西平铁矿深孔绳索取心钻探技术应用

绳索取心钻进技术已经广泛用于钻探工程中,深孔钻探采用绳索取心技术可大大提高钻探效率和钻探质量。结合西平铁矿对深孔绳索取心钻探技术进行了应用研究,阐述了深孔绳索取心钻探过程中,钻孔结构的优化以及匹配合理钻具型式的重要性。还就泥浆体系和孔斜控制等关键技术进行了探讨。     

浅谈绳索取心钻探技术用于煤田勘探的几个问题

绳索取心钻探技术在我国金属矿床的岩心钻探当中已经得到了较为普遍的应用。然而，在煤田钻探施工中由于其特有的复杂性及人们的认识等诸方面原因，使得绳索取心在煤田勘探领域中的运用还处于起步状态。近二年来，一部分施工单位对煤田绳索取心钻探进行了初步尝式，取得了喜人的效果，显示了绳索取心钻探用于煤田勘探的美好前景。     

浅谈绳索钻探工艺在煤田钻探中的合理应用

主要分析了绳索取心钻进工艺在煤田沉积岩地层钻探中的应用方法与存在问题。煤田沉积岩绳索取心钻进大幅度提高了效率和质量,减轻了工人的劳动强度,降低了成本,加快了勘探进度,但是煤系地层的自有特性还有很多制约绳索取心钻进地方,通过不断地在技术上进行研究与探索,必将使绳索取心钻进在煤田钻探的应用中上一个新的台阶。     

绳索取心技术在钻探施工中的应用

本文介绍了绳索取心钻探工艺钻具的结构,钻进规程的各种具体参数,注述了绳索取心钻探技术的主要优越性及实际工作中的应用。     

绳索取心工艺在大口径深部钻探中的应用研究

绳索取心工艺具有效率高、取心质量好等优点,所以,在小口径固体矿产钻探工程中已得到推广应用。但是,在沉积地层大口径深孔钻探中应用较少。文中针对绳索取心和石油钻井工艺各自优缺点,提出了增加钻孔和钻具的环空间隙,采用大泵量、高上返速度的石油钻井和绳索取心"二合一"钻探技术思路,结合河南叶舞凹陷盆地2630m盐矿(地热)勘探孔进行了生产性试验,就试验中存在的主要问题进行了分析研究,并提出了具体措施。通过试验证实:绳索取心技术在大口径深部钻探工程应用可行,且具有成本低、安全可靠等优点;同时,增加泵量和环空间隙可以避免岩屑重复破碎,从而可大幅度提高钻探效率。     

南方不稳定煤田绳索取心问题及对策

近年来，绳索取心钻进工艺在南方不稳定煤田试验应用，对于提高钻探效率，加速煤田地质勘探步伐起了积极作用。我局在赣西煤田开动了三台S75绳索取心钻机，在提高煤田钻探技术经济效果和质量方面，显示了这种新工艺的优越性，如下表所示。绳索取心在煤田应用，虽然见到了成效，但仍存     

国产绳索取心钻杆用冷拔无缝钢管性能分析

介绍了国内绳索取心钻探技术研发和应用情况,总结了目前国产绳索取心钻杆的型式、品种及采用的材质等,对国产绳索取心钻杆用冷拔无缝钢管的技术性能进行了全面比对。     

水利水电工程钻探绳索取心钻进中压水试验研究

在水利水电钻探中要充分发挥绳索取心钻进的优势,压水试验和绳索取心的有机结合是必须解决的重要问题,分析对比了全孔钻进双栓塞压水试验方案和不提大钻压水试验方案的优缺点,得出不提大钻压水试验方案能够很好的解决绳索取心应用到水利水电钻探中的适应性问题。     

河北涞源木吉村铜矿ZK6801孔深孔绳索取心钻进体会

结合河北涞源木吉村铜矿ZK6801孔深孔绳索取心钻进实践,总结了金刚石绳索取心钻探工艺在地层复杂的深孔钻探施工的几点经验和体会,着重论述了泥浆护壁堵漏、水泥浆护壁以及套管护壁的应用原则。     

国内常规海洋地质钻探取心技术进展

为实现在海洋地质钻探中高效、便捷地采获海底各类地层样品,设计研发了绳索取心泥浆静压活塞取心钻具、海洋砂质地层绳索取心钻具和液动冲击绳索取心钻具,并在南海进行了钻探试验和作业。结果表明,泥浆静压活塞取心钻具能有效减少样品扰动,原始结构较为完整,海洋砂质地层绳索取心钻具和液动冲击绳索取心钻具在粉砂层、砂层中的岩心采取率高于规范要求,能够满足作业需求。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

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.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

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.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

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.     

Late Wuchiapingian (Late Dzhulfian,early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon,central–eastern Peloponnesus,Greece)

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.     

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.)     

GEOCHEMICAL EXPLORATION

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.)     

MICROPALAEONTOLOGY

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.)     

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.,     

ENVIRONMENTAL GEOLOGY

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     

PROSPECTING EXPLORATION

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