Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …

Anisotropy of magnetic susceptibility (AMS) was recognized as a feature of minerals in 1899,
and petrofabric-compatible AMS fabrics were reported from 1942–1958. Shortly thereafter …

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 …

Magnetostratigraphic and rock magnetic results from 1006 horizons in Paleogene and
Neogene sediments between the upper Kumugeliemu Formation and the base of the Kuche …

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 …

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 Pamir plateau forms a prominent tectonic salient that marks the western end of the
Himalayan orogen containing several terranes that were accreted to Eurasia from the Late …

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 …

In this work we compare the results of anisotropy of magnetic susceptibility (AMS) with
palaeostress analysis at local scale. The AMS data refer to 14 sites from weakly deformed …