New Middle Jurassic Paleomagnetic and Geochronologic Results From the Lhasa Terrane: Contributions to the Closure of the Meso-Tethys Ocean and Jurassic True Polar Wander

The drift history of the Lhasa terrane is crucial for understanding the tectonic evolution of Tethyan Oceans and Jurassic true polar wander. However, high-quality Middle Jurassic paleomagnetic data from the Lhasa terrane are limited in number. Here we report a combined paleomagnetic and geochronologic study on the Yeba Formation volcanic rocks, dated at similar to 170 Ma, from the Lhasa terrane. Robust field and reversal tests indicate that the characteristic remanent magnetizations are primary. Our results provide a reliable Middle Jurassic (similar to 170 Ma) paleopole at 29.8 degrees N, 180.7 degrees E with A(95) = 5.7 degrees and a paleolatitude of 14.4 +/- 5.7 degrees N for the Lhasa area. Compared with previous paleomagnetic and geologic evidence, we propose that the Meso-Tethys Ocean probably began to close in the eastern part at similar to 168 Ma and that the Lhasa terrane underwent a similar to 2,900 km southward "monster shift" during the Late Jurassic.