黄河上游德恒隆-锁子滑坡堵塞黄河事件

黄河上游龙羊峡刘家峡河段两岸岸坡形成了众多残留体积超过10⁸ m³的古巨型滑坡,最大体积近30×10⁸ m³,且大部分堵塞过黄河。但部分巨型滑坡至今未有学者进行科学研究,其中包括德恒隆滑坡和锁子滑坡。结合区域地质环境条件,通过对德恒隆-锁子两个巨型滑坡基本特征和滑坡堵塞黄河的野外7个地质现象进行分析,并对德恒隆-锁子滑坡形成机制进行初步探讨,认为德恒隆-锁子滑坡为地震型滑坡,且形成原因与青藏高原8万 a的构造期有密切关系。通过分析黄河沿岸堰塞湖湖相沉积,认为堰塞湖形成时间为8万 a左右,这与德恒隆-锁子滑坡的形成年代一致。因此德恒隆-锁子滑坡在地震作用下触发并堵塞黄河。     

黄河龙羊峡-刘家峡河段特大型滑坡成因分析

文章在阐述黄河上游龙羊峡-刘家峡河段内滑坡类型及分布的基础上,分析了滑坡发育与黄河形成演化历史的关联性。认为距今12.5万a前后的共和运动使得黄河溯源侵蚀加剧,水资源的重新分配,导致黄河切蚀能力加强,并于距今1.8-2.9万a达到高潮。因此,构造抬升致使黄河水流快速下切,是造就区内特大滑坡发生的根本原因。     

黄河上游拉干峡—寺沟峡段特大型滑坡 及其成因研究

黄河上游拉干峡—寺沟峡段共发育特大型滑坡116处,群尖盆地无论是数量还是强度上都占到了绝对优势,这与其所处的特殊构造部位和昆黄运动时期各大断裂带运动性质的转变直接相关;高原掀斜式隆升过程导致各大支流水系特大型滑坡西岸多发于东岸。研究区特大型滑坡有明显的4个群发期,各期都有其不同的触发因素,50 ka和30 ka属构造和气候的耦合成因,10 ka为构造触发, 5 ka 为降雨所致。     

Landslide Developmental Characteristics and Response to Climate Change since the Last Glacial in the Upper Reaches of the Yellow River,NE Tibetan Plateau

The upper reaches of the Yellow River in northeastern Tibetan Plateau are geohazards areas. The evolution of the Yellow River, chronology of some landslides, and spatiotemporal distribution characteristics of super large scale and giant landslides within the region are summarized using paleoclimate evidence, and the relationship between the intensive landslide period and climatic changes since the Last Glacial period is analyzed. It is concluded that(1) Super large scale and giant landslides are distributed widely within the region, particularly in the Qunke-Jianzha basin.(2) The chronological sequence of landslides is established by dating the slip zones of landslides and analyzing the relations between landslides and their overlying or underlying loess formations. Five landslide development periods are determined: 53–49 ka BP, 33–24 ka BP, 10–8 ka BP, 5–3.5 ka BP, and the present.(3) These correspond closely to warm and wet periods during the last 100,000 years, i.e., two weak paleosol development stages of Malan loess deposited during the last Glacial period in the Chinese loess Plateau, L1-4 and L1-2 that belong to the marine oxygen isotope stage 3, the last deglacial period, the Holocene Optimum, and the modern global warming period.(4) Landslide triggers may be closely linked to warm and wet periods related to rapid climatic transitions.     

黄河上游物质在新近纪未流入晋陕峡谷*

河流的出现是其流域内构造活动和气候变化综合作用的结果。晋陕峡谷位于黄河上游和中游的衔接部位,对于研究上游黄河何时进入晋陕峡谷具有无可替代的地理位置优势。目前对于黄河何时进入晋陕峡谷一直存有较大争议,存在中新世、上新世和更新世几种主要观点。基于此,作者对晋陕峡谷北段新近纪地层开展碎屑锆石U-Pb年龄分析和沉积相观察。首次报道了磨扇沟、大烟墩、高家窨子3个剖面270颗碎屑锆石 U-Pb 年龄结果。通过和区域内潜在源区进行对比,以及古流向都是自东向西的现象,判定磨扇沟和大烟墩2个剖面的物质来自近源的吕梁山北段; 高家窨子剖面底部的砂岩流向为自南向北,其物源区来自鄂尔多斯地块北部中生代地层。结合这些地层已经报道的古地磁年龄,认为晋陕峡谷北段在6.2~3.7 Ma期间以近源堆积为主,是对青藏高原隆升远程效应和东亚夏季风增强的沉积响应,而和黄河上游物质不存在物源联系。     

