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Geology; October 1992; v. 20; no. 10; p. 935-938; DOI: 10.1130/0091-7613(1992)020<0935:PEOTTR>2.3.CO;2
© 1992 Geological Society of America
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Paleomagnetic evidence of Tertiary tectonic rotation in west Texas

William W. Sager1, Carlos A. Mortera-Gutierrez2 and Jaime Urrutia-Fucugauchi3

1 Departments of Oceanography and Geophysics, Texas A&M University, College Station, Texas 77843
2 Department of Geophysics, Texas A&M University, College Station, Texas 77843
3 Instituto de Geofisica, Universidad Nacional Autónoma de México, 04510 Delegació n Coyoacan, D.F., México

Paleomagnetic samples obtained from Rawls Formation (26.9-28.3 Ma) lava flows of Bofecillos volcano in west Texas give a paleomagnetic pole at lat 76.5°N, long 348.0°E ({alpha}95 = 9.4°; N = 20). This pole is displaced significantly from North American reference poles of similar age, implying a clockwise rotation of 21.3° ± 8.8°. It is also consistent with other paleomagnetic data from west Texas. We argue that the discordance is a result of vertical-axis crustal rotation in west Texas caused by shear deformation that was probably related to Basin and Range tectonics.







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