[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 …
Late Cenozoic Cooling History of the Xigaze Fore-Arc Basin along the Yarlung–Zangbo Suture Zone (Southern Tibet): New Insights from Low-Temperature …
Abstract The Tibetan Plateau is currently the widest and highest elevation orogenic plateau
on Earth. It formed as a response to the Cenozoic and is still ongoing collision between the …
on Earth. It formed as a response to the Cenozoic and is still ongoing collision between the …
[HTML][HTML] Late Cenozoic denudation and topographic evolution history of the Lhasa river drainage in southern Tibetan plateau: insights from inverse thermal history …
The interaction of surface erosion (eg, fluvial incision) and tectonic uplift shapes the
landform in the Tibetan Plateau. The Lhasa River flows toward the southwest across the …
landform in the Tibetan Plateau. The Lhasa River flows toward the southwest across the …
A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau
Y Tian, BP Kohn, AJW Gleadow… - Journal of Geophysical …, 2014 - Wiley Online Library
A large part of the southeastern Tibetan Plateau (TP) is characterized by low‐relief surfaces
at high elevations (> 3.5 km). The origin of these landscapes and their geodynamic …
at high elevations (> 3.5 km). The origin of these landscapes and their geodynamic …
Late Mesozoic–Cenozoic cooling history of the northeastern Tibetan Plateau and its foreland derived from low-temperature thermochronology
The growth history and formation mechanisms of the Cenozoic Tibetan Plateau are the
subject of an intense debate with important implications for understanding the kinematics …
subject of an intense debate with important implications for understanding the kinematics …
Late Oligocene-Miocene morpho-tectonic evolution of the central Gangdese batholith constrained by low-temperature thermochronology
The morpho-tectonic evolution of the Tibetan Plateau is controlled by complicated
interactions between tectonic uplift and surface erosion. The Gangdese batholith in the …
interactions between tectonic uplift and surface erosion. The Gangdese batholith in the …
Thermochronology constraints on the Cretaceous-Cenozoic thermo-tectonic evolution in the Gaize region, central-western Tibetan Plateau: Implications for the …
K Tong, Z Li, L Zhu, G Xu, Y Zhang, PJJ Kamp… - Journal of Asian Earth …, 2022 - Elsevier
The temporal and spatial variations of exhumation in the central Tibetan Plateau (TP)
contain information about timing of the initial rise and growth of the TP. Here, we present …
contain information about timing of the initial rise and growth of the TP. Here, we present …
[HTML][HTML] Early Pleistocene drainage pattern changes in Eastern Tibet: Constraints from provenance analysis, thermochronometry, and numerical modeling
The geometry and evolution of fluvial systems are thought to be related to surface uplift. In
eastern Tibet, rivers exhibit peculiar drainage patterns but how these patterns were …
eastern Tibet, rivers exhibit peculiar drainage patterns but how these patterns were …
Cenozoic cooling history and fluvial terrace development of the western domain of the Eastern Kunlun Range, northern Tibet
The growth of the Tibetan Plateau resulted primarily from Cenozoic India-Asia collision and
continued convergence, and thus the deformation timing and geomorphic evolution of …
continued convergence, and thus the deformation timing and geomorphic evolution of …
Cenozoic cooling history of the North Qilian Shan, northern Tibetan Plateau, and the initiation of the Haiyuan fault: Constraints from apatite-and zircon-fission track …
The growth of the Tibetan Plateau resulted primarily from India-Asia convergence since
initial collision at 65–55 Ma. The Cenozoic Qilian Shan thrust belt and the left-slip strike …
initial collision at 65–55 Ma. The Cenozoic Qilian Shan thrust belt and the left-slip strike …
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