青藏高原古人类的艺术创作——基于中更新世手脚印形态分析     

章典  王蕾彬  MatthewR Bennett  张盛达  张海伟  李腾  张悦  苏佳佳  王晓晴 《地理科学》2022,42(5):782-790

在第二次青藏科考过程中,作者在西藏自治区拉萨市邱桑村的古泉华沉积上新发现了由5个手印和5个脚印组成 “岩面艺术” （parietal art）。对这一“岩面艺术”进行解剖学测量、3D 模型模拟、铀系测年和手脚印形态分析后,得到以下认识：① “岩面艺术”是在泉华没有成岩之前由古人类有意压上去的;② “岩面艺术”所在岩层的U/Th年代为226~169 ka B.P.,这其中包含一个手指印岩层的表面直接年龄（207~188 ka B.P.）;③ 这一发现是迄今为止发表的古人类在青藏高原上活动的最早记录之一,也为古人类适应高寒、低氧环境提供了新的证据;④ 此岩面艺术是目前世界上已知的最古老的艺术,上面的手印也是古人类留下的最早的手印;⑤ 这一原始的岩面艺术表明,创作它的古老人种可能具有一定的认知和空间感知能力,此岩面艺术的发现也将有可能改写人类艺术史,并且加深我们对已消失的古人类认知水平的认识。  相似文献   

Vestiges of the Kerguelen Mantle Plume in Southern Tibet:Evidence from 123–117 Ma Magmatism in the Dingri Area of the Central Tethys Himalaya     

YAN Songtao  WU Qingsong  LI Hu  DAI Xuejian  ZHU Lidong  WANG Jie  XIN Chongyang 《《地质学报》英文版》2023,97(4):1163-1180

The widely distributed Early Cretaceous magmatism in the Tethys Himalaya(TH) of southern Tibet is related to the Kerguelen mantle plume. Associated magmatic activity products are distributed in the eastern TH, where the active age is earlier than the peak ages of the Kerguelen mantle plume. This study investigated magmatic activity of the Dingri area in the central TH which was coeval with the Kerguelen mantle plume. The intrusion in the Dingri area contains diabases and monzonites. The zircon a...  相似文献   

钒矿床研究进展与展望          下载免费PDF全文

杨立飞  李增华  欧阳永棚  邓腾  邓友国  孟德磊  郑华 《沉积与特提斯地质》2023,43(1):48-58

钒是工业国家重点关注和争夺的资源,已被部分国家列为关键金属。本文对矿床类型、地质特征、时空分布以及成矿机制等方面进行了系统总结和分析,以期丰富钒成矿理论研究,为提高钒资源的预测和勘查效率提供支撑,为钒资源储备提供保障。研究发现,钒矿床主要分为岩浆型和沉积型,其中岩浆型钒矿床（主要指钒钛磁铁矿床）成矿与铁镁质–超铁镁质岩及部分斜长岩侵位密切相关,成矿年龄与成岩年龄一致,钒可能来自上地幔并在岩浆演化过程中结晶析出赋存于含钒钛磁铁矿中;沉积型钒矿床多形成于黑色岩系及部分砂岩中,成矿多集中于上寒武世,钒可能来自海水和赋矿围岩,由于氧化还原电位降低,以吸附和类质同象等形式赋存于有机质和硅酸盐矿物中。同时,钒矿床的成因研究存在较多问题,如成矿物质钒的来源、迁移过程、赋存形式及富集条件等。笔者建议在今后研究中通过分析钒化学行为、围岩沉积物理–化学–生物条件及岩浆演化的地质动力背景来解析钒矿床成因机制。  相似文献   

基于机器学习模型的淮河流域中长期径流预报研究     

胡义明  陈腾  罗序义  唐超  梁忠民 《地学前缘》2022,29(3):284-291

准确可靠的中长期径流预报是支撑水资源科学调配、提高水资源利用效率的关键。本研究采用AdaBoost模型(AdB)、随机森林模型(RF)和支持向量机模型(SVM)进行淮河流域王家坝和蚌埠站当年11月至次年10月共12个月的中长期径流预报研究。采用置换准确度重要性度量法从130项气象-气候因子及前期降雨/流量构建的1 562个因子变量中筛选出影响各月径流的关键因子,构建了基于AdB、RF和SVM模型的各月径流预报模型,模型参数采用随机搜索技术并结合交叉验证方式确定。采用变幅误差合格率和等级(五级)预报合格率指标对模型的预报精度进行了评估。变幅误差合格率指标表明,王家坝12个月的平均合格率分别为99.8%(AdB)、96.6%(RF)和95.9%(SVM),蚌埠站分别为100%(AdB)、94.8%(RF)和93.8%(SVM);等级预报合格率指标表明,王家坝12个月的平均合格率分别为79.0%(AdB)、76.4%(RF)和79.9%(SVM),蚌埠站分别为81.0%(AdB)、75.6%(RF)和76.6%(SVM)。模型均具有较好的预报效果,但RF和SVM模型对于高流量值的预报存在偏低现象,AdB模型整体上优于RF和SVM模型。  相似文献   

基于窗口理论的时频分析方法研究     

贺梅  刘财  周寅  罗腾  张鹏  丁玲 《世界地质》2015,34(2):476-483

通过对比短时Fourier变换、连续小波变换、S变换、广义S变换等时频分析方法发现,从窗的维度看,它们具有统一的内积形式,差别在于窗函数中σ(f)的取值。通过分析相应方法中σ(f)随信号频率的变化规律,以及随之产生的时窗与时频分辨率问题,解释广义S变换的相对优越性。将广义S变换应用于四类薄互层模型,研究薄互层时频特性与地质特性的对应关系,指导地层旋回方向的预测。  相似文献   