黄河上游物质在新近纪未流入晋陕峡谷*

河流的出现是其流域内构造活动和气候变化综合作用的结果。晋陕峡谷位于黄河上游和中游的衔接部位,对于研究上游黄河何时进入晋陕峡谷具有无可替代的地理位置优势。目前对于黄河何时进入晋陕峡谷一直存有较大争议,存在中新世、上新世和更新世几种主要观点。基于此,作者对晋陕峡谷北段新近纪地层开展碎屑锆石U-Pb年龄分析和沉积相观察。首次报道了磨扇沟、大烟墩、高家窨子3个剖面270颗碎屑锆石 U-Pb 年龄结果。通过和区域内潜在源区进行对比,以及古流向都是自东向西的现象,判定磨扇沟和大烟墩2个剖面的物质来自近源的吕梁山北段; 高家窨子剖面底部的砂岩流向为自南向北,其物源区来自鄂尔多斯地块北部中生代地层。结合这些地层已经报道的古地磁年龄,认为晋陕峡谷北段在6.2~3.7 Ma期间以近源堆积为主,是对青藏高原隆升远程效应和东亚夏季风增强的沉积响应,而和黄河上游物质不存在物源联系。     

Landslide-dam paleolakes in the Central Pyrenees,Upper Gállego River Valley,NE Spain: timing and relationship with deglaciation

The production of a cartographic landslide inventory in the glaciated headwaters of the upper Gállego River, Axial Zone of the Spanish Pyrenees, revealed several paleolakes. These relict lake basins are related to the blockage of drainages by postglacial earthflows and slides, mainly developed on Paleozoic slates. The paleolakes are recorded either by non-dissected infilled basins or by hanging and incised lacustrine terraces that persisted for thousands of years. The development of lakes upstream of landslides, was favored, despite their erodibility, by high-displacement rates and the occurrence of paired landslides on both sides of the valley. Radiocarbon and single-grain optically stimulated luminescence (OSL) ages obtained on the lake sediments range between 41.5?±?3.9 ka and 15.1?±?0.3 ka. These chronologies indicate prolonged landslide activity long after the early deglaciation in the upper Gállego River Valley. The landslide-lake dating results support the interpretation that the regional maximum ice extent (MIE) in the Pyrenees occurred during the marine isotope stage 4 (MIS 4), long before the global Last Glacial Maximum (LGM).     

关于黄河形成时代的一些认识

以黄河中游河套盆地-晋陕峡谷-三门峡盆地-三门峡峡谷-郑州邙山段黄河形成时代为主要研究内容,辅以黄河上游兴海盆地-共和盆地段黄河出现的时代来探讨统一黄河形成的时代。黄河上游兴海盆地共发育9级黄河阶地,ESR和OSL年代结果表明,最高三级阶地分别形成于200ka,100ka和80ka; 中游河套盆地普遍发育一套湖相沉积,其中盆地东南端托克托台地郝家窑剖面湖相沉积的亮度和烧失量数据呈现一致的由下向上波动上升变化趋势,反映沉积物碳酸盐含量在不断增高,湖水盐度在增大,可能指示了湖泊处于封闭的环境,OSL结果显示湖相沉积结束的年代在100ka前后; 三门峡盆地东端发育的最高黄河阶地年代为150ka,而指示古三门湖湖水外泄的河湖相白砂层结束时间是200ka。文章总结对比前人的研究成果,认为共和运动才是形成统一黄河的主因,尽管如此,上游兴海-共和河段及中游三门峡河段黄河(分别形成于200ka和200~150ka)出现要早于河套地区(100ka),而晋陕峡谷最晚贯通。也就是说,现今统一的黄河形成于100ka前后。     

