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1.
介绍了GPS RTK技术的基本特点,说明了GPS RTK作为一种高科技的三维测量工具在工程测量方面所具有的优越性及应用的广泛性。结合城市道路改造中的实践,阐述了该技术在工程测量中的基本应用步骤。为更好地利用GPS RTK技术,提高工程测量精度和作业效率提供参考。 相似文献
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在土地测量工作中,RTK技术已作为主要测绘技术手段广泛地得到运用。然而,RTK测量精度究竟如何,是每个从事测绘技术工作者所关心的问题。本文将通过土地测量实例的实践数据比较,对RTK的测量精度进行探讨。 相似文献
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分析实时GPS误差的来源,并用RTK测量技术来检核GPS静态相对定位所测设的E级控制点,对其测量精度做出相应的比较分析,阐述GPS静态相对定位和RTK定位技术在煤田勘探测量中的应用. 相似文献
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RTK测量技术因具有作业精度、作业效率高等明显优势,被广泛应用于矿区测量工作中。宁东煤田梅花井井田．总测量面积约70km^2,测区内沙漠较多．原有控制点破坏严重,采用常规测量手段施测十分困难,为此采用RTK技术,并建立了精度高、布局合理的矿区控制网。控制网由已知点4个,未知点15个组成,共处理基线65条。通过对控制网进行技术分析,发现RTK测量的各项指标均优于规范要求。结合GPS RTK技术在该矿区测量中的应用实例．指出RTK技术从基准站与流动站的设置至数据检验各程序中应注意的问题,并认为RTK技术是矿区测量工作的优先选择。 相似文献
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GPS-RTK技术在公路测量中的应用 总被引：1，自引：0，他引：1
RTK技术是在GPS基础上发展起来的一种新的常用的GPS测量方法,在很多领域已得到广泛的应用,GPS—RTK技术对公路测量的作业方式产生了很大的变革,极大地提高了测绘精度。本文从公路测量工程的几个关键过程阐述了应用GPS-RTK技术进行野外数据采集技术及处理方法。 相似文献
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GPS技术是测量技术革命性进步,特别是实时动态(RTK)定位技术效率高,精度也较高,其应用及开发的前景十分广阔。本文简要阐述了GPS-RTK的工作原理,结合管线测量工程的应用,介绍了用GPS-RTK技术进行图根控制测量的方法,并对影响GPS-RTK测量精度的因素进行了分析,提出了相应的对策。 相似文献
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GPS RTK技术用于滑坡动态实时变形监测的研究 总被引：2，自引：0，他引：2
为了研究GPS RTK技术用于滑坡动态变形监测的精度和可靠性,本文结合某类滑坡的大型物理模型试验,在滑坡体上布设了若干监测点,并用GPS RTK技术、全站仪三维测量技术和GPS单历元定位技术实时跟踪监测了该滑坡在自然状态下从稳定到产生破坏的全部过程。通过对监测数据的处理和分析,获得了RTK技术用于滑坡变形监测的可靠性和精度等技术参数,即在基准站和流动站同步观测到的卫星数在7颗以上且RTK系统的数据链能够正常工作的情况下,RTK测量的平面和高程精度就能分别控制在15mm和20mm以内。研究结果表明,RTK技术在一定条件下完全可用于滑坡灾害的动态实时变形监测。 相似文献
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GPS-RTK测量技术具有较高速度和精度。电台模式和CORS模式是RTK测量比较常用两种模式,而常规的RTK作业具有一定的局限性,测站周围地形地物和无线电都会对RTK的测量精度造成一定影响。在参考相关研究成果的基础上,对电台模式和CORS模式这两种较常用的模式从工作原理、设备配置、作业流程与误差处理等方面进行了对比分析,此外并对GPS技术在控制测量和高程控制测量方面的应用进行了分析。 相似文献
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GPS RTK定位技术测量精度高、测站间无需通视、操作简单,在测量领域有着广泛的应用。本文结合工程实例介绍了利用GPS RTK技术进行公路测量的方法及建议。 相似文献
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The marine Cretaceous of China is distributed mainly in southwestern Xinjiang, the West Kunlun Mountains, the Karakorum Mountains and most parts of Xizang (Tibet), with findings even from Taiwan.The marine Cretaceous of China may be divided into three sedimentary belts according to the lithologic and tectonic characters, biological provinces and the different modes of deposition.On the basis of recent research on the Cretaceous marine strata and faunas in China, the lithostratigraphic and biostratigraphic sequences have been preliminarily established and the division and correlation of strata and boundaries between the Jurassic and Cretaceous, Lower Cretaceous and Upper Cretaceous, as well as Cretaceous and Tertiary outlined; the position of the beach line of the Laurasian landmass in China and the events of the tectonic movement and the transgression and regression during the Cretaceous period are discussed. 相似文献
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铁板砂是一种特殊的沉积地貌,其性质和形成演化涉及海洋沉积动力、海洋工程地质等学科方向,对海岸防护、航运安全和海洋工程建设有重要影响。介绍了铁板砂的概念、特征和分布,以铁板砂形成和演化机制为主线,从原生沉积、冲刷分选和液化渗流3种模式出发,对国内外铁板砂研究现状进行总结和论述,分析了3种模式的优缺点和适用条件,从研究思路和研究方法等方面对铁板砂的研究趋势进行了展望,指出基于海洋土力学与沉积动力学相结合的思路,开展水体-床面-床内耦合的多要素同步观测,构建机制清晰的物理模型和定量评价的数学模型是今后铁板砂研究的发展方向。 相似文献
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江苏侏罗系—白垩系火山岩地层对比及划分探讨 总被引：1，自引：0，他引：1
排除火山岩系的复杂性产生的对区域地质调查和地层划分造成的干扰,综合生物化石、同位素年龄及地球化学特征等数据提出了江苏地区侏罗系—白垩系火山岩系地层的层序划分,建议将燕山运动以来侏罗系—白垩系火山喷发岩系的三大旋回所形成的各火山岩和火山碎屑岩组,包括龙王山组、云合山组、大王山组、姑山组、娘娘山组名称取消,并将其作为不同时期的火山喷发岩系夹层分别归入西横山组、浦口组、赤山组,同时将苏北地区的象山群也归入西横山组,将白垩系底界放在西横山组与苏南所见的象山组之间。 相似文献
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钾霞橄黄长岩是一种非常稀少的超钾质火山岩,也是一个岩石系列,包括黄长煌斑岩、橄榄石黄长岩、白橄黄长岩、橄辉钾霞岩和乌干达岩等多种岩石类型。钾霞橄黄长岩包含了丰富的地球内部的深部信息,是火成岩石学中一个新的研究热点。结合对意大利和中国西秦岭钾霞橄黄长岩和碳酸岩的野外观察和研究,简要介绍了超钾质岩石的定义和分类以及钾霞橄黄长岩的岩石学和地球化学特征,并对钾霞橄黄长岩及共生的碳酸岩的成因和构造环境作了简要的评述。 相似文献
