双泵大流量振孔高压旋喷防渗墙在粉细砂坝中的应用

振孔高喷是近几年发展的钻喷一体化、一次成墙较为先进的高喷防渗墙施工工艺,是利用高压喷射流对地层产生冲切、掺搅、升扬、置换、充填挤压、渗透固结等作用,形成所需性状的防渗固结体。本工程是首次将水力冲填粉细砂坝应用到水利枢纽大坝工程中,采用高喷防渗墙进行防渗更是初次在这样的条件中使用。大流量振孔高压旋喷施工工艺既能保证施工质量,又能提高施工工效,是高压旋喷工艺的又一次革新。     

单向高压摆喷防渗墙不分序研究与应用

高压摆喷防渗墙是成熟的施工工艺,其地层适应范围广,在国内的各种防渗工程中被广泛应用。常规的施工工艺分Ⅰ、Ⅱ序孔施工,在本工程通过试验与施工研究的不分序钻孔高喷工艺,不但有利于桩间搭接、加快施工工期,而且能够控制墙体厚度,为钻孔高喷防渗墙的推广应用奠定了基础。     

高频振锤薄壁板墙技术处理砂砾石堤基试验研究

高频振锤薄壁板墙技术在砂层堤基的垂直防渗施工中得到了广泛应用。为探索一种适用于洞庭湖区砂砾石堤基的垂直防渗施工方法,对高频振锤薄壁板墙技术的施工工艺、流程等进行了一些改进,实现了施工全过程的计算机控制。将改进后的工法应用到周家湾堤段试验工程中,并采用围井检测、钻孔取芯、测压管监测等手段检验了超薄防渗墙的成墙效果。结果表明,改进后的高频振锤薄壁板墙技术具有成墙连续、完整,防渗效果好、工效高、造价低等特点,是一种适用于处理砂砾石堤基的垂直防渗技术,可用于处理洞庭湖区及其他具有类似地质特征的堤防防渗工程。     

砂卵石层高压旋喷灌浆成墙的成孔技术

讨论了回转钻进工艺、跟管钻进工艺、反循环回转钻进工艺、顶驱式回转钻进工艺以及振孔高喷成孔工艺在砂卵石层高压旋喷灌浆成墙中成孔施工适应性、有效性以及经济性。     

高喷技术在长江垂直防渗墙复杂地层中的应用探讨

结合长江罗家潭堤段高压防渗墙工程的施工情况，对复杂地层的防渗墙施工进行了分析，并结合高喷技术的固结防渗机理提出了高压旋喷方法在复杂地层中应用时应注意的几个问题。     

振动成孔高压喷射注浆成墙技术

介绍了研究成功的振动成孔高压喷射注浆成墙技术的概况，设备配置及ＤＪ－６０型振孔高喷机，施工工艺和工程应用情况，并对其技术性，经济性作了简要分析。     

高压旋喷柱单桩承载力分析

高压喷射注浆于1968年首创于日本。我国于20世纪70年代初相继引进并开始研究高压喷射注浆技术。目前,高压旋喷工艺应用最为广泛,工艺技术最为成熟。对旋喷桩成桩质量及单桩承载力进行研究分析,为旋喷桩在地基与基础工程、水利水电工程、止水、加固工程中的应用提供设计参考依据。该试验在陕西省延安市某建成小区内选三个试验点,按不同旋喷桩施工工艺成桩,通过对桩身完整性检测、单桩承载力试验,分析旋喷桩成桩质量及单桩承载力。     

高压旋喷桩单桩承载力分析

高压喷射注浆于1968年首创于日本。我国于20世纪70年代初相继引进并开始研究高压喷射注浆技术。目前,高压旋喷工艺应用最为广泛,工艺技术最为成熟。对旋喷桩成桩质量及单桩承载力进行研究分析,为旋喷桩在地基与基础工程、水利水电工程、止水、加固工程中的应用提供设计参考依据。该试验在陕西省延安市某建成小区内选三个试验点,按不同旋喷桩施工工艺成桩,通过对桩身完整性检测、单桩承载力试验,分析旋喷桩成桩质量及单桩承载力。     

黄壁庄水库副坝高喷灌浆施工技术

为了解决黄壁庄水库副坝渗漏问题，采用高喷灌浆技术通过坝体成功建造了地下连续墙，通过检查完全满足防渗要求，高压旋喷套接单排防渗墙具有独创性和试验性。介绍了高喷灌浆工程的设计、施工方法。     

高喷灌浆技术在卵砾石层中的应用

高压喷射灌浆法具有适用的范围广、施工简便、设备简单、管理方便等许多优点,已广泛应用于水工建筑物的基础防渗工程中。结合灵关水电站尾水渠高喷灌浆施工,介绍施工过程中遇到的问题及处理措施,为类似工程提供借鉴。     

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