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MDES2000型微钻实验装置可模拟真实钻进情况,可开展岩石研磨性与可钻性试验、金刚石钻头性能参数及寿命试验、优化钻进规程参数试验等室内的各种微钻实验研究工作。该实验装置可通过手动或程序控制完成模拟钻进工作,能够实现钻进过程中各项钻进参数(钻压、钻速、扭矩、转速及进尺)的监测、采集、处理及存储功能,还可建立钻进参数报表文件数据库。该实验装置对岩心钻探研究工作具有很好的实际指导意义。 相似文献
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在水井等钻井工程中,广泛采用牙轮钻头钻进硬岩。为了更好地发挥牙轮钻头高效钻进的优越性,进一步提高钻进效率,延长钻头使用寿命,降低钻井成本,有必要深入讨论牙轮钻头在钻进中的钻压、转速及冲洗液等钻进参数与钻进效率的关系。1 钻压牙轮齿对岩石的破碎作用有3种:即压碎、冲击和剪切。压碎是牙轮在钻压的作用下对岩石的静力压碎作用,其效果主要取决于钻压的大小和岩石的硬度;冲击是牙轮滚动时轮齿交替作用于岩石,而使牙轮轴心产生上下往复振动,冲击作用与牙轮的齿数、转速和钻压有关,冲击力与齿数成反比,与转速和钻压成正… 相似文献
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我们在应用日产BDR5、BDR5A两种型号的钻参仪进行两个钻孔钻进参数的监测与优化设计过程中逐步认识到,要实现各钻进技术参数的准确监测和科学优化乃至实现钻进全过程的科学监控,应解决好以下几个技术问题。1钻参仪系统硬件的选择与安装1.1钻参仪系统硬件的... 相似文献
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针对科学深探的复杂性和模糊性,初步建立了大陆科学深钻钻进参数计算机模拟系统。该系统以科学深钻数据库系统为基础,以计算机成图技术为手段,实现了理想钻进数据计算与成图和实际采集数据成图,最终实现两种图形的对比。通过对比可以发现钻井过程存在的问题并及时加以纠正,达到模拟监测钻井过程,修正钻井过程。这套系统是在WIN32平台上开发成功的。系统分为数据管理、数据浏览、算法处理、回写数据库和图形输出等几个部分 相似文献
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微钻机是一种用小尺寸钻头进行模拟钻进的钻机,是进行岩石破碎和可钻性研究的必要手段。1984年地矿部频布的《金刚石岩心钻探岩石可钻性分级表》(试行)中将微钻指标列为岩石可钻性分级的指标之一,因此微钻机就成为岩石可钻性分级的主要设备之一。由于微钻要求稳定的钻压和转速,且要求将较短时间内的钻进参数和钻进指标准确无误地记录下来,因此微钻机必须能稳定加压并正确测试各钻进参数和钻进指标。我们在完成岩石可钻性分级研究课题的过程中,研制了较为适用的SDY-1型微钻机,用其钻进了400余块岩样。现将该微钻机简要介绍如下。 相似文献
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针对钻孔过程中煤体应力对钻进能量的影响问题,利用自制的恒钻压钻进试验装置开展煤岩钻孔试验,测定了钻进参数,研究了钻进能量与煤体应力的关系;利用钻屑参数计算了钻屑表面能,研究了煤体应力与表面能的关系,通过对比钻进能量和钻屑表面能,对钻孔过程中能量的转化进行了分析。研究结果表明:扭矩功在钻进能量中占比95%以上,钻进能量随煤体应力增加而增加,近似呈线性关系;钻屑量和钻屑表面能均随煤体应力增加而增加,钻进能量向钻屑表面能转化过程中存在8%~33%的能量损耗,损耗能量的形式主要是声能和钻头摩擦生热。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco. 相似文献
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Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引:4,自引:0,他引:4
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species. 相似文献
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Emmanuel Skourtsos Daniel Vachard Alexandra Zambetakis-Lekkas Rossana Martini Louisette Zaninetti 《Comptes Rendus Geoscience》2002,334(12):925-931
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931. 相似文献
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正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.) 相似文献
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正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.) 相似文献
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正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.) 相似文献
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正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus., 相似文献
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正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an 相似文献
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正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of 相似文献