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| 1 | Discovery of Quaternary glacial evidence of Snow Mountain in Taiwan, China显示文摘There are glacial remains of three different periods on the main peak of Snow Mountain in Taiwan province, including cirque lake, crosswall, polished surface, striation, moraine ete. These three different periods were called, respectively, Shanzhuang ((44.25 ± 3.72) kaBP), Shuiyuan ((18.26 ± 1.52) kaBP), and Xueshan glacial stages (the late period of last glaciation). it is characterized by the earlier glacier broad in scale. | CUI Zhijiu YANG Jianfu LIU Gengnian WANG Xin SONG Guocheng | 2000 | Chinese Science Bulletin2000，45，6： | 20 |
| 2 | Late Pleistocene glaciation of the Changbai Mountains in northeastern China显示文摘The Changbai Mountains (2749 m a.s.l.) in northeastern China are one of the typical mountain regions with glaciation since late Pleistocene as evidenced by well-preserved erosive and accumulative landforms at elevations above 2000 m a.s.l. formed by glaciers around the crater lake, Tianchi Lake. Cirque glaciers developed on both the inner and outer sides of the volcanic cone. Well-preserved cirques, glacial trough valleys, glacial threholds, polished surfaces of the glacial erratics and the moraine ridges indicate that several glaciation processes took place during the last glacial period in this region. Results of optically stimulated luminescence (OSL) dating on the moraine sediments, and the K/Ar, ther- mal ionization mass spectrometry (TIMS), electronic spinning resonance (ESR) dating on the volcanic rocks suggest two periods of glacier advances. One is named the Black Wind Mouth glacier advance taking place on the west and north slopes of the volcanic cone at an elevation of 2000―2100 m a.s.l., which is dated to about 20 ka, being the result of the Last Glacial Maximum (LGM). The other is named the Meteorological Station glacier advance at the elevation of 2400―2600 m a.s.l., dated to 11 ka during the late glacial period, and is tentatively correlated to the Younger Dryas stage. The scope of the former glacier advance is larger than that of the latter. Regional comparisons showed that the glacial sequences in the Changbai Mountains are similar to other glaciated areas in eastern Asia during the later part of the last glacial cycle. | ZHANG Wei NIU YunBo YAN Ling CUI ZhiJiu LI ChuanChuan MU KeHua | 2008 | Chinese Science Bulletin2008，53，17： | 18 |
| 3 | Discovery and character of the Kunlun-Yellow River Movement显示文摘Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recognized in 1 10-0 60 Ma B.P. This tectonic movement, which leads to uplift of the Qinghai_Xizang (Tibet) Plateau from 1 500 to 3 000-3 500 m, is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping. | CUI Zhijiu 1, WU Yongqiu 2,3 and LIU Gengnian 1 1. Department of Geography, Peking University, Beijing 100871, China 2. Open Research Laboratory of Environmental Changes and Natural Disaster of State Education Commission, Beijing 100875, China | 1998 | Chinese Science Bulletin1998，43，10： | 16 |
| 4 | AMS dating on glacial tills at the source area of the Urumqi River in the Tianshan Mountains and its implications显示文摘Using accelerating mass spectrometry (AMS) dating method, a dating has been made on the primary calcium carbonate in tills and secondary calcium carbonate coating on till gravel and the roche moutonnee formed since the Last Glaciation at the source area of the Urumqi River valley in the Tianshan Mountains, northwestern China. The results reveal that the carbonate content in the tills in this noncarbonate area is high enough to date by AMS, that the carbon in the coatings on the newly exposed roche moutons and in the modern till is modern carbon and so the 14 C dating results in the ancient till can represent the actual ages of the till formation, and that the warm period during the Holocene began as early as 6 500 a B.P. and lasted to 1 800 a B.P. | Chaolu Yi Kexing Liu Zhijiu Cui | 1998 | Chinese Science Bulletin1998，43，20： | 15 |
