How the present-day northern Tibetan Plateau was involved in the plateau formation
process in context of the Cenozoic India–Eurasia collision has been disputed for decades …

The high values of La/Yb (> 15–20) obtained from late Eocene to Pliocene volcanic rocks of
central Tibet indicate that source regions were in a thickened (> 35 km) crust. The higher …

We use the improved Parker‐Oldenburg's formulas that include a reference depth into the
exponential term and employ the Gauss‐fast Fourier transform method to determine Moho …

Two hyperparameters, the mean Moho depth and the Moho density contrast, must be
specified before the gravity inversion of Moho. Incorrect estimation will impact inversed …

We develop a novel gravity inversion algorithm in spherical coordinates based on adaptive
inversion mesh refinement and multiphysical parameter constraints. The inversion mesh is …

Abstract The Tibetan Plateau (TP) is the youngest orogenic belt resulting from a continental
collision on the Earth. It is a natural laboratory for studying continental dynamics, such as …

Although a large number of geophysical experiments have been performed in the Tibetan
plateau and its surroundings, our knowledge and understanding of the uplift and …

The uplift of the Qinghai–Tibet Plateau (TP) strongly influences climate change, both
regionally and globally. Surface observation data from this region have limited coverage and …

Uncertainty quantification is an important part of validation, because the pixel scale
reference generally suffers from uncertainty caused by different factors, lowering the …

We present a new Moho map for the north-eastern part of Eurasia, which remains almost
non-studied by seismic methods. The new map is based on the analysis of various data sets …