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四川元坝地区陆相下沙溪庙组—须家河组地层岩性复杂、可钻性差、研磨性强、地层压力高,使用牙轮钻头、PDC钻头等常规钻井技术钻速慢、周期长、效率低,引进扭力冲击器+PDC钻头、孕镶金刚石钻头+涡轮等进口提速工具费用昂贵,提速效果明显,但经济效益差。为降低钻井成本,结合地层地质特性,开展了个性化钻头及配套提速工具的研制及优选,形成了元坝高研磨性地层提速提效集成钻井技术,即自流井组珍珠冲段以上地层采用研制的KS1362ADGR型PDC钻头+国产大扭矩螺杆马达;珍珠冲及须家河组地层优选国产NR826M型孕镶金刚石钻头+高转速螺杆马达。通过3口井现场试验表明:同比2012—2013年完钻井指标,平均机械钻速提高64.7%;在井段长度增加8.7%的情况下,平均钻井周期缩短36.3%。该技术将对川东北、川西须家河组等高研磨性地层钻井具有指导作用。 相似文献
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梨树断陷区块登娄库组、营城组、沙河子组、火石岭组地层可钻性差、岩性较致密、局部含砾严重,并且沙河子组局部层位岩石硬度达到7级,采用常规钻井技术,存在牙轮钻头效率低、寿命短等问题;各种型号PDC钻头试用后效果不理想。通过采用涡轮钻井技术,平均机械钻速提高了4倍,钻井周期缩短,钻井综合成本大大降低。实践证明,高速涡轮钻具+孕镶金刚石钻井技术是高研磨性、高抗挤强度、高温地层深井钻进提速的有效技术。 相似文献
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水平井技术是实现致密油开发的重要途径。自2013年开始,大庆油田在齐家、长垣等3个致密油区块开展了水平井井组开发先导性试验,其中齐家区块施工难度最大,针对该区块水平井水平段长、位移大的特点,及钻遇地层岩石可钻性差、三维扭方位难度大、机械钻速低、钻井周期长等主要技术难点,在分析地层特征的基础上,通过优化井身结构,井眼轨迹控制,优化三维井眼轨迹,开展个性化钻头、降摩减扭措施和配套工具的技术攻关及现场应用,初步形成了一套大庆油田齐家区块致密油水平井钻井提速技术,并取得了较好的应用效果,为大庆油田致密油长水平段水平井进一步提速及规模应用奠定了基础。 相似文献
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东海油气田是我国海上当前勘探开发的主要区域之一,该油田主要储层埋藏较深,钻井过程揭开多套地层,深部地层岩石抗压强度达到了100 MPa以上,可钻性差、地层温度较高。钻井过程中面临井壁失稳、机械钻速低、轨迹难以控制等诸多问题。针对上述问题,通过对国内外相关提速技术的调研,优选液力冲击工具开展东海深部地层的钻井提速研究与实践。该工具结构简单、可靠性较高,通过加放位置分析、操作参数优选,使现有钻井设备与工艺参数基本不改变,而创新性地提出了旋转导向与液力冲击工具配合,最终在X4H井的应用中机械钻速提高30%~200%,效果显著。 相似文献
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随着鄂北大牛地气田的持续建产,水平井规模开发已成为气田开发的重点技术。但在水平井施工中,由于诸如地层岩性变化,可钻性差异大问题;泥岩稳定性问题;低破裂压力层段地层漏失问题等;钻井液润滑性和携岩性能和岩屑床清除问题;以及地层变化、尖灭使得突然钻遇泥岩、煤层,发生坍塌、掉块等不可控因素,对水平井钻井提速提效产生不利影响和困难。本文分析了影响水平井提速提效的瓶颈问题,提出较为完善的技术方案,从而实现水平井施工安全、快速、高效钻进的目的。 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