R., 1968, Magnetic anomalies in the Indian Ocean and sea-floor spreading, Journal of Geophysical Research, vol. 73, no. 6, p. 2101-2117.Le Pichon, X. and Heirtzler, J.R.. 1968. Magnetic anomalies in the Indian Ocean and sea-floor spreading. J. Geophys. Res.. 73: 21Oll2117....
R., 1968, Magnetic anomalies in the South Atlantic and ocean floor spreading: J. Geophys. Res ., v. 73, n. 6.Dickson, G. O., Pitman. W. C., III. and Heirtzler, J. R., 1968, .Magnetic anomalies in the South Atlantic and ocean floor spreading: Jour. Geophys. Research, v. ...
Magnetic anomalies are bands of rock that run parallel to the mid-ocean ridge system. What do they provide evidence for? A. Bacteria lived in the ocean floor millions of years ago B. Volcanoes form at ocean ridges. C. The sea floor was formed in stripes D. Granite is...
By tracing these magnetic anomalies along the ocean floor, scientists have found a total of 183 pole reversals, just in the past 83 million years. Content continues below In that same 83 million years, however, we have...
ocean floormagnetic anomaliesstrongly magnetised basalts/ A9125 Geomagnetism and geoelectricity A9210 Physics of the oceansSTRONGLY magnetised basalts occur at the basement surface in ridge crest areas (see, for example, refs 1, 2) and various models for the magnetic sources have been devised. A ...
Identifying marine magnetic anomalies is the most common way to date the ocean floor. Although the technique of magnetic anomaly identification has not changed since the 1960s, a forward modeling software that is easy to use, fast and automatic, without abstruse parameters, was lacking. We present...
The most widely known example of the utility of the field is its role in deciphering the process of seafloor spreading through the recognition of alternately normally and reversely magnetized rock stripes on the ocean floor (see Magnetic anomalies, marine ; Magnetic anomalies for geology and ...
The most widely known example of the utility of the field is its role in deciphering the process of seafloor spreading through the recognition of alternately normally and reversely magnetized rock stripes on the ocean floor (see Magnetic anomalies, marine ; Magnetic anomalies for geology and ...
The transition zones in this layer are broad, sloping boundaries reflecting the delayed acquisition of magnetization with depth as, for example, along a sloping Curie point isotherm. The lower layer can account for a skewness discrepancy of 10°–15° in the observed skewness of some anomalies. ...
Magnetic anomalies in the South Atlantic and ocean floor spreading Magnetic profiles across the South Atlantic Ocean from the Rio Grande rise and Argentine basin to the southwest coast of Africa and between 25掳 and 50掳S ... GO Dickson,WC Pitman,JR Heirtzler - 《Journal of Geophysical Resear...