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Chinese Academy of Sciences Institutional Repositories Grid
Ages and magnitudes of base level fall and valley downcutting in ten tributaries (the Ten Kongduis) of the upper Yellow River, China

文献类型:期刊论文

作者Shi, Changxing
刊名GEOMORPHOLOGY
出版日期2019-01-15
卷号325页码:29-39
关键词Morphometric dating Slope-area power law relation Tectonic uplift Valley downcutting
ISSN号0169-555X
DOI10.1016/j.geomorph.2018.10.005
通讯作者Shi, Changxing(shicx@igsnrr.ac.cn)
英文摘要Using a morphometric dating method and the S-A (channel slope vs. drainage area) power law relation, the history of tectonic uplift and valley downcutting was investigated in the catchments of the Ten Kongduis (ten ephemeral streams) in Inner Mongolia, China, for the past ca. 5 Ma. These streams drain an area of the northern Ordos Plateau and flow northward into the Hetao Basin where they eventually debouch into the Yellow River. To derive reasonable ages of tectonic perturbation in catchments with obviously different widths between their lower and upper sections, an index was constructed for removing the effect of geometric irregularity on the morphometric ages. The morphometric analysis discloses an episode of tectonic uplift in the study area as early as 2.2-5.8 Ma, an episode or episodes of tectonic uplift after 1.15-0.50 Ma, and an episode of base level fall starting from 0.025-0.036 Ma. In the period of 1.15-0.50 Ma, the eastern stream catchments were uplifted from 0.99-1.15 Ma, a middle stream catchment was uplifted after 0.74 Ma, and a western stream catchment was uplifted after 0.50 Ma. The episode of base level fall after 0.025-0.036 Ma was detected only in some western streams, presumably indicating a recent subsidence episode of the western part of the Hetao Basin. After the episode of tectonic uplift dated to 2.2-5.9 Ma, equilibrium longitudinal profiles were formed in the streams and preserved in the sources of some streams. By comparing the elevations of the projected equilibrium profiles based on their S-A power law relations with the current ones, and considering the valley downcutting of the equilibrium profiles in the past 0.5-1.15 Ma, the largest valley downcutting magnitude upstream of the southernmost fault between the Ordos Plateau and the Hetao Basin in two western and three eastern streams was found to be in the ranges of 142-194 m and 52-145 m, respectively, and the base level fall at the northernmost fault between the plateau and the basin was estimated to be 317 m and 138 m on average for the two western and three eastern streams, respectively. (C) 2018 Elsevier B.V. All rights reserved.
WOS关键词TECTONICS ; EVOLUTION ; UPLIFT
资助项目National Natural Science Foundation of China[41671004] ; National Natural Science Foundation of China[41371036]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000451353800003
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/51494]  
专题中国科学院地理科学与资源研究所
通讯作者Shi, Changxing
作者单位Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Shi, Changxing. Ages and magnitudes of base level fall and valley downcutting in ten tributaries (the Ten Kongduis) of the upper Yellow River, China[J]. GEOMORPHOLOGY,2019,325:29-39.
APA Shi, Changxing.(2019).Ages and magnitudes of base level fall and valley downcutting in ten tributaries (the Ten Kongduis) of the upper Yellow River, China.GEOMORPHOLOGY,325,29-39.
MLA Shi, Changxing."Ages and magnitudes of base level fall and valley downcutting in ten tributaries (the Ten Kongduis) of the upper Yellow River, China".GEOMORPHOLOGY 325(2019):29-39.

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来源:地理科学与资源研究所

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