黄河上游寺沟峡拉干峡段滑坡时空特征及对气候变化的响应研究

滑坡发育动力机制对全球气候变化的响应过程逐渐成为地质灾害研究领域的热点和焦点问题。文章以我国地质灾害高易发区的黄河上游寺沟峡拉干峡段大型、特大型、巨型滑坡为研究对象,在广泛收集区域古气候演化资料和滑坡年代测定的基础上,开展了末次冰期以来特大型、巨型滑坡发育的时空分布规律研究,分析了滑坡的主要发育期与全球气候变化的响应关系,在此基础上探讨了研究区滑坡发育的动力机制对气候变化的响应过程。主要取得了以下认识:(1)研究区滑坡异常发育,分布广泛、成灾规模大、动力机制复杂、危害严重,在空间上以群科尖扎盆地最为发育; (2)利用滑坡钻孔滑带土和滑坡体与上下覆黄土的叠置关系开展了滑坡体的年代学测定工作,并从时间尺度上划分了滑坡的5个主要发育期,其分别为53～49ka B.P.、33～24ka B.P.、10～8ka B.P.、5～3.5ka B.P.和现代; (3)研究区滑坡的主要发育期分别对应于中国黄土高原马兰黄土中的2层弱发育古土壤层L1-4 和L1-2、末次冰期晚期/全新世过渡期、全新世适宜期和现代全球升温期; (4)全球不同地区滑坡的发育期与气候变化有密切联系,其主要发育于古气候的温暖湿润期和气候变化的快速转型期。     

Ancient landslide-dam events in the Jishi Gorge,upper Yellow River valley,China

Some scholars have argued that the formation and outburst of an ancient dammed lake in the Jishi Gorge at ca. 3700 cal yr BP resulted in the destruction of Lajia, the site of a famous prehistoric disaster in the Guanting Basin, upper Yellow River valley, China. However, the cause of the dammed lake and the exact age of the dam breaching are still debated. We investigated ancient landslides and evidence for the dammed lake in the Jishi Gorge, including dating of soil from the shear zone of an ancient landslide, sediments of the ancient dammed lake, and loess above lacustrine sediments using radiocarbon and optically stimulated luminescence (OSL) dating methods. Six radiocarbon dates and two OSL dates suggested that the ancient landslides and dammed lake events in the Jishi Gorge probably occurred around 8100 cal yr BP, and the ancient dammed lake was breached between 6780 cal yr BP and 5750 cal yr BP. Hence, the outburst of the ancient dammed lake in the Jishi Gorge was unrelated to the ruin of the Lajia site, but likely resulted in flood disasters in the Guanting Basin around 6500 cal yr BP.     

黄河上游曲哇加萨滑坡“9?20”动力学过程模拟与分析

位于黄河上游的曲哇加萨巨型滑坡1985—2020年间发生多起不同程度的局部滑动,严重威胁国道G227 及下方村民生命和财产安全。以2019年9月20日发生于曲哇加萨老滑坡东北段中前缘的H1滑坡为例,在野外调查、形变数据以及稳定性分析的基础上,研究了该滑坡的变形破坏特征,并通过动力学模拟进一步分析了滑坡的成灾范围,反演分析验证了1号滑面浅层滑坡按照摩擦流变模型运动后,将运动堆积到挡墙至军功路段国道G227和居民区,而预测分析发现欠稳定状态的2号滑面浅层滑坡运动后,将运动堆积到军功路至黄河段居民区,但不至于引起堵塞黄河灾害发生。研究结果可为黄河上游巨型滑坡的运动预测评价方法提供一定参考。     

中更新世早中期以来黄河上游与三峡库区滑坡形成机理与气候变化关系研究

气候变化对滑坡的影响关系研究是近年来滑坡灾害研究的热点问题之一。本研究以我国中更新世早中期以来黄河上游和三峡库区的滑坡为研究对象,分析了其发育期与气候变化的对应关系以及气候演变对滑坡发育的作用机理。研究认为: 1）大型古滑坡在时空分布上具有明显的多期性和时段性,大区域滑坡的广泛发育与全球古环境变化的暖湿间冰期之间呈现良好的对应关系。2）黄河上游龙羊峡-刘家峡段干流区内共发育有3期滑坡,其中早期滑坡多披覆于黄河Ⅲ～Ⅳ级阶地,光释光年龄显示其发生于MIS3时期;  晚期滑坡多披覆于黄河Ⅱ级阶地,发育于MIS1时期;  现代滑坡披覆于黄河Ⅰ级阶地,多为早期滑坡前缘因人类工程活动诱发的次级滑坡。3）三峡库区中更新世早中期以来主要发育了3期古滑坡,并以深海氧同位素的MIS5和MIS3为最多,尤其是中更新世晚期以来,滑坡数量明显增加,延续时间明显增长。     