| 5 | Quaternary glacier development and the relationship between the climate change and tectonic uplift in the Helan Mountain显示文摘孤立拉长 Helan 山脉山岳的 NE-SW,分开从 Tenggeli 沙漠的 Ordos 高原的适度的草地,是在西方中国学习冰河发展的一个关键位置以及气候的联合条件随着变化构造高举。冰川的地形和存款包括冰斗,山峰,刀口山脉,侧面的冰碛,和终端冰碛在 Helan 山的中间的部分在 2800 m a.s.l 上面散布。这分布显示这曾经是 glaciated 在期间晚第四级。形态学特征证明形成事件的风景的一个清楚的序列发生在整个 Helan 山。实验室光学地刺激了光(OSL ) 和标明日期的加速器团 spectrometry 放射性碳(AMS 14C ) 结果显示冰川的进展的迟了的历史。在 Helan 山的中间的部分的迟了的更新世冰河进展了接近他们的位置至少四次,并且冰川的序列能作为最后一个冰川的周期的中间的阶段被分配(MIS3b, 43.2 ????????? ′ ? 錸? 錸?@ | ZHANG Wei HE MingYue LI YongHua CUI ZhiJiu WANG ZhiLin YU Yang | 2012 | Chinese Science Bulletin2012，57，34： | 14 |
| 6 | Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province显示文摘Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountainsconstitute one ofthe typicalplacesonce glaciated.Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about100 ka BP and two TL absolute ages(101,100 ±7780 a BP;104,000±8300 a BP)indicate thisadvance happened during the Penultimale Glaciation.The early stage glacialadvance (YJT-II advance) during the last glaciation occurred about 40,920±3400 a BP. The last glacial maximum advance (YJT-IIIadvance)about18-25 ka BP,which sustained by two TL ages(18,230 ± 1420 a BP;25,420 ±2110 a BP).The Penultimale and the early stage glaciationswere more extensive and the lastglacialmaximum (LGM )and the late-glacialperiod (YJT-IV advance,10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains justlike the advances in the western partsuch as Diancang mountains,Yulong mountains ofYunnan Province and the glacierseries are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representativeofclimatechangesduring thelastglacialcyclein Yunnan Province. | ZHANG Wei CUI Zhijiu FENG Jinliag YI Chaolu YA NG Jianqiang | 2005 | Journal of Geographical Sciences2005，15，4： | 13 |
| 7 | Late Cenozoic high-resolution magnetostratigraphy in the Kunlun Pass Basin and its implications for the uplift of the northern Tibetan Plateau显示文摘The Kunlun Pass Basin, located in the middle of the eastern Kunlun Mountains, received relatively continuous late Cenozoic sediments from the surrounding mountains, archiving great information to understand the deformation and uplift histories of the northern Tibetan Plateau. The Kunlun-Yellow River Movement, identified from the tectonomorphologic and sedimentary evolution of the Kunlun Pass Basin by Cui Zhijiu et al. (1997, 1998), is roughly coincident with many important global and Plateau climatic and environmental events, becoming a crucial time interval to understand tectonic-climatic interactions. However, the ages used to constrict the events remain great uncertainty. Here, we present the results of detailed magnetostratigraphy of the late Cenozoic sediments in the Kunlun Pass Basin, which show the basin sediments were formed between about 3.6 Ma and 0.5 Ma and the Kunlun-Yellow River Movement occurred at 1.2 to ~0.78 Ma. The lithology, sedimentary facies and lithofacies associations divide the basin into five stages of tectonosedimentary evolution, indicating the northern Tibetan Plateau having experienced five episodes of tectonic uplifts at ~3.6, 2.69-2.58, 1.77, 1.2, 0.87 and ~0.78 Ma since the Pliocene. | SONG Chunhui GAO Dongling FANG Xiaomin CUI Zhijiu LI Jijun YANG Shengi JIN Hongbo Douglas Burbank Joseph L. Kirschvink | 2005 | Chinese Science Bulletin2005，50，17： | 10 |
