Paleomagnetic data constrain paleogeographic motion of rocks relative to the Earth's spin axis, which is a sum of plate motion relative to the mantle and true polar wander. Discerning between these effects is challenging for studies aiming to reconstruct paleo-plate motions from deformed orogenic terranes. Here, we study the paleolatitudinal drift history of the Lhasa terrane of southern Tibet that migrated from the northern Gondwana to the southern Eurasian margin between late Triassic and early Cretaceous time. Previous work identified a 180 Ma near-equatorial Lhasa latitude and assumed near-constant paleolatitudinal drift. Large-scale true polar wander at this time, however, which has been argued for in previous work, requires highly variable Lhasa plate motion rates relative to Gondwana. Here, we test whether the alternative interpretation of constant plate motion rates provides a better prediction of paleomagnetic data. To this end, we present a new paleomagnetic pole from ∼155 Ma volcanics (here dated by U/Pb zircon) of the Lhasa terrane. Our pole comprises site mean directions from 46 lavas, passes a fold test, and is supported by an extensive rock magnetic and microscopic analysis that reveals no evidence of remagnetization. Our results give an average direction of D ± Δ D x = 337.1 ° ± 2.6 ° , I ± Δ I x = − 13.8 ° ± 4.9 ° , and a corresponding paleopole position at λ p = 45.3 ° N, φ p = 295.3 ° E with K=69.8 and A 95 = 2.5 ° , predicting a similar near-equatorial, paleolatitude as at 180 Ma. This paleolatitudinal standstill is consistent with predicted paleolatitudes from global APWPs that account for Jurassic TPW and assume a constant Lhasa-Gondwana (India) oceanic spreading rate of ∼8 cm/a during the 215-130 Ma opening of the Neotethys and closure of the Mesotethys oceans. Contemporaneous arc magmatism on the Lhasa terrane was previously interpreted to indicate that the Lhasa terrane was located above a subduction zone during its northward journey to Tibet: our results show that if our reconstruction is accurate, then trench migration rates also must have been ∼8 cm/a. Our results are consistent with the range of rates of global long-lived trench migration that have been reconstructed in other studies, but they are much higher than measured in most modern systems. Our results more completely document the Lhasa terrane's separation from Gondwana and provide a straightforward methodology of using paleomagnetic data to test plate kinematic scenarios, overcoming the problem of the unknown effect of true polar wander on paleomagnetic data from deformed terranes. To better constrain the paleolatitude and paleogeography of the Lhasa terrane within Eastern Tethys realm in the Jurassic time, we used paleomagnetic and zircon U-Pb dating technique to try to give a quantitative constraint. To this end, we obtained a high-quality paleopole with well-dated age of 155 Ma from the Upper Jurassic-Lower Cretaceous Zenong Group volcanic rocks of the Lhasa terrane (southern Tibet). Based on this newly obtained paleopole, it predicts a similar paleolatitude as a recently published 61-lava based pole of 180 Ma of the Sangri volcanics, showing that the Lhasa terrane stayed at a southern hemisphere near-equatorial position over at least 25 Myr starting from 180 Ma up to 155 Ma, indicating a distinct stand-still feature for the Lhasa terrane during this time interval. On the other side, this paleolatitudinal stand-still is consistent with predicted paleolatitudes by global APWPs assuming a constant Lhasa-Gondwana (India) spreading rate during the 215-130 Ma opening of the Neotethys and closure of the Mesotethys oceans. We show that this Jurassic paleolatitudinal stand-still of the Lhasa terrane is readily explained by the interplay between true polar wander shifting Lhasa to the south and plate motion shifting Lhasa to the north. Finally, our results unlock the mobile Lhasa terrane and its overlying Jurassic magmatic record, as future study site to a proposed major, short-lived true polar wander event in the latest Jurassic and earliest Cretaceous. • A high-quality ∼155 Ma paleopole was obtained from the Zenong Group volcanics within central Lhasa terrane. • Zenong Group volcanics recorded paleolatitudinal standstill of Lhasa, which was ascribed to Jurassic True Polar Wander. • This recorded standstill of the Lhasa terrane is a sum of true polar wander and its northward plate tectonic motion.
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