黄河上游龙羊峡-刘家峡河段巨型滑坡形成机理分析

在阐述黄河上游龙羊峡-刘家峡河段内巨型滑坡类型及分布基本事实的基础上,分析了巨型滑坡发育与黄河形成演化历史的关联性。认为黄河上游龙羊峡-刘家峡河段的共和盆地、贵德盆地、循化盆地经历了昆黄运动B幕(距今800ka左右)的流水侵蚀夷平,而李家峡-公伯峡及龙羊峡多隆沟西段为剥蚀台面(分水岭带); 距今125ka年以来的共和运动导致了本河段的切穿贯通,并使得黄河呈阶段性塑造高陡岸坡,从而导致了早期的快速下切,并于距今30-50ka在尖扎盆地达到高值,引发了早期推移式高速巨型滑坡及堵塞河道事件和古湖岸再造型巨型滑坡; 晚期的间歇性下切,引发了晚期气候解体型巨型滑坡。因此,构造抬升致使黄河流水阶段性下切,是造就区内巨型滑坡发生的根本原因。而地震地质作用及堵河事件的发生,是区内巨型滑坡形成的诱发因素。并确定了黄河上游龙羊峡-刘家峡河段巨型滑坡形成机理可分为地震型、库岸再造型和气候解体型等3种类型。     

黄河上游龙羊峡至积石峡段巨型滑坡OSL测年

通过对青藏高原东部黄河上游龙羊峡—积石峡段10个特大型古滑坡的地质结构、地层岩性的分析,结合各滑坡特征,在特定部位进行采样,归纳整理出滑坡光释光（OSL）测年样品的5种采样方法。选取11个样品应用OSL测年方法,得到各滑坡的年龄数据,分析各样品的可靠性,并探讨其构造时间、气候变化与滑坡群发性之间的关系。研究表明,由于样品来源广泛,实验方法高效准确,OSL方法可成功地应用于滑坡年龄测定,为滑坡研究提供可靠的地质依据。研究区特大型群发性滑坡和初步划分为4期分别为130~110ka、50~30ka、12~9ka和5~3ka,并解释了各期滑坡群发的主要触发因素。     

黄河上游康杨滑坡堆积体特征及形成机理分析

滑坡堆积体特征及其成因机理是进一步研究滑坡防治及开发利用的基础与前提。位于青藏高原东北缘的黄河上游群科—尖扎盆地内的康杨滑坡属于典型的巨型古滑坡,其堆积体特征及形成机制在该地区具有典型性和代表性,具有较高的学术研究价值。结合工程地质钻孔资料,通过详细的野外调查、粒度分析等方法对康杨滑坡形态特征、形成年代、滑坡体粒度特征及其成因机理进行了研究,主要认识如下:（1）康杨滑坡为晚更新世晚期发生的泥岩滑坡,体积约为12.59×108?m3,为一典型巨型古滑坡,后壁高耸直立;（2）滑坡前缘曾滑移至黄河北岸,堆积体可能堵塞黄河,后被黄河从中部侵蚀切穿,目前在黄河北岸仍存留有古滑坡堆积体;（3）高原抬升和黄河下蚀等作用可能是滑坡发生的背景条件,降水入渗形成软弱滑带和黄河侧蚀作用可能是触发康杨滑坡的主要因素。     

青海尖扎盆地寺门村滑坡发育特征及成因分析

滑坡形成演化及复活一直是滑坡防灾减灾领域研究的热点问题。本文在对黄河上游尖扎盆地地质环境背景分析和滑坡体野外调查、遥感解译、实验测试的基础上,分析研究了盆地内寺门村滑坡的变形过程、滑带土和堆积体特征,还原了滑坡的演化过程,厘定了滑坡复活因素,提出了黄河上游滑坡堆积体开发利用对策建议,认为(1)该滑坡是2005年之前发生的老滑坡因河流侧蚀和2018年春季人工灌溉引发的复活性滑坡;(2)滑坡体综合治理应与土地整治相结合且应选择合适的灌溉方式。研究结果对于青藏高原东北缘黄河上游地区的滑坡防灾减灾及滑坡体开发利用具有重要意义。     

