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  • Open Daily: 10am - 10pm
    Alley-side Pickup: 10am - 7pm

    3038 Hennepin Ave Minneapolis, MN
    612-822-4611

Open Daily: 10am - 10pm | Alley-side Pickup: 10am - 7pm
3038 Hennepin Ave Minneapolis, MN
612-822-4611
Paleomagnetic Rotations and Continental Deformation

Paleomagnetic Rotations and Continental Deformation

Kissel, Catherine
Laj, Carlo

Paperback

Series: NATO Science Series C:, Book 254

General GardeningGeologyPhysics

ISBN10: 940106878X
ISBN13: 9789401068789
Publisher: Springer Nature
Published: Sep 26 2011
Pages: 530
Weight: 1.64
Height: 1.08 Width: 6.14 Depth: 9.21
Language: English
One of the most interesting results obtained in the last two decades in the study of crustal deformation has been the recognition that large regions of continental crust undergo rotations about vertical axis during deformation. Proof of such rotations has come through the paleomagnetic studies, which reveal rotations when paleomagnetic declinations within the deforming region arc compared with those found in coeval rocks in the stable regions outside the deforming zone. Such rotations were first described in Oregon then in the North American Cordilleras and in Southern California and were a surprise to everyone. Even in California which, as a result of oil exploration, was among the best geologically explored regions in the world, no one could claim to have predicted that these rotations would be found. Rotations have subsequently been found in other areas of recent continental tectonic activity, notably in the Basin and Range province, New Zealand, the Andes, Greece and Western Turkey, so that they appear as an important feature of continental deformation.

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