Based on the marine magnetic anomalies identified in the Argo Abyssal Plain offshore
northwestern Australia, the conceptual continent of Argoland must have rifted off in the Late …

The drift history of the Lhasa terrane from Gondwana to Asia plays a crucial role in
understanding the Tethys evolution and true polar wander (TPW). However, few reliable …

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 …

True polar wander (TPW), or planetary reorientation, is the rotation of solid Earth (crust and
mantle) about the liquid outer core in order to stabilize Earth's rotation due to mass …

Abstract The Lhasa‐Qiangtang collision closed the Meso‐Tethys Ocean, but the exact timing
of this event remains hotly debated. Here, we present geochronological and paleomagnetic …

The reorientation of Earth through rotation of its solid shell relative to its spin axis is known
as True polar wander (TPW). It is well-documented at present, but the occurrence of TPW in …

To constrain the paleolatitude evolution and orientation of the Lhasa terrane in the
Cretaceous, we performed a paleomagnetic study on the Qushenla Formation volcanic …

The paleogeography of the Tethyan Himalaya (TH) during the Mesozoic is vital to constrain
the evolutionary history of the Neo‐Tethys Ocean, but reliable paleomagnetic data from …

Understanding the dynamics of the uplift of the Tibetan blocks requires constraints on the
timing and magnitude of the crustal shortening accommodated by the different blocks …

Carbonate rocks, widely used for quantifying paleolatitude of the Gondwana‐derived
terranes on the Tibetan Plateau and the geodynamic evolution of the Tethyan Oceans, are …