Paleogeographic maps are essential tools for understanding Earth system dynamics. They
provide boundary conditions for climate and geodynamic modelling, for analysing surface …

Key in understanding the geodynamics governing subduction and orogeny is reconstructing
the paleogeography of 'Greater India', the Indian plate lithosphere that subducted since …

The enigmatic geodynamic processes involved in the India-Asia collision shape our
understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes …

The Cenozoic inception and development of the Asian monsoons remain unclear and have
generated much debate, as several hypotheses regarding circulation patterns at work in …

A common feature of tectonic reconstructions is the migration of subduction zones and their
interactions, resulting in complex tectonic patterns. Reduced migration rates, uplift, strong …

The evolution of large fluvial drainages in SE Tibet and adjacent areas reflects the degree of
coupling between tectonics, erosion, and climate. Reconstruction of their spatio-temporal …

Abstract The Tibetan Plateau plays a crucial role in both Asian and global geomorphology
and climate dynamics. However, the precise mechanisms through which its deep …

Low-grade metamorphosed Cretaceous sedimentary records of forearc basin systems in the
eastern part of the Transhimalaya (Gangdese) arc system have not been reported yet …

The present study deals with detecting seismic anisotropy parameters beneath southeastern
Tibet near Namcha Barwa Mountain using the splitting of direct S waves. We employ the …

Subduction can pose a fundamental tectonic overprint on the overriding plate by generating
a variety of deformation patterns incorporating both extension and shortening strains. Latest …