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论中国前寒武纪地质时代及年代地层的划分 总被引：7，自引：1，他引：7
Wang Hongzhen 《地球科学》1986,(5)
本文讨论了前寒武纪地质时代和年代地层划分的原则和命名,提出建立隐生宙、原生宙和显生宙。隐生宙包括冥古代和太古代;原生宙分始元代、中元代和新元代。划分中的重要改变是根据新的年龄值数据将五台群归入太古代,将长城系底界改为1700Ma;并根据蠕虫-须腕动物群的出现,将震旦纪归入古生代。文中还阐述了作者对前寒武纪时代划分的新观点。 相似文献
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《Geoforum》2017
By engaging with ‘pro-anorexia’ and ‘food porn’ on the Internet, this paper explores eating in cyberspace. Reflecting on the ways in which virtual, but affective, consumption is central to both food porn and pro-anorexia websites, the paper asks what the act of eating ‘triggers’ and produces, connects and displaces. It traces how eating in, and through, cyberspace shapes the biological materialities of bodies whilst also collapsing neat distinctions between offline and online worlds. Virtual vectors of spectating, salivating and digesting are disembodied and yet corporeal. Eating is seen to take place beyond and among bodies and to be dissipated both spatially and temporally. As such, cyberspace is outside and other to lived corporeality, and yet also folded into and productive of the intimate geographies and embodied subjectivities of everyday lives. As eating takes myriad forms across the de-materialised viscerality of the Internet, it also emerges as central to the production and ‘matter(ing)’ of cyberspace itself; this is (an) eating space in which what is eaten, by whom and with what bodies, perpetually shifts. Thus, seeking to contribute to geographical scholarship on affect and food, this paper engages with eating as both the subject of enquiry and also as a productive pathway into an interrogation of cyberspace and its place within the affective productions of the everyday. It suggests that this is a key site in which to explore the intimate socialities, materialities and biopolitics of food. 相似文献
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At Segura, granitic pegmatite veins with cassiterite and lepidolite, hydrothermal Sn–W quartz veins and Ba–Pb–Zn quartz veins intruded the Cambrian schist–metagraywacke complex and Hercynian granites. Cassiterite from Sn–W quartz veins is richer in Ti and poorer in Nb and Nb+Ta than cassiterite from granitic pegmatite. Wolframite from Sn–W quartz veins is enriched in ferberite component. The Sn–W quartz veins contain pyrrhotite, arsenopyrite, sphalerite, chalcopyrite, stannite, matildite and schapbachite and the Ba–Pb–Zn quartz veins have cobaltite, pyrite, sphalerite, chalcopyrite, galena and barite, which were analyzed by electron microprobe. The presently abandoned mining area was exploited for Sn, W, Ba and Pb until 1953. Stream sediments and soils have higher concentrations of metals than parent granites and schists. Sn, W, B, As and Cu anomalies found in stream sediments and soils are associated with Sn–W quartz veins, while Ba, Pb and Zn anomalies in stream sediments and soils are related to Ba–Pb–Zn quartz veins. Sn, W, B, As, Cu, Ba, Pb and Zn anomalies in stream sediments and soils are also related to the respective old mining activities, which increased the mobility of trace metals from mineralized veins to soils, stream sediments and waters. Stream sediments and soils are sinks of trace elements, which depend on their contents in mineralized veins and weathering processes, but Sn, W and B depend mainly on a mechanic process. Soils must not be used for agriculture and human residence due to their Sn, B, As and Ba contents. Waters associated with mineralized veins were analyzed by flame atomic absorption spectroscopy (FAAS) and ICP-AES have high As, Fe and Mn and should not be used for human consumption and agriculture activities. The highest As values in waters were all related to Sn–W quartz veins and the highest Fe and Mn values were associated with the Ba–Pb–Zn quartz veins. No significant acid drainage was found associated with the old mine workings. 相似文献
