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Guangrong Dong

Researcher at Chinese Academy of Sciences

Publications -  26
Citations -  944

Guangrong Dong is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Plateau & Glacial period. The author has an hindex of 13, co-authored 26 publications receiving 872 citations.

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Pliocene uplift of the northern Tibetan Plateau

TL;DR: In this paper, a 45 km section near Yecheng in the western Kunlun Mountains of the northern Tibetan Plateau was investigated and the change from deposition on distal alluvial plains to proximal fans occurred during the Gilbert reversed chron (45-35 Ma) followed by an increase in sedimentation rate.
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Influence of desertification on vegetation pattern variations in the cold semi-arid grasslands of Qinghai-Tibet Plateau, North-west China

TL;DR: In this paper, a field study was conducted in the Guinan desertified grassland of the Qinghai-Tibet plateau, North-west China, to test the hypotheses on a regional scale.
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Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing

TL;DR: In this paper, a newly-constructed record of magnetic susceptibility (SUS) and the depositional rate change of eolian loess-red clay sequences in the last 7.2 and 3.4 Ma BP from the Qinghai-Xizang Plateau, together with a cornperison of a record of °18O values from the equatorial East Pacific Ocean and Eolian Quartz flux variations fmm the North Pacific Ocean, the evolutiomuy process of the Late Cenozoic Great Glaciation in the Northern Hemisphere can be divided
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Estimates of soil movement in a study area in Gonghe Basin, north-east of Qinghai-Tibet Plateau

TL;DR: In this paper, a study was conducted to estimate soil erosion rates and assess patterns of soil movement by wind erosion in a 600 ha area during a 37-year period using the 137 Cs tracer technique.
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Morphodynamic study of reticulate dunes at southeastern fringe of the Tengger Desert

TL;DR: In this paper, the authors studied the morphodynamics and formation mechanism for reticulate dunes in the southeastern Tengger Desert and found that the primary ridges were formed by dominant northwest wind and the secondary ridges developed and maintained by alternating dominant wind and subdominant northeast wind on the basis of the primary ridge.