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Abstract
Paleomagnetic Results from the Perij Mountains, Venezuela: An Example of Vertical Axis Rotation
Wulf A. Gose,1 Adrin Perarnau,2 Jess Castillo3
1Department of Geological Sciences, The University of Texas at Austin, Austin, Texas, U.S.A.
2Departamento de Fsica, Universidad Simn Bolvar, Caracas, Venezuela; Current affiliation: Baker Atlas, Maturin, Venezuela.
3Departamento de Fsica, Universidad Simn Bolvar, Caracas, Venezuela
ACKNOWLEDGMENTS
Fieldwork for this project was done in 1988 through 1990. We appreciate the support of National Science Foundation (INT-8608620) and CONICIT (Venezuela) and the supplemental funding by the Melon Foundation. We benefited from discussions with many Venezuelan researchers, particularly Felipe Audemard, and we thank Brooks Ellwood and Bill MacDonald for thoughtful reviews.
ABSTRACT
Paleomagnetic analyses of 161 samples of Jurassic through Eocene age from 11 sites in the Venezuelan foothills of the Perij Mountains yield a pole position at 44.1 N, 6.6 E with an error of A95 = 9.6. These data indicate that the sampling sites underwent a 50 12 clockwise rotation. The rotations are interpreted to be the result of Neogene compression, which caused the rotation of fault-bounded blocks. Model calculations suggest a shortening between 8 km and 20 km across the eastern portion of the Perij Mountains.
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