Matches in SemOpenAlex for { <https://semopenalex.org/work/W2040272748> ?p ?o ?g. }
- W2040272748 endingPage "224" @default.
- W2040272748 startingPage "207" @default.
- W2040272748 abstract "Intensities of natural remanent magnetization compiled for 177 subaerial basaltic flows ranging from historical time to 10 My and for 204 submarine basalt samples from the North Atlantic basement show that subaerial basalts have a mean intensity, reduced to an equatorial equivalent value, of 36 × 10−4 emu cm−3, about 2·5 times weaker than for submarine basalts (89·6 × 10−4 emu cm−3). Normally magnetized flows have significantly greater NRM than reversed flows owing to a viscous component that represents about one-fifth of the stable remanence. No significant difference appears in the mean intensity between the Brunhes basalts and the older normal basalts or between the intensity, after partial demagnetization, of historic basalts and those ranging from 0·01 to 1, 1 to 2, 2 to 3, or 3 to 4 My. This seems to indicate (i) that no important decrease of the intensity of magnetization of subaerial basalts takes place for periods of several million years, and (ii) that a possible increase of the intensity of the geomagnetic field during the Brunhes epoch is not responsible for the larger amplitude of the axial magnetic anomaly over mid-ocean ridges. For the oceanic basement, the mean intensity decreases by about two-thirds from the basalts of the bottom of the median valley to the basalts from the crests and flanks of the ridge. This diminution, probably produced by intensive low-temperature oxidation of titanomagnetite, is comparable to the decrease of the magnetic anomalies observed in the North Atlantic when going away from the ridge axis." @default.
- W2040272748 created "2016-06-24" @default.
- W2040272748 creator A5049713123 @default.
- W2040272748 creator A5058652009 @default.
- W2040272748 date "1975-02-01" @default.
- W2040272748 modified "2023-10-14" @default.
- W2040272748 title "Intensity of Magnetization of Subaerial and Submarine Basalts and its Possible Change with Time" @default.
- W2040272748 cites W1693558092 @default.
- W2040272748 cites W1974109556 @default.
- W2040272748 cites W1977156846 @default.
- W2040272748 cites W1991661691 @default.
- W2040272748 cites W2000031188 @default.
- W2040272748 cites W2001478521 @default.
- W2040272748 cites W2001843504 @default.
- W2040272748 cites W2009988234 @default.
- W2040272748 cites W2016659885 @default.
- W2040272748 cites W2022777953 @default.
- W2040272748 cites W2022956894 @default.
- W2040272748 cites W2030216780 @default.
- W2040272748 cites W2033730095 @default.
- W2040272748 cites W2039026488 @default.
- W2040272748 cites W2053404792 @default.
- W2040272748 cites W2061317292 @default.
- W2040272748 cites W2062349922 @default.
- W2040272748 cites W2067689144 @default.
- W2040272748 cites W2073394204 @default.
- W2040272748 cites W2074049528 @default.
- W2040272748 cites W2079035957 @default.
- W2040272748 cites W2084274947 @default.
- W2040272748 cites W2088789430 @default.
- W2040272748 cites W2092021792 @default.
- W2040272748 cites W2104332376 @default.
- W2040272748 cites W2105642936 @default.
- W2040272748 cites W2113298283 @default.
- W2040272748 cites W2122695340 @default.
- W2040272748 cites W2122806043 @default.
- W2040272748 cites W2124077998 @default.
- W2040272748 cites W2135897987 @default.
- W2040272748 cites W2141831807 @default.
- W2040272748 cites W2143145176 @default.
- W2040272748 cites W2145844826 @default.
- W2040272748 cites W2148472374 @default.
- W2040272748 cites W2151593792 @default.
- W2040272748 cites W2167856353 @default.
- W2040272748 doi "https://doi.org/10.1111/j.1365-246x.1975.tb07047.x" @default.
- W2040272748 hasPublicationYear "1975" @default.
- W2040272748 type Work @default.
- W2040272748 sameAs 2040272748 @default.
- W2040272748 citedByCount "45" @default.
- W2040272748 countsByYear W20402727482012 @default.
- W2040272748 countsByYear W20402727482013 @default.
- W2040272748 crossrefType "journal-article" @default.
- W2040272748 hasAuthorship W2040272748A5049713123 @default.
- W2040272748 hasAuthorship W2040272748A5058652009 @default.
- W2040272748 hasConcept C115260700 @default.
- W2040272748 hasConcept C121332964 @default.
- W2040272748 hasConcept C127313418 @default.
- W2040272748 hasConcept C155058782 @default.
- W2040272748 hasConcept C161509811 @default.
- W2040272748 hasConcept C17409809 @default.
- W2040272748 hasConcept C194482375 @default.
- W2040272748 hasConcept C32546565 @default.
- W2040272748 hasConcept C62520636 @default.
- W2040272748 hasConcept C66944017 @default.
- W2040272748 hasConcept C8058405 @default.
- W2040272748 hasConcept C84983702 @default.
- W2040272748 hasConcept C93038891 @default.
- W2040272748 hasConceptScore W2040272748C115260700 @default.
- W2040272748 hasConceptScore W2040272748C121332964 @default.
- W2040272748 hasConceptScore W2040272748C127313418 @default.
- W2040272748 hasConceptScore W2040272748C155058782 @default.
- W2040272748 hasConceptScore W2040272748C161509811 @default.
- W2040272748 hasConceptScore W2040272748C17409809 @default.
- W2040272748 hasConceptScore W2040272748C194482375 @default.
- W2040272748 hasConceptScore W2040272748C32546565 @default.
- W2040272748 hasConceptScore W2040272748C62520636 @default.
- W2040272748 hasConceptScore W2040272748C66944017 @default.
- W2040272748 hasConceptScore W2040272748C8058405 @default.
- W2040272748 hasConceptScore W2040272748C84983702 @default.
- W2040272748 hasConceptScore W2040272748C93038891 @default.
- W2040272748 hasIssue "2" @default.
- W2040272748 hasLocation W20402727481 @default.
- W2040272748 hasOpenAccess W2040272748 @default.
- W2040272748 hasPrimaryLocation W20402727481 @default.
- W2040272748 hasRelatedWork W1977165140 @default.
- W2040272748 hasRelatedWork W1997003100 @default.
- W2040272748 hasRelatedWork W2018376393 @default.
- W2040272748 hasRelatedWork W2040272748 @default.
- W2040272748 hasRelatedWork W2054281412 @default.
- W2040272748 hasRelatedWork W2123343313 @default.
- W2040272748 hasRelatedWork W2138118634 @default.
- W2040272748 hasRelatedWork W2157366305 @default.
- W2040272748 hasRelatedWork W2286328395 @default.
- W2040272748 hasRelatedWork W2315566686 @default.
- W2040272748 hasVolume "40" @default.
- W2040272748 isParatext "false" @default.
- W2040272748 isRetracted "false" @default.
- W2040272748 magId "2040272748" @default.