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Particle size scales and classification of sediment types based on particle size distributions: Review and recommended procedures 总被引：1，自引：0，他引：1
This paper provides a review of different particle size scales, size class terminology and particle size distribution (‘textural’) classification schemes which are widely used in sedimentology, geomorphology, soil science, aquatic ecology and civil engineering. It is concluded that a revised system of size class nomenclature, based on the Udden (1898) and Wentworth (1922) schemes, provides the most logical and consistent framework for use with sediments and a wide range of other particulate materials. A refined scheme is proposed which has five first‐order size classes (boulder, gravel, sand, silt and clay), each of which has five second‐order subdivisions with limits defined at one phi intervals. The scheme is simple and intuitively easy to understand. The paper also provides a review of previous schemes that have been proposed to describe and classify sediments on the basis of the proportions of gravel, sand and mud, or sand, silt and clay using trigons (also termed ternary diagrams). Many of these schemes do not have a logical basis and provide limited or uneven resolution. New gravel, sand and mud and sand, silt and clay classification systems are proposed that are both more logical and provide greater discriminatory power than previous schemes; they are therefore more suitable for use in environmental and forensic investigations. A new Microsoft Excel® program, freely available to download from http://www.kpal.co.uk , allows rapid classification of sediments based on the proportions of gravel, sand and mud and sand, silt and clay proportions and graphical comparison of the data for different sample groups. 相似文献
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Palladium, Platinum and Gold Concentrations in Fengshan Porphyry Cu–Mo Deposit, Hubei Province, China 总被引：1，自引：0，他引：1
Abstract: The Fengshan porphyry-skarn copper–molybdenum (Cu–Mo) deposit is located in the south-eastern Hubei Province in east China. Cu–Mo mineralization is hosted in the Fengshan granodiorite porphyry stock that intruded the Triassic Daye Formation carbonate rocks in the early Cretaceous (~140 Ma), as well as the contact zone between granodiorite porphyry stock and carbonate rocks, forming the porphyry-type and skarn-type association. The Fengshan granodiorite stock and the immediate country rocks are strongly fractured and intensely altered by hydrothermal fluids. In addition to intense skarn alteration, the prominent alteration types are potassic, phyllic, and propylitic, whereas argillation is less common. Mineralization occurs as veins, stock works, and disseminations, and the main ore minerals are chalcopyrite, pyrite, molybdenite, bornite, and magnetite. The contents of palladium, platinum and gold (Pd, Pt and Au) are determined in nine samples from fresh and mineralized granodiorite and different types of altered rocks. The results show that the Pd content is systematically higher than Pt, which is typical for porphyry ore deposits worldwide. The Pt content ranges from 0.037 to1.765 ppb, and the Pd content ranges between 0.165 and 17.979 ppb. Pd and Pt are more concentrated in porphyry mineralization than skarn mineralization, and have negative correlations with Au. The reconnaissance study presented here confirms the existence of Pd and Pt in the Fengshan porphyry-skarn Cu–Mo deposit. When compared with intracontinent and island arc geotectonic settings, the Pd, Pt, and Au contents in the Fengshan porphyry Cu–Mo deposit in the intracontinent is lower than the continental margin types and island are types. A combination of available data indicates that Pd and Pt were derived from oxidized alkaline magmas generated by the partial melting of an enriched mantle source. 相似文献