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- W4254358949 abstract "Positions on the globe are given by the colatitude (θ) and the longitude (∅), measured from the north geographical pole and from the Greenwich meridian eastwards, respectively.The declination of the geomagnetic field or a palaeomagnetic direction (D ) is measured from the geographical meridian eastwards and the inclination (I) (the term * angle of dip ’ is not used here because of possible confusion with the term ‘geological dip’) is measured from the horizontal plane, positive if the north-seeking pole is below the horizon, negative if it is above." @default.
- W4254358949 created "2022-05-12" @default.
- W4254358949 date "1957-08-29" @default.
- W4254358949 modified "2023-10-18" @default.
- W4254358949 title "Palaeomagnetic investigations in Great Britain" @default.
- W4254358949 doi "https://doi.org/10.1098/rsta.1957.0011" @default.
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