河南栾川南泥湖和上房沟花岗岩体黑云母成分特征及其成岩成矿意义     

唐灿辉  张寿庭  张云辉  曹华文  唐利  陈慧军  许腾  武宗林 《矿物岩石地球化学通报》2015,(3)

河南栾川南泥湖和上房沟花岗岩体与钼多金属成矿作用密切相关。本文用电子探针测试方法,分析了南泥湖岩体和上房沟岩体中黑云母的成分特征。结果表明,2个岩体中黑云母均具有高硅、富镁、低铝和贫铁的特征,属镁质黑云母。2个岩体的结晶温度分别为730~830℃和750~860℃,氧逸度(logfO2)分别为-8.5~-7.0和-8.0~-6.5,结晶压力和深度分别为72~120MPa、54~127MPa和2.62~4.37km、1.97~4.63km,有利于南泥湖-三道庄和上房沟超大型钼矿床的形成,地球化学特征显示2个岩体均属壳幔混源的Ⅰ型花岗岩,属深源中浅成花岗岩。  相似文献   

变权组合预测模型在大坝沉降监测中的应用   总被引：1，自引：0，他引：1  

谢朋朋  黄腾  刘阳 《测绘工程》2015,(4):74-76

为探讨变权组合预测模型在变形监测中的应用,以监测某大坝沉降量为实例,研究基于线性回归预测模型和灰色模型GM(1,1)的变权组合。通过预测该大坝坝内沉降量,比较两种单一预测模型和变权组合预测模型的预测误差平方和,证明变权组合预测模型在沉降预测中具有更好的预测精度。  相似文献   

Middle and Late Devonian microbial carbonates,reefs and mounds in Guilin,South China and their sequence stratigraphic,paleoenvironmental and paleoclimatic significance   总被引：2，自引：0，他引：2  

Pedoja Kevin 《中国科学D辑(英文版)》2005,48(11):1900-1912

The importance of calcimicrobes and microbialite in carbonate platform and reefal environments has been stressed in recent literature. Burne and Moore[1] introduced the term microbialite to describe the clotted, laminated and undifferentiated fabrics formed by mi-crobial communities. Microbialites are organosedi-mentary deposits that have accreted as a result of ben-thic (prokaryotic or eukaryotic) communities, trapping and binding detrital sediment[1]. Microbial organisms and microbialite are…  相似文献   

Carbonate biomineralization induced by soil bacterium Bacillus megaterium     

Bin Lian  Jun Chen  H. Henry Teng 《Geochimica et cosmochimica acta》2006,70(22):5522-5535

Biogenic carbonates spawned from microbial activities are common occurrences in soils. Here, we investigate the carbonate biomineralization mediated by the bacterium Bacillus megaterium, a dominant strain separated from a loess profile in China. Upon completing bacterial cultivation, the ensuring products are centrifuged, and the resultant supernatant and the concentrated bacterial sludge as well as the un-separated culture are added separately into a Ca-CO₃ containing solution for crystallization experiments. Results of XRD and SEM analysis indicate that calcite is the dominant mineral phase formed when the bacteria are present. When the supernatant alone is used, however, a significant portion of vaterite is also precipitated. Experimental results further reveal that the bacteria have a strong tendency to colonize the center area of the calcite {1 0  4} faces. Observed crystal morphology suggests that the bacterial colony may promote the growth normal to each individual {1 0  4} face of calcite when the cell concentration is high, but may retard it or even cause dissolution of the immediate substrate surfaces when the concentration is low. SEM images taken at earlier stages of the crystallization experiments demonstrate the nucleation of calcite on the bacterial cell walls but do not show obvious morphological changes on the nanometer- to submicron-sized nuclei. δ¹³C measurements unveil that the crystals grown in the presence of bacteria are further enriched in the heavy carbon isotope, implying that the bacterial metabolism may not be the carbon sources for the mineralization. Based upon these findings, we propose a mechanism for the B. megaterium mediated calcite mineralization and conclude that the whole process involves epi- and inter-cellular growth in the local microenvironments whose conditions may be controlled by cell sequestration and proton pumping during bacterial respiration.  相似文献   

基于时间序列法的北京市需水量预报(英文)   总被引：2，自引：0，他引：2  

翟远征  王金生  滕彦国  左锐 《地理学报(英文版)》2012,22(5):919-932

It is essential to establish the water resources exploitation and utilization planning,which is mainly based on recognizing and forecasting the water consumed structure rationally and scientifically.During the past 30 years(1980-2009),mean annual precipitation and total water resource of Beijing have decreased by 6.89% and 31.37% compared with those perennial values,respectively,while total water consumption during the same period reached pinnacle historically.Accordingly,it is of great significance for the harmony between socio-economic development and environmental development.Based on analyzing total water consumption,agricultural,industrial,domestic and environmental water consumption,and evolution of water consumed structure,further driving forces of evolution of total water consumption and water consumed structure are revealed systematically.Prediction and discussion are achieved for evolution of total water consumption,water consumed structure,and supply-demand situation of water resource in the near future of Beijing using Time Series Forecasting Method.The purpose of the endeavor of this paper is to provide scientific basis for the harmonious development between socio-economy and water resources,for the establishment of rational strategic planning of water resources,and for the social sustainable development of Beijing with scientific bases.  相似文献