Abandonment of ancient cities near the Salawusu River valley, China, triggered by stream capture
暂无分享,去创建一个
Liubing Xu | Jing Feng | Bao-sheng Li | Xiaohao Wen | Rihui Huang | Wei Wang | Mingkun Qiu
[1] M. Caffee,et al. Late Cenozoic climate change paces landscape adjustments to Yukon River capture , 2020, Nature Geoscience.
[2] Nai’ang Wang,et al. Fluvial incision caused irreversible environmental degradation of an ancient city in the Mu Us Desert, China , 2020, Quaternary Research.
[3] Huiping Zhang,et al. Climate-driven formation of fluvial terraces across the Tibetan Plateau since 200 ka: A review , 2020, Quaternary Science Reviews.
[4] P. Reimer. Composition and consequences of the IntCal20 radiocarbon calibration curve , 2020, Quaternary Research.
[5] M. Karamouz,et al. Groundwater Hydrology , 2020, Groundwater Hydrology.
[6] D. Jiang,et al. A multi-model analysis of ‘Little Ice Age’ climate over China , 2019, The Holocene.
[7] Xing-nian Liu,et al. Abrupt drainage basin reorganization following a Pleistocene river capture , 2018, Nature Communications.
[8] Yongqiu Wu,et al. Evolution of Peatlands in the Mu Us Desert, Northern China, Since the Last Deglaciation , 2018 .
[9] Yongqiu Wu,et al. Holocene water-level changes inferred from a section of fluvio-lacustrine sediments in the southeastern Mu Us Desert, China , 2017 .
[10] Morteza Fattahi,et al. Employing Minimum age model (MAM) and Finite mixture modeling (FMM) for OSL age determination of two important samples from Ira Trench of North Tehran Fault , 2016 .
[11] Y. Sheng,et al. Holocene environment changes around the Sara Us River, northern China, revealed by optical dating of lacustrine–aeolian sediments , 2016 .
[12] R. Unkefer. Charcoal , 2015, Reactions Weekly.
[13] L. Scuderi,et al. Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner Mongolia, northern China , 2015, Proceedings of the National Academy of Sciences.
[14] J. Pitlick,et al. Sediment supply and channel morphology in mountain river systems: 1. Relative importance of lithology, topography, and climate , 2013 .
[15] G. Burr,et al. Radiocarbon dating, reservoir effects, and calibration , 2013 .
[16] J. Cui,et al. The possible climate impact on the collapse of an ancient urban city in Mu Us Desert, China , 2013, Regional Environmental Change.
[17] M. Macklin,et al. U-Pb zircon dating evidence for a Pleistocene Sarasvati River and capture of the Yamuna River , 2012 .
[18] Gregory S. Springer,et al. CLIMATE DRIVEN CHANGES IN RIVER CHANNEL MORPHOLOGY AND BASE LEVEL DURING THE HOLOCENE AND LATE PLEISTOCENE OF SOUTHEASTERN WEST VIRGINIA , 2009 .
[19] David Dian Zhang,et al. Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3 , 2009 .
[20] D. Zhang,et al. Phases of Environmental Evolution Indicated by Primary Chemical Elements and Paleontological Records in the Upper Pleistocene‐Holocene Series for the Salawusu River Valley, China , 2007 .
[21] Lian Baosheng,et al. A Multi‐cycle Climatic Fluctuation Record of the Last Interglacial Period: Typical Stratigraphic Section in the Salawusu River Valley on the Ordos Plateau, China , 2005 .
[22] T. Pietsch,et al. Optical dating of Holocene sediments from a variety of geomorphic settings using single grains of quartz , 2004 .
[23] K. Schilling,et al. Water table fluctuations near an incised stream, Walnut Creek, Iowa , 2004 .
[24] L. Starkel. Climatically controlled terraces in uplifting mountain areas , 2003 .
[25] Lawrence E. Band,et al. Down by the riverside: urban riparian ecology , 2003 .
[26] J. Wallinga. Optically stimulated luminescence dating of fluvial deposits: a review , 2002 .
[27] R. Westaway,et al. Uplift-driven valley incision and climate-controlled river terrace development in the Thames Valley, UK , 2001 .
[28] D. Zhang,et al. Paleo-monsoon activities of Mu Us Desert, China since 150 ka B.P. — a study of the stratigraphic sequences of the Milanggouwan Section, Salawusu River area , 2000 .
[29] Nicholas Brozovic,et al. Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas , 1996, Nature.
[30] P. Bishop. Drainage rearrangement by river capture, beheading and diversion , 1995 .
[31] D. Merritts,et al. Long river profiles, tectonism, and eustasy: A guide to interpreting fluvial terraces , 1994 .
[32] Hou Ren-zhi. Ancient City Ruins in the Deserts of the Inner Mongolia Autonomous Region of China , 1985 .
[33] R. C. Selley. Depositional Sedimentary Environments: with Reference to Terrigenous Clastics , 1982 .
[34] K. G. Johnson. Depositional Sedimentary environments, with reference to terrigenous clastics: H.-E. Rineck and I.B. Singh, Springer Verlag, Berlin, 1973, 439 pp., DM. 108.00 , 1975 .
[35] R. Folk,et al. Brazos River bar [Texas]; a study in the significance of grain size parameters , 1957 .
[36] A. Shakoor,et al. Relationships Between Grain Size Distribution Indexes and Permeability of Sands , 2015 .
[37] S. Tooth,et al. Geological controls on alluvial river behaviour: a comparative study of three rivers on the South African Highveld , 2004 .
[38] K. R. Rushton,et al. Groundwater Hydrology: Conceptual and Computational Models , 2003 .
[39] Deng Qi. DISCUSSION ON CENOZOIC TECTONICS AND DYNAMICS OF ORDOS BLOCK , 1999 .
[40] Robert C. Wolpert,et al. A Review of the , 1985 .
[41] J. Brice,et al. Channel patterns and terraces of the Loup Rivers in Nebraska , 1964 .