| 8 | Granite landform characteristics,distribution and evolution patterns in Huangshan Mt.显示文摘The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern. The remaining parts of the planation surface are in the center; domical peaks, castle peaks, pointed peaks, and ridges are arranged from the center to the periphery accordingly. This reveals that knick points are still near the center and the center area is the common divide of the radial water system. It is inferred that the granite bodies in the Huangshan Mt. were exposed to erosion in Miocene and Pliocene, and the planation surface was also formed then. After the slight uplift in late Pliocene, a light-incised surface was formed. Then, in early Quaternary, there were intense uplifts and incisions so that deep incised surface was formed. The above process is still in progress, and results in high peaks and deep gorges outside of the center area. However, due to the limited catchment area in the center, headward erosion is mild, and the current landforms in the Huangshan Mt. can be maintained for a long time. | CUI ZhiJiu CHEN YiXin YANG XiaoYan | 2009 | Chinese Science Bulletin2009，54，23： | 7 |
| 9 | Much late onset of Quaternary glaciations on the Tibetan Plateau:determining the age of the Shishapangma Glaciation using cosmogenic 26Al and 10Be dating显示文摘The onset of Quaternary glaciations is a critical event in the climate and tectonic history of the Tibetan Plateau.The Shishapangma Glaciation,defined based on the till deposit from the northern slopes of Mt.Shishapangma,has been identified as the oldest glaciation on the Tibetan Plateau.However,the timing of this glaciation has not been constrained.We measured^(10)Be and^(26)Al concentrations of a set of boulders on top of this till and simulated their complex exposure-burial histories.The simulated results indicate that the formation age of this till is likely around 835.2±241.0 ka,representing the minimum timing of glacial onset on the Tibetan Plateau.The Shishapangma Glaciation is apparently much younger than the glacial onset in many other areas of the world,such as Europe and North America,and was likely driven by the coupled effect between tectonic uplift and climate cooling during the early–middle Pleistocene transition. | Yixin Chen Yingkui Li Mei Zhang Zhijiu Cui Gengnian Liu | 2018 | Science Bulletin2018，63，5： | 7 |
| 10 | The discovery and environmental significance of Chifeng wind route and huge pots of Inner Mongolia and Hebei Province显示文摘The pots discovered in Inner Mongolia and Hebei Province are huge with a maximum diameter of 9 m and a depth of 3.5 m, singular in shape,caused by weathering and wind erosion and have certain direction. They are a kind of typical climatic geomorphology. This | Zhijiu Cui Hongjiang Li Ling Nan Dewen Li | 1999 | Chinese Science Bulletin1999，44，16： | 5 |
| 11 | Comments on the planation surface once more显示文摘The authors reviewed the research of planation surface in recent years and commented on the development of method and theory about the planation surface. Some aspects of research, such as the restrictive planation surface, the karst planation surface, the fossil planation surface, the dating of weathering crust, the research of weathering crust and environmental evolution, extremely enriched the method and theory of the planation surface. Besides, the authors pointed out that we must take further steps to study the following issues: the deformation of planation surface, the original height of planation surface, the recognition and contrast of the planation surface. The weathering crust and planation surface should be regarded as a whole, and it will still be a principal aspect in the future. | CUI Zhijiu LI Dewen FENG Jinliang LIU Gengnian | 2002 | Chinese Science Bulletin2002，47，10： | 4 |
| 12 | Global warming accelerates the upfreezing of permafrost in arid middle Tianshan Mountains显示文摘Upfreezing is an important geomorphic process in the periglacial environment.It is a product of cold climate and thus an important part of the cryospheric processes.Based on the long-term positioning observations in the source area of the Urumqi River,this article represents an in-depth discussion of the characteristics of sorted circles and upfreezing mechanisms in the Tianshan Mountains.In the source area of the Urumqi River,the intensity of upfreezing is the highest within the top 25 cm near the surface,while targets with a diameter of 3 cm are