Abstract
Two oppositely directed secondary directions of magnetization were isolated from some of the dikes in the Esh El Mellaha Range. Radiometric and paleomagnetic age considerations suggest that these were acquired during an interval of low-grade metamorphism in late Cambrian time (approx. 530 m.y.). The paleopole position for the acidic dikes (three sites) is 87.3N 25.9E dp 9.6, dm 14.5, for the intermediate dikes (eight sites) 81.6N 120.8E dp 3.3 dm 5.2 and for the basic dikes (11 sites) 82.7N 86.5W dp 5.6 dm 9.1.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