川西巴塘断裂带黄草坪滑坡形成机制

青藏高原东缘巴塘断裂带内地震滑坡大量发育,部分保存有堵江证据,是该区历史构造活动的良好地质载体.以川西地区巴塘县黄草坪滑坡为研究对象,通过遥感解译、现场调查、地质时代测年、工程地质分析等方法,对滑坡发育特征和形成演化过程进行研究.结果表明:①黄草坪滑坡为巴塘断裂带内全新世大型岩质滑坡,发育于中—下寒武统灰岩和板岩中,体...     

Combined numerical investigation of the Gangda paleolandslide runout and associated dam breach flood propagation in the upper Jinsha River,SE Tibetan Plateau

A large paleolandslide occurred opposite the Gangda village in the upper Jinsha River, SE Tibetan Plateau. Field geological investigations and remote sensing indicated that the Gangda paleolandslide once blocked the Jinsha River. Evidence of river blocking, including landslide dam relics, upstream lacustrine sediments, and downstream outburst sediments, has been well preserved. To understand the river-blocking event including landslide, dam breach, and associated outburst flooding, optically stimulated luminescence (OSL) dating and numerical simulations were performed in this study. OSL dating results showed that the paleolandslide dam was formed at 5.4?±?0.5 ka BP and breached at 3.4?±?0.3 ka BP, indicating that the dam lasted approximately 2000 years. The discrete element method was used to simulate the dynamics of the Gangda rock landslide based on the restored topography, while a fluid–solid coupling model was performed to simulate the landslide dam breaching and flooding. The fluid–solid coupling model can simultaneously reflect the process of landslide-dam collapse and the propagation of outburst flood. The simulated results indicate that the whole landslide process lasted about 60 s with a peak velocity of 38 m/s. It is significant that the simulated morphology of the residual landslide dam and downstream outburst sediments is consistent with the field observations. The combined numerical investigation in this paper provided new insights into the research of landscape evolution and helped to understand the chain disaster of landslide, dam breach, and flooding.

     

川西大渡河泸定段大型古滑坡发育特征与稳定性评价

川西大渡河泸定段地形地貌和地质构造复杂,地质灾害特别是古滑坡极发育.通过遥感解译、InSAR形变分析、野外调查等手段,在泸定县城上游约25 km(至姑咱镇)到下游约43 km(至得妥镇)段发现229处崩塌、滑坡、泥石流等地质灾害,古滑坡规模大、部分具有复活迹象.地质时代测年数据表明,该区古滑坡主要发育于120 ka左右...     

Tephrochronologic Constraints on Temporal Distribution of Large Landslides in Northwest Argentina

Two morphologic settings in the northwestern Argentine prone to giant mountain-front collapse-deeply incised narrow valleys and steep range fronts bordering broad piedmonts-were analyzed through detailed investigations of fossil landslides and related fluvio-lacustrine sediments. Nine different rhyodactic tephra layers were defined by geochemical fingerprinting of glass, morphology of pumice, stratigraphic relationships, and mineralogy. The age of three tephra could be determined either directly by 40Ar/39Ar dating or relatively by 14C dating of associated sediments: Paranilla Ash (723+/-89 ka), Quebrada del Tonco Ash ( approximately 30 ka), and Alemanía Ash ( approximately 3.7 ka). These units permit correlation of several spatially separate landslide deposits. Landslide deposits in narrow valleys were generated in the late Pleistocene between 40 and 25 ka and in the Holocene since ca. 5 ka and correspond to periods characterized by increased humidity in subtropical South America. In contrast, the age of large landslides in piedmont regions is significantly greater but more difficult to define by tephrochronology. However, selected deposits from this second environment have cosmogenic nuclide exposure ages of 140-400 ka. Because of the large distance of the collapsed mountain fronts from eroding streams and because of important Quaternary displacement along the mountain-bounding faults, we suggest that strong, low-frequency seismic activity is the most likely trigger mechanism for most of the landslides in this environment.