least affected by upfreezing.There is no distinct difference between the centre with fine grains and the margin with coarse debris within the same sorted circle in terms of the intensity of upfreezing.The correlation analysis demonstrates that temperature plays an important role in upfreezing and the development of sorted circles.A long-time positioning observation of sorted circles reveals that periglacial landforms are sensitive to regional climate change and respond quickly to the temperature increase of the recent two decades.Enhanced upfreezing was found to be due to increased soil moisture content. | LI ChuanChuan CHEN YiXin NIE ZhenYu CUI ZhiJiu LIU GengNian | 2013 | Chinese Science Bulletin2013，58，31： | 2 |
| 13 | Processes and environmental significance of the subglacial chemical deposits in Tianshan Mountains显示文摘On the bedrock surface of Glacier No.1 in the headwater of Urumqi River, Tianshan Mts., well layered and crystallized subglacial calcite precipitations were discovered. Based on observations and analysis of the surface form, sedimentary texture and structure, and chemical composition of the deposits, clues about the subglacial processes and environment are deduced. The radial-growth crustation texture of the deposits, which builds up in the saturated CaCO3 so- lution, proves the existence of pressure melting water and water films under Glacier No.1; and their rhythmic beddings, dissolved planes and unconformable contacts show that the water films responsible for the formation of these structures were in a wide range of spatial as well as tem- poral variations. Though formed under continental glacier in non-limestone area, the deposits are quite similar to those formed under temperate glaciers in limestone areas, a fact that shows a similar process of chemical precipitation between the two. Hence the enrichment of calcium in the subglacial melting water and the process of precipitation have actually little to do with the bedrock lithology and the glacier types. The cemented detritus in the deposits are rich in Fe and Al while depleted in K, Na and Si; also the included clay mineral consists mainly of illite, which reveals some weak chemical weathering under the continental glacier. The subglacial CaCO3 precipitates when plenty of Ca++ melt into the subglacial melting water on a comparatively en- closed ice-bedrock interface under a high CO2 partial pressure, the forming of subglacial chemical deposits therefore offers unequivocal evidence for the ongoing of subglacial chemical reactions. | LIU Gengnian LUO Risheng CAO Jun CUI Zhijiu | 2005 | Science China Earth Sciences2005，48，9： | 2 |
| 14 | The cover karst,weathering crust and karas (donble-level) planation surface显示文摘 | Cui Zhijiu Li Dewen Feng Jinliang | 2002 | Science in China (Series D)2002，45，4： | 1 |
| 15 | The cover karst, weathering crust and karas (double-level) planation surface显示文摘 | Cui Zhijiu Li Dewen Feng Jinliang | 2002 | Science in China (SeriesD)2002，45，4： | 1 |
| 16 | Glacial valley cross-profile morphology, Tian Shan Mountains, China显示文摘 | Yingkui Li Gengnian Liu Zhijiu Cui | 2001 | Geomorphology2001，，1： | 1 |
| 17 | Late Pleistocene glaciation of the Dianeang and Gongwang Mountains, southeast margin of the Tibetan Plateau显示文摘 | Jianqiang Yang Wei Zhang Zhijiu Cui | | Quaternary International0，5262，： | 1 |
| 18 | About KunlunHuanghe Movement显示文摘 | Cui Zhijiu Wu Yongqiu Liu Gengnian | 1998 | Science in China (Series D-Earth Science)1998，28，1： | 1 |
| 19 | A review of glacial sequences of the Kunlun Pass, northern Tibetan Plateau显示文摘 | Gengnian Liu Xiaoyong Zhang Zhijiu Cui Yongqiu Wu Yuanjiang Ju | 2006 | Quaternary International2006，，： | 1 |
| 20 | Review of the timing and extent of glaciers during the last glacial cycle in the bordering mountains of Tibet and in East Asia显示文摘 | Zhang Wei Cui Zhijiu Li Yonghua | 2006 | Quaternary International2006，，： | 1 |
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