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Modern Yellow River began forming 1.25 million years ago: study

Chinese researchers have found that the modern Yellow River began to form 1.25 million years ago, according to a paper published in the journal Science Bulletin. ....

Wang Xin , Yellow River , China General , Institute Of Geology , Application Center , China University Of Geosciences Wuhan , China Earthquake Administration , Shimane University , Lanzhou University , First Monitoring , China University , Ordos Block ,

Modern Yellow River began forming 1.25 million years ago: study-Xinhua

Modern Yellow River began forming 1.25 million years ago: study- ....

Wang Xin , Yellow River , China General , Institute Of Geology , Application Center , China University Of Geosciences Wuhan , China Earthquake Administration , Shimane University , Lanzhou University , First Monitoring , China University , Ordos Block ,

Modern Yellow River began forming 1.25 million years ago: study

BEIJING, Aug. 21 (Xinhua) Chinese researchers have found that the modern Yellow River began to form 1.25 million years ago, according to a paper published in ....

Wang Xin , Yellow River , China General , Institute Of Geology , Application Center , China University Of Geosciences Wuhan , China Earthquake Administration , Shimane University , Lanzhou University , First Monitoring , China University , Ordos Block , The Modern , The Formation , She Yellow ,

Frontiers | Early Quaternary Tectonic Transformation of the Helan Shan: Constraints Due To Quantitative Geomorphology

The Helan Shan is located on the front edge of the expanding Tibetan Plateau. However, how the topography here responds to this propagation and its precise time constraints remains unknown. Based on the response process of fluvial landforms and tectonic evolution, we conducted a quantitative landform analysis of the Helan Shan region. Here, the spatial distribution features of various geomorphic indices were coupled, demonstrating that the mountain is tilting toward the west and north. The steeper downstream and gentle upper reaches indicate that the fluvial landforms have experienced an accelerated incision event, which can be attributed to the tectonic activity along the East Helan Shan Fault. Furthermore, the response time of the tectonic knickpoints ranges from 0.1¬–1.4 Ma based on the paleochannel reconstruction method. Combined with previous studies on low temperature thermochronology and active tectonics, we propose a tectonic transformation model where the Helan Shan shi ....

Inyo Mountains , United States , China General , Inner Mongolia , Nei Mongol , South China Sea , Brunei General , Republic Of China , Taiwan General , Roan Plateau , Yellow River , Tibetan Plateau , Ma Liu , Gediz Ala , Cihat Al , Helan Shan Liu , Helan Shan , Helan Shan Yang , Baiyin Obao , Niushou Shan , Yumu Shan , National Science Foundation Of China , China University Of Geosciences , Shuttle Radar Topography Mission , National Key Research , Development Program Of China ,

Frontiers | Strain Transformation Adjacent to the West Qinling Orogen: Implications for the Growth of the Northeastern Tibetan Plateau

Frontiers | Strain Transformation Adjacent to the West Qinling Orogen: Implications for the Growth of the Northeastern Tibetan Plateau
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United States , Sierra Nevada , United Kingdom , China General , Qilian Shan , Yu Chen , Guo Chen , Long Valley Caldera , Hwang Shen , Chen Lin , Nei Mongol , Tibetan Plateau , Harkins Kirby , Molnar Tapponnier , Qinling Orogen , Davidk Wright , Kirby Harkins , Qinling Dabie Orogen , Duvall Clark , Loveless Meade , National Natural Science Foundation Of China , Massachusetts Institute Of Technology , Development Program Of China , Cenozoic Tectonic Development Of Northern Tibet , Research On Recent , Analysis Program ,