绳索取心液动锤技术的应用与拓展

SYZX系列绳索取心液动锤已获得广泛应用并取得显著的经济效益和社会效益。介绍了如何在客户现有的绳索取心钻具中设计加装液动锤冲击装置,使之形成相同规格的绳索取心液动锤钻具,进一步拓展YZX系列液动锤的应用,促进了我国钻探技术的进步。     

蓄能式绳索取心液动潜孔锤的应用研究

蓄能式绳索取心液动潜孔锤钻具是在普通绳索取心钻具总成上端增加了发生和传递冲击载荷的结构,将冲击载荷通过绳索取心钻具外管传递至钻头。新疆达坂城黑沟-达拉地布拉克铀矿工区裂隙、构造蚀变带和构造破碎带发育,地层破碎,使用普通绳索取心钻具钻进,岩心极易堵塞、回次进尺短、频繁打捞内管、钻进效率极低。使用蓄能式绳索取心液动潜孔锤钻具钻进,增加了回次进尺,提高了钻进效率。论文依据施工现场使用情况,介绍了蓄能式绳索取心液动潜孔锤的结构和工作原理,统计、总结了应用情况,论述了绳索取心液动潜孔锤得出的应用结论。     

海底沉积地层保真取样钻具的设计及应用

钻探取样技术作为海洋地质调查和资源勘探的主要方法,在海洋探索领域占据着十分重要的地位。海底地层以松软沉积物为主,常规钻探回转取样的方法极易破坏样品原状性,且样品采取率低,难以满足科学研究的要求。研制了一种以泥浆泵压驱动的沉积物保真取样钻具,并结合绳索取心技术,实现海底沉积地层保真取样。试验证明,该海底沉积地层保真取样钻具取样成功率高、作业效率高,所采取样品原位性、原状性好,完全满足海洋地质和土工实验等对样品的严格要求。     

福建马坑外围铁矿深部勘查钻探工艺组合应用研究

针对福建马坑外围铁矿深部复杂地层钻探技术难题,开展钻探工艺的组合应用探讨,通过采用绳索取心液动锤、多功能孔底反循环单动双管取心技术等以及复杂地层护壁堵漏的技术组合（套管、泥浆、水泥）,初步解决矿区复杂地层取心难、孔壁故障频发、易斜等问题,总结了一套对后续施工具有参考价值的钻探工艺和措施。     

内蒙古曹四夭钼矿复杂地层深孔钻探技术

针对内蒙古兴和县曹四夭钼矿区构造发育,地层坚硬、岩心破碎,以及钻孔缩径、漏失、坍塌、掉块等复杂情况,总结了该矿区“硬、脆、碎”复杂地层绳索取心深孔钻探施工技术经验,从钻孔结构、泥浆配置和冲洗液选取以及钻探设备、新型SYZX75 2（77）型绳索取心液动锤钻具等方面采取措施,解决了破碎漏失、坍塌掉块及坚硬“打滑”地层的难题。着重阐述了高强度快失水堵漏技术试验,改善了复杂地层的深孔钻进环境,提高了钻探生产效率,保证了钻孔的安全终孔。     

“七五”期间新疆局的探矿新技术推广工作

我局“七五”期间在金刚石绳索取心钻探新技术的完善配套方面有了新的进展.形成了绳索取心91、75、56mm系列为主的多级口径金刚石钻探,同时引进了绳索取心冲击回转、绳索取心反循环钻头、螺杆钻具、连续造斜器等新技术,基本解决了深孔、坚硬“打滑”地层、易斜地层的钻探技术问题.天湖铁矿     

SYZX96型绳索取心液动锤在甘肃李坝金矿

在陇南紫金李坝金矿钻探施工中遇强水敏性、破碎、复杂地层,普通绳索取心钻具岩心采取率低,平均采取率86.5%,回次进尺少,多在1 m以下,最小回次进尺只有20～30 cm,钻进效率低,平均台班进尺约5 m。通过使用SYZX96型绳索取心液动锤,钻进效率明显提升,平均岩心采取率提高8%,平均回次进尺提高50%,平均台月效率提高17.5%,纯钻时间增加到了60%左右。共完成6个钻孔,进尺2488 m,其中2个钻孔采用SYZX96型绳索取心液动锤,效果明显。总结出适合强水敏性、破碎、复杂地层绳索取心液动锤的使用经验,为类似地层钻探施工提供技术借鉴。     

SYZX96/75绳索取心液动锤钻具的应用效果

主要介绍了SYZX96/75绳索取心液动锤钻具在湖南常德仙人金矿软硬交替复杂地层中的应用情况,总结了其中的施工经验。该孔使用SYZX96/75绳索取心液动锤钻具,大幅度提高了回次长度,减少了辅助时间;对提高破碎地层的取心效果起到了关键作用;降低孔斜效果显著。     

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。     

贵州省水银洞金矿区簸箕田矿段ZK42316钻孔施工技术

从分析钻孔钻遇地层入手,总结了贵州省水银洞金矿区簸箕田矿段ZK42316钻孔设计、钻探施工技术、Q系列绳索取心钻具的使用效果、抑制性泥浆护壁技术应用情况等钻探施工技术经验。     

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.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

NONMETALS DEPOSITS

正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)     

MATHEMATICAL GEOLOGY

正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,     

PROSPECTING EXPLORATION

正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)     

STRUCTURAL GEOLOGY

正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-     

STRUCTURAL GEOLOGY

正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with