Expression of active tectonics in erosional landscapes
Understanding the manner and degree to which topography in active mountain ranges
reflects deformation of the Earth's surface remains a first order goal of tectonic …
reflects deformation of the Earth's surface remains a first order goal of tectonic …
Outward-growth of the Tibetan Plateau during the Cenozoic: A review
The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …
evaluating models of collisional tectonics and holds important implications for processes …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …
geological framework and initial growth were fundamentally the result of multiple, previous …
Crustal deformation in the India‐Eurasia collision zone from 25 years of GPS measurements
Abstract The India‐Eurasia collision zone is the largest deforming region on the planet;
direct measurements of present‐day deformation from Global Positioning System (GPS) …
direct measurements of present‐day deformation from Global Positioning System (GPS) …
Oblique stepwise rise and growth of the Tibet Plateau
P Tapponnier, X Zhiqin, F Roger, B Meyer, N Arnaud… - science, 2001 - science.org
Two end member models of how the high elevations in Tibet formed are (i) continuous
thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) …
thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) …
[图书][B] Active tectonics
Active Tectonics Page 1 Active Tectonics Earthquakes, Uplift and Landscape Second
Edition Edward A. Keller Nicholas Pinter 'ЯШ _ Page 2 Contents 1 Preface xiii Introduction …
Edition Edward A. Keller Nicholas Pinter 'ЯШ _ Page 2 Contents 1 Preface xiii Introduction …
Dynamics of the stream‐power river incision model: Implications for height limits of mountain ranges, landscape response timescales, and research needs
The longitudinal profiles of bedrock channels are a major component of the relief structure of
mountainous drainage basins and therefore limit the elevation of peaks and ridges. Further …
mountainous drainage basins and therefore limit the elevation of peaks and ridges. Further …
Topographic ooze: Building the eastern margin of Tibet by lower crustal flow
Topography extracted from swath profiles along the northern, southern, and eastern margins
of the Tibetan Plateau show two end-member morphologies: steep, abrupt margins and long …
of the Tibetan Plateau show two end-member morphologies: steep, abrupt margins and long …
Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism
Cenozoic magmatism on the Tibetan plateau shows systematic variations in space and time
that must be considered in models concerning Tibetan tectonic evolution. After the India …
that must be considered in models concerning Tibetan tectonic evolution. After the India …