Landscape evolution models(LEMs)are essential tools for analyzing tectonic-climate interactions and reproducing landform-shaping processes.In this study we used a LEM to simulate the evolution of the mountains from th...Landscape evolution models(LEMs)are essential tools for analyzing tectonic-climate interactions and reproducing landform-shaping processes.In this study we used a LEM to simulate the evolution of the mountains from the central Hexi Corridor in the northeastern Tibetan Plateau,where the climate is arid and the surface processes are relatively uniform.However,there are pronounced differences in the topography between the mountains around the central Hexi Corridor.The East Jintanan Shan,West Jintanan Shan and Heli Shan are located in the northern part of the corridor;and the Yumu Shan in the southern part.Firstly,several representative areas were selected from these mountains to analyze the topographic characteristics,including the uniform valley spacing,local relief,and the outlet number.Secondly,a LEM for these areas was constructed using the Landlab platform,and the landscape evolution was simulated.With uniform valley spacing and other topographic characteristics as the criteria,we compared the realistic and simulated terrain for different model ages.Finally,based on the similarity of the simulated and realistic terrain,we estimated the timing of the initial uplift and the uplift rate of the four mountain ranges.The results are consistent with previous geological and geomorphological records from these youthful stage mountains that have not yet reached a steady state.Our findings demonstrate that LEMs combined with topographic characteristics are a reliable means of constraining the timing of the initial uplift and the uplift rate of the youthful stage mountain.Our approach can potentially be applied to other youthful stage mountains and it may become a valuable tool in tectonic geomorphology research.展开更多
Active orogenic belts provide natural laboratories for investigating the mechanisms of tectonic deformation and landscape evolution.Along their foreland basins,the relatively continuous sedimentary archives and varied...Active orogenic belts provide natural laboratories for investigating the mechanisms of tectonic deformation and landscape evolution.Along their foreland basins,the relatively continuous sedimentary archives and varied geomorphic units have documented the history of the tectonic uplift of the adjacent orogenic belts.Geological records(e.g.,low-temperature thermochronology and sedimentology)can reveal the history of mountain building on a timescale of tens of millions of years.In contrast,geomorphic evidence generally documents the history of much younger landforms.展开更多
基金the National Natural Science Foundation of China(Grant Nos.41730637&41571003)。
文摘Landscape evolution models(LEMs)are essential tools for analyzing tectonic-climate interactions and reproducing landform-shaping processes.In this study we used a LEM to simulate the evolution of the mountains from the central Hexi Corridor in the northeastern Tibetan Plateau,where the climate is arid and the surface processes are relatively uniform.However,there are pronounced differences in the topography between the mountains around the central Hexi Corridor.The East Jintanan Shan,West Jintanan Shan and Heli Shan are located in the northern part of the corridor;and the Yumu Shan in the southern part.Firstly,several representative areas were selected from these mountains to analyze the topographic characteristics,including the uniform valley spacing,local relief,and the outlet number.Secondly,a LEM for these areas was constructed using the Landlab platform,and the landscape evolution was simulated.With uniform valley spacing and other topographic characteristics as the criteria,we compared the realistic and simulated terrain for different model ages.Finally,based on the similarity of the simulated and realistic terrain,we estimated the timing of the initial uplift and the uplift rate of the four mountain ranges.The results are consistent with previous geological and geomorphological records from these youthful stage mountains that have not yet reached a steady state.Our findings demonstrate that LEMs combined with topographic characteristics are a reliable means of constraining the timing of the initial uplift and the uplift rate of the youthful stage mountain.Our approach can potentially be applied to other youthful stage mountains and it may become a valuable tool in tectonic geomorphology research.
基金supported by the National Natural Science Foundation of China(41730637,41971001,and 42071005)。
文摘Active orogenic belts provide natural laboratories for investigating the mechanisms of tectonic deformation and landscape evolution.Along their foreland basins,the relatively continuous sedimentary archives and varied geomorphic units have documented the history of the tectonic uplift of the adjacent orogenic belts.Geological records(e.g.,low-temperature thermochronology and sedimentology)can reveal the history of mountain building on a timescale of tens of millions of years.In contrast,geomorphic evidence generally documents the history of much younger landforms.
