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How do landscapes record tectonics and climate?
The Earth's surface is shaped by tectonics and climate. This simple statement implies that
we should, in principle, be able to use the landscape as an archive of both tectonic rates and …
we should, in principle, be able to use the landscape as an archive of both tectonic rates and …
Landslide erosion controlled by hillslope material
Steep hillslopes in mountain belts are eroded by landslides, and landsliding is ultimately
driven by the topographic relief produced by fluvial and glacial erosion,,,,. Landslide erosion …
driven by the topographic relief produced by fluvial and glacial erosion,,,,. Landslide erosion …
Driving the upper plate surface deformation by slab rollback and mantle flow
The relative contribution of crustal and mantle processes to surface deformation at
convergent plate margins is still controversial. Conflicting models involving either extrusion …
convergent plate margins is still controversial. Conflicting models involving either extrusion …
The trajectory of geomorphology
Modern geomorphology was founded in the nineteenth century as an exercise of historical
interpretation of landscapes. After the mid-twentieth century it dominantly became a quest to …
interpretation of landscapes. After the mid-twentieth century it dominantly became a quest to …
Morphotectonic and lithostratigraphic analysis of intermontane Karewa basin of Kashmir Himalayas, India
Morpho-tectonic study plays an important role in deciphering the effects of tectonic activity in
the geomorphic evolution of the drainage basins. Romushi watershed forms one of the …
the geomorphic evolution of the drainage basins. Romushi watershed forms one of the …
How rivers react to large earthquakes: Evidence from central Taiwan
Earthquakes and bedrock river incision are fundamental processes in the evolution of
tectonically active landscapes, yet little work has focused on understanding how a bedrock …
tectonically active landscapes, yet little work has focused on understanding how a bedrock …
New constraints on the late Oligocene‐Miocene thermo‐tectonic evolution of the southeastern Tibetan Plateau from low‐temperature thermochronology
Abstract The southeastern (SE) Tibetan Plateau (Yunnan) is characterized by low‐relief
uplands that were deeply incised by large rivers. The thermal history of basement rocks in …
uplands that were deeply incised by large rivers. The thermal history of basement rocks in …
[HTML][HTML] Cenozoic low temperature cooling history of the eastern Lhasa terrane: Implications for high-relief topography of external drainage area in the southern …
Abstract The Tibetan Plateau geographically contains internal and external drainage areas
based on the distributions of river flows and catchments. The internal and external drainage …
based on the distributions of river flows and catchments. The internal and external drainage …
Decoding downstream trends in stratigraphic grain size as a function of tectonic subsidence and sediment supply
Downstream grain-size fining in stratigraphy is driven primarily by selective deposition of
sediment, and the long-term efficiency of this process is determined by:(1) the magnitude …
sediment, and the long-term efficiency of this process is determined by:(1) the magnitude …
Late Mesozoic-Cenozoic multistage exhumation of the central Bangong-Nujiang suture, central Tibet
The Cenozoic rise of the Tibetan Plateau has significantly altered global climate change and
the biological redistribution of Asia. However, there remain great controversies about its …
the biological redistribution of Asia. However, there remain great controversies about its …