• W2000367104 hasConcept C189479680 @default.
• W2000367104 hasConcept C194482375 @default.
• W2000367104 hasConcept C2776698055 @default.
• W2000367104 hasConcept C32546565 @default.
• W2000367104 hasConcept C58097730 @default.
• W2000367104 hasConcept C62520636 @default.
• W2000367104 hasConcept C77928131 @default.
• W2000367104 hasConcept C8058405 @default.
• W2000367104 hasConcept C98742433 @default.
• W2000367104 hasConceptScore W2000367104C115260700 @default.
• W2000367104 hasConceptScore W2000367104C121332964 @default.
• W2000367104 hasConceptScore W2000367104C127313418 @default.
• W2000367104 hasConceptScore W2000367104C141646446 @default.
• W2000367104 hasConceptScore W2000367104C151730666 @default.
• W2000367104 hasConceptScore W2000367104C152406496 @default.
• W2000367104 hasConceptScore W2000367104C154200439 @default.
• W2000367104 hasConceptScore W2000367104C155058782 @default.
• W2000367104 hasConceptScore W2000367104C165205528 @default.
• W2000367104 hasConceptScore W2000367104C189479680 @default.
• W2000367104 hasConceptScore W2000367104C194482375 @default.
• W2000367104 hasConceptScore W2000367104C2776698055 @default.
• W2000367104 hasConceptScore W2000367104C32546565 @default.
• W2000367104 hasConceptScore W2000367104C58097730 @default.
• W2000367104 hasConceptScore W2000367104C62520636 @default.
• W2000367104 hasConceptScore W2000367104C77928131 @default.
• W2000367104 hasConceptScore W2000367104C8058405 @default.
• W2000367104 hasConceptScore W2000367104C98742433 @default.
• W2000367104 hasIssue "26" @default.
• W2000367104 hasLocation W20003671041 @default.
• W2000367104 hasOpenAccess W2000367104 @default.
• W2000367104 hasPrimaryLocation W20003671041 @default.
• W2000367104 hasRelatedWork W1904986766 @default.
• W2000367104 hasRelatedWork W1999697500 @default.
• W2000367104 hasRelatedWork W2040041774 @default.
• W2000367104 hasRelatedWork W2048372491 @default.
• W2000367104 hasRelatedWork W2050249216 @default.
• W2000367104 hasRelatedWork W2052199633 @default.
• W2000367104 hasRelatedWork W2093888945 @default.
• W2000367104 hasRelatedWork W2147270527 @default.
• W2000367104 hasRelatedWork W287664748 @default.
• W2000367104 hasRelatedWork W2993751311 @default.
• W2000367104 hasVolume "81" @default.
• W2000367104 isParatext "false" @default.

• next