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- W2054221471 abstract "Paleomagnetic study of two stratigraphic sections of the Upper Silurian-Lower Devonian Ringerike Sandstone, Oslo area, Norway, indicate a straightforward multicomponent NRM for these rocks. A lower temperature magnetization component gives a southwest and up (reversed polarity) in-situ direction, yields a negative fold test (i.e. post-folding) at the 99% confidence level, and is nearly identical to directions obtained from overlying Permo-Carboniferous lavas. A high temperature magnetization component exhibits both normal and reversed polarity directions, passes a fold test at the 95% confidence level, and is supported by a baked contact test which indicates a pre-intrusion age of magnetization. This characteristic high temperature component was successfully isolated in 79 samples, from 19 sites within the Ringerike succession. Results indicate a tilt corrected, characteristic magnetic direction of declination = 26°, inclination = −16°, which is consistent with earlier work. This direction corresponds to a time-integrated paleopole position of 19°N latitude, 164° longitude (dp = 4.8°, dm = 9.3°). When compared to previous results from rocks of similar age from the British Isles, an approximately 20° latitudinal displacement between Britain and Baltica during Late Silurian-Early Devonian time is suggested." @default.
- W2054221471 created "2016-06-24" @default.
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- W2054221471 date "1988-04-01" @default.
- W2054221471 modified "2023-10-04" @default.
- W2054221471 title "Paleomagnetics of Ringerike Old Red Sandstone and related rocks, southern Norway: implications for pre-Carboniferous separation of Baltica and British terranes" @default.
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- W2054221471 doi "https://doi.org/10.1016/0040-1951(88)90157-6" @default.
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