ISSN:
1365-246X
Source:
Blackwell Publishing Journal Backfiles 1879-2005
Topics:
Geosciences
Notes:
A total of 151 oriented samples were drilled out of 14 basaltic flows southwest of Harrat Rahat (22.1°N, 39.3°E). Ar39/Ar40 age determinations for these flows range between 3.3 ± 0.17 and 3.73 ± 0.16 Ma. Microscopic observations of 56 thin, and polished sections indicate a secondary crystallization of very fine grained magnetite and iddingsite at the boundaries and along microfractures in the olivine crystals. These single to multi-domain crystals produce a strong secondary magnetization unstable against alternating field demagnetization. The mean direction of these magnetic overprints is: D= 345.4, I= 28.0, α95 = 16.4, k= 32.3, n= 4 (sites) yielding a mean palaeopole at: 285.5°E, 74.4°N, A95 = 14.1, K= 34.5, N= 4. The stable remanent magnetization of all the samples is of reverse polarity and has a mean direction: D= 168.7, I= 38.8, α95 = 3.7, k= 114.5, n= 14, yielding a mean palaeomagnetic pole position at: 310.4°E, 80.0°N, A95 = 3.9, K= 102.6, N= 14. These data, together with other data for the Arabian plate were used to construct a preliminary apparent pole wander path (APWP) for Arabia during the Tertiary. The APWPs for Africa and Arabia during the Tertiary were constructed. Comparison of the Arabic and African APWPs indicate high mobility during the Miocene to Holocene, but the APWPs are in agreement with each other after proper reconstruction of Arabia to Africa.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1111/j.1365-246X.1989.tb02051.x
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