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1.
胡仲杰  张利明 《探矿工程》2008,35(10):28-29,32
分析了机械动力头、液压控制长行程给进钻机研发的必要性,提出了新型机械动力头钻机需要解决的相关问题,介绍了XL-5型钻机的结构形式、参数、特点及生产试验情况。  相似文献   

2.
姚克 《探矿工程》2020,47(10):48-52,71
煤矿井下智能化钻探技术及装备是煤炭生产企业急需的先进技术装备。文章介绍了相关科研院所及企业在研制自动化钻机方面取得的一些阶段性成果。由于钻探施工环节多、工艺复杂、现场条件多变,许多关键技术仍未解决,智能化程度、可靠性、适应性和实用性还需进一步提高。文章分析了钻机装备适应性、工艺复杂性及需求的多样性问题、防爆问题和钻杆连接及钻杆补充问题。指出需要开展导航与定位、程序控制自动钻进、自动装卸钻杆、参数实时监测及传输等技术攻关,从而达到智能钻机功能实用、施工高效及性能稳定的目标。同时指出真正意义上的智能化钻机大量应用还需要持续的研发投入和数年的时间过程,并提出逐步按全自动钻机阶段、智能化钻机阶段和钻孔机器人3个阶段分级实现井下智能化钻探较为适宜。  相似文献   

3.
概括地介绍了近年来我国钻掘设备的最新进展与应用情况,主要从钻掘设备的基本性能和技术原理及基本结构等方面进行介绍。介绍的主要设备有全液压岩心钻机系列、轻便设备系列、地源热泵钻机、浅海及滩涂取样钻机、全套管钻机等。  相似文献   

4.
介绍了新型声频振动钻机的发展现状、原理及优点,与传统的钻机相比,这种钻机具有高效、安全、可靠的优点;同时介绍了声频振动钻机液压系统的工作原理和各油路系统。  相似文献   

5.
CMD系列模块化钻机是顺应国家对能源开发和相应勘探钻机国情发展的需要而研制的新一代能源钻机。本文对CMD系列模块化各规格钻机的性能参数和结构功能进行了介绍,并结合该系列钻机在地热井施工中的应用情况,对该系列钻机在地热井施工中具有的优势进行了归纳和总结。  相似文献   

6.
冉灵杰  宋殿兰  卢猛 《探矿工程》2016,43(6):49-51,55
目前在普查踏勘阶段,地质工作者要求随时随地取样,迫切地需要迁移便捷、快速钻进、高效高质的便携式取样钻机。本文介绍了研制的TGQ背包式取样钻机的参数、特点及试验情况。该钻机体积小、质量轻、结构设计合理,具有高、低两挡转速,可以实现金刚石钻进、螺旋钻进工艺,可以进行斜孔钻进取心,可以解决复杂地层的取样问题。钻具采用高强度的材料,钻杆采用插装式快速连接结构,提高了加减钻杆的效率。钻机的研制打破了国外背包式轻便钻机对我国市场的垄断。  相似文献   

7.
方俊 《探矿工程》2010,37(4):1-5
深部和外围找矿工作的不断发展,需要研制出新型深孔钻机及其配套的钻探参数监测系统。全液压动力头岩心钻机将是未来深部钻探的主力钻机,CUG-2钻参仪是中国地质大学研制的与2000 m全液压动力头岩心钻机配套的钻探参数监测系统。介绍了CUG-2钻参仪的设计特点和检测参数,重点介绍了与常规转盘式、立轴式钻机不同的参数检测原理及其传感器选型安装,包括孔深、钻速、扭矩、功率和出口流量等。  相似文献   

8.
在我国西部冻土地区及干旱地区,普通取样钻机和钻进工艺钻探取样困难,因此需要对无循环取样工艺及设备进行研究。无循环钻进工艺是在钻探取样过程中,孔内没有冲洗液或虽有稳定液但不循环流动的钻进方式,这种工艺环保、取样质量高、效率高、能满足特殊地层的取样需求。介绍了无循环工艺和30m无循环取样钻机的参数特点及试验情况。钻机钻进中不需要循环介质,能够实现自装卸上下车,液压系统恒功率输出,钻机的研制为干旱地区及冻土地区增添了一种新设备、新工艺,有广阔的应用前景,将在以后的浅层取样中发挥重要作用。  相似文献   

9.
XDL-1800型全液压岩心钻机的研发   总被引:1,自引:1,他引:0  
为满足深孔绳索取心钻探需求,研究开发了XDL-1800型全液压岩心钻机。阐明了钻机的研制背景,介绍了钻机的特点、性能参数及结构和功能。  相似文献   

10.
分析了国内外车装钻机的现状;介绍了国外小型地质取样钻机装载形式、国内小型地质钻机及轻型越野车辆现状;提出了钻深15~30 m、50~60 m、100 m钻机的车载化技术方案。  相似文献   

11.
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   

12.
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   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
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   

14.
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   

15.
PALEONTOLOGY     
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   

16.
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   

17.
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   

18.
PETROLOGY     
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   

19.
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   

20.
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   

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