Eocene red sandstones were collected at 15 sites for paleomagnetic study from two areas (Lanping and Yunlong) of the western part of Yunnan province, China, in the northern part of Indochina. The high-temperature magnetization component with an unblocking temperature of around 680oC is isolated after stepwise thermal demagnetization. Characteristic directions from nine accepted sites reveal a positive fold test at the 99% confidence limit, indicating that the high-temperature magnetization component is possibly of Eocene age. A tilt-corrected mean direction from nine accepted sites is D=266.1o, I=-39.8o with alpha95=11.2o, corresponding to a paleopole at 14.5oN, 169.7oE with A95=10.9o. A comparison with previously reported Tertiary paleomagnetic data indicates that the Lanping basin of the northern part of the Indochina block rotated clockwise through 91o (+/-15o) with respect to the Yangtze craton. This large magnitude clockwise rotation is probably caused by the superimposition of regional and local rotations. Our previous middle Cretaceous paleomagnetic results from the Yunlong area indicate that about 40o of clockwise rotation out of 90o is explained by tectonic rotation due to a relatively rigid body rotation of the Simao Terrane during indentation of India. The remaining component of rotation is probably ascribed to further Eocene/post-Eocene rotational motion of the tectonically independent small blocks within the Lanping basin associated with fault movement.
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