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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Altyn Tagh Fault
Lithospheric Structure of the Central Altyn Tagh Fault System Revealed by Teleseismic Travel‐Time Tomography Available to Purchase
Landform evolution of the Qilian Shan since 120 Ma revealed by apatite fission track data Available to Purchase
Cenozoic dextral transpressional tectonics in the northwestern Qaidam Basin, northern Tibet: Evidence from paleomagnetic and kinematic analysis of the arcuate belts Available to Purchase
Observation of Higher‐Mode Rayleigh Waves from Ambient Noise in the Tarim Basin, China Available to Purchase
The newly discovered ca. 1.35 Ga metamafic rocks in the Oulongbuluke Block, NW China, and its record for transition from the Columbia to Rodinia supercontinent Available to Purchase
Jurassic Provenance System and Its Geological Implication in Altyn Piedmont, Qaidam Basin Open Access
Late Quaternary slip rate of the Aksay segment and its rapidly decreasing gradient along the Altyn Tagh fault Open Access
Source Model of the 2014 M w 6.9 Yutian Earthquake at the Southwestern End of the Altyn Tagh Fault in Tibet Estimated from Satellite Images Available to Purchase
Characteristic slip distribution and earthquake recurrence along the eastern Altyn Tagh fault revealed by high-resolution topographic data Open Access
Segmentation and termination of the surface rupture zone produced by the 1932 Ms 7.6 Changma earthquake: New insights into the slip partitioning of the eastern Altyn Tagh fault system Open Access
Exploring the theory of plate tectonics: the role of mantle lithosphere structure Available to Purchase
Abstract This review of the role of the mantle lithosphere in plate tectonic processes collates a wide range of recent studies from seismology and numerical modelling. A continually growing catalogue of deep geophysical imaging has illuminated the mantle lithosphere and generated new interpretations of how the lithosphere evolves. We review current ideas about the role of continental mantle lithosphere in plate tectonic processes. Evidence seems to be growing that scarring in the continental mantle lithosphere is ubiquitous, which implies a reassessment of the widely held view that it is the inheritance of crustal structure only (rather than the lithosphere as a whole) that is most important in the conventional theory of plate tectonics (e.g. the Wilson cycle). Recent studies have interpreted mantle lithosphere heterogeneities to be pre-existing structures and, as such, linked to the Wilson cycle and inheritance. We consider the current fundamental questions in the role of the mantle lithosphere in causing tectonic deformation, reviewing recent results and highlighting the potential of the deep lithosphere in infiltrating every aspect of plate tectonics processes.