The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …

Mudrocks have varied composition and texture, and heterogeneous nano to micro-scale
pore assemblages, and therefore show distinctly different well log responses. A better …

Abstract The Tibetan Plateau accommodated major upper crustal shortening during Indian
Plate oceanic and continental lithosphere subduction. Deciphering whether shortening was …

The timing of onset of deposition of the Lulehe Formation is a significant factor in
understanding the genesis of the Qaidam basin and the evolution of the Tibetan Plateau …

Oligocene-Miocene convergence of the Eurasian and Arabian plates resulted in (i) the
gradual closure of the Neo-Tethys Ocean that formed an open marine connection between …

The northward indentation of the Pamir salient into the Tarim basin at the western syntaxis of
the India‐Asia collision zone is the focus of controversial models linking lithospheric to …

Kinematic reconstruction of modern ocean basins shows that since Pangea breakup a vast
area in the Neotethyan realm was lost to subduction. Here we develop a first‐order …

The Cenozoic evolution of the Qaidam basin, especially its paleostress field, can provide a
better understanding of the dynamistic process of the northern Tibetan Plateau. Under …

The precollisional locations and geometries of the Lhasa terrane (LT) are critical to constrain
the India‐Asia collision. However, the inclinations of the Cretaceous paleomagnetic data …

Knowing the rotation and paleo-stress history in Qaidam Basin is a fundamental parameter
to quantify the mechanism of intracontinental deformation in Tibetan Plateau. However, few …