Erosion of orogenic mountain ranges exhumes deeply buried rocks and controls
weathering, climate, and sediment production and transport at a variety of scales. Erosion …

Simple physical arguments, analogue experiments and numerical experiments all suggest
that the internal dynamics of actively deforming collisional mountain ranges are influenced …

Plane strain, thermal‐mechanical numerical models are used to examine the development
of midcrustal channel flows in large hot orogens. In the models, radioactive self‐heating …

The Himalayan range exposes a spectacular assemblage of metamorphic rocks from the
mid-and deep crust that have fostered numerous models of how the crust responds to …

Geomorphological mapping plays an essential role in understanding Earth surface
processes, geochronology, natural resources, natural hazards and landscape evolution. It …

摘要构造地貌学是发展迅速的新兴交叉学科, 与传统地貌学不同, 构造地貌学是一种定量地貌学,
强调对地貌过程的定量描述, 其核心概念是构造-气候-地表过程相互作用, 聚焦于以量化的方式 …

The channel flow model aims to explain features common to metamorphic hinterlands of
some collisional orogens, notably along the Himalaya-Tibet system. Channel flow describes …

Results from a thermal‐mechanical model (HT1) that includes midcrustal channel flow are
compatible with many features of the Himalayan‐Tibetan system. Radioactive self‐heating …

The Himalayan crystalline core zone exposed along the Sutlej Valley (India) is composed of
two high‐grade metamorphic gneiss sheets that were successively underthrusted and …

Many seismic and magnetotelluric experiments within Tibet provide proxies for lithospheric
temperature and lithology, and hence rheology. Most data have been collected between c …