粉细砂层中锚索施工涌水涌砂的处理技术

广州市良业大厦基坑支护工程存在较厚的淤泥质粉细砂层,预应力锚索锚点位置处于粉细砂层中时,锚索施工易发生涌水涌砂现象而引发基坑事故。施工过程中通过采取跟管钻进干钻成孔、墙后孔口设置止浆袋及墙后注浆的处理措施,减少了锚索施工过程中涌水涌砂现象的发生,避免了因涌水涌砂水土流失造成基坑外地面下沉而引发的基坑事故。     

管井降水技术在深基坑涌水事故处理中的应用与启示

江苏残疾人康复中心项目基坑涌水事故是因前期降水方案设计和降水施工质量控制不到位而导致,事故处理过程中通过对项目所在地地层资料深入分析,该地区为典型的长江漫滩二元地质结构,主要含水层为巨厚砂层,充分考虑该地区含水层厚、渗透系数大的特点,合理布置降水井数量及深度。对基坑内已施工的不合格降水井作报废处理、严控施工质量和运行管理,成功地解决了基坑涌水事故。本文详述了该项目事故发生和解决过程,为类似工程提供有益经验。     

珠江特大桥承台基坑突涌事故处理降水设计与施工

珠江一特大桥主墩位于珠江水域中,承台基坑施工采用锁口钢管桩围堰围护, C30水下混凝土封底。封底完成后进行围堰内排水时,基底承压水击穿了封底混凝土,造成了基底突涌事件。对比在围堰内降水和在围堰外降水两种方案后,决定采用围堰外降水的方法,将承压水位降至封底顶面以下。该方案工期短、费用低,开创了在珠江内降底承压水的先例,成功处理了围堰封底失败的事故,确保了承台的顺利施工。实践证明在深水中降承压水是可行的,降水是保证承台基坑安全的重要手段之一,为类似工程提供了宝贵的经验。     

承压水地基高层建筑基础工程施工技术分析

论述了承压水对高层建筑基坑支护、桩基础、抗浮锚杆（桩）施工的不利影响。结合工程实例,介绍了喷射注浆止水墙处理承压水的设计方法,并分析了总施工顺序、涌水钻孔处理和地下水水位观测等关键技术问题。     

压浆成桩技术的研究及应用

注浆技术在封堵地下涌水和加固岩体工程中应用甚广，利用钻孔成桩技术是在地面注浆基础上发展起来的，对地基进行处理而形成的一种注浆法。它将注浆技术与钻孔桩放了工技术相结合，应用于基坑挡土桩施工的压浆成桩新工艺，发展了现行传统桩基础施工法。     

冻结井筒冻结孔涌水机理及逆流引流注浆封堵技术

针对我国西部地区深基岩冻结井筒冻结孔涌水水害技术难题,以胡家河矿主立井井筒冻结孔水害治理工程为实例,分析了冻结孔环状导水通道生成及涌水机理,进而提出一种创新性的逆流引流注浆封堵技术,并介绍了该技术的原理及施工工艺。工程实践证明,该技术能高效快速治理冻结孔涌水水害。     

江底隧道垮塌涌水冒顶地质灾害的高压注浆防治

在江底隧道施工中，以砂岩和泥质砂岩为主的破碎、裂隙节理发育地层经钻眼爆破震动后，出现了垮塌、涌水、冒顶等事故，直接危及工程和江堤安全。针对事故突发性、破坏性及危害性，制定了严格周密的防治 方案。应用高压封闭注浆技术，进行地层改良。首先砌筑封闭墙是关键一步，务必完全封闭，并能承受高压，该墙直接影响注浆成败；其次，河床沉陷处注浆既与井下注浆相互补充，又稳固河床及江堤；第三，注浆使浆液充填裂隙通道和垮塌体空隙，在高压下充填饱满、密实；第四，浆液硬化使裂隙被封堵、垮塌体胶结成完整一体，初步达到防垮止水目的；第五，浆液养护后，破碎地层在浆液胶结硬化作用下具有一定强度，达到地层改良目的；最后，地层改良后务必钻眼芯进行检 测，以观注浆效果。经过高压封闭注浆治理，垮塌、涌水、冒顶地层得到完全改观，注浆区域内不再垮塌、涌水，使工程顺利通过该垮塌涌水区，进入下一步施工程序。     

SJP水泥浆封堵强涌水钻孔可控注浆工艺技术研究

以云南毛坪铅锌矿勘查钻孔涌水治理实践为背景,针对金刚石钻进钻孔高涌水压力和大流量涌水的工程实际,对多种涌水治理方案进行了论证分析。依据实测的涌水量及涌水压力等参数,提出了可控注浆堵涌工艺。论述了SJP水泥浆基本组成及其性能特点,可控注浆止涌的工艺技术,分析了止涌注浆孔口压力变化与孔内浆液处境之间的关系,提出了止涌注浆压力变化中的“零起点”和“零末点”及h值等新概念,以及利用压力变化判断涌水通道类型的方法等。经3个涌水钻孔的注浆止涌的实践表明,按研究成果对大涌水量钻孔进行治理,有效封堵了这3个强涌水钻孔,保证了工程顺利施工。     

特长隧道高压大流量突涌水治理施工和技术探讨

结合工程实例,介绍了长大隧道施工中高压大流量突涌水治理所采用的超前地质预报、突涌水的预防及帷幕注浆封堵等主要施工技术。并对岩溶发育富含水地区隧道工程的施工进行了分析和探讨,并提出了可行性施工方案。     

黑山煤田封堵涌水孔段的浆液和注浆方法

黑山煤田处于沙漠边侧,地层有纯砂粒构成的、透水性较強的中细砂层,这类地层中如含有承压水时,会发生钻孔涌水,对于中细砂涌水钻孔,用泥浆冲孔时,可通过适当增大泥浆相对密度,来压制地下水涌出,ZK18-28孔是涌水孔,也是采用绳索取心钻进的孔,因此不宜使用高相对密度泥浆。用套管亦未奏效。若用注浆法,对于中细砂层是不适用水泥浆的。而溶液型浆液的注浆封堵中细砂层,在技术有可行性,对于涌水压力不大的孔,又有可用低强度,因而也是低成本的浆液,因此选择了比较亷价的水玻璃类的SPN浆液,并采用双隔离塞的注浆法,在ZK18-28孔中取得了封堵中细砂涌水层的初步封堵效果。     

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.     

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     

OCEANOGRAPHY & MARINE GEOLOGY

正20140582 Fang Xisheng(Key Lab.of Marine Sedimentology and Environmental Geology,First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China);Shi Xuefa Mineralogy of Surface Sediment in the Eastern Area off the Ryukyu Islands and Its Geological Significance(Marine Geology Quaternary Geology,ISSN0256-1492,CN37     

ENVIRONMENTAL GEOLOGY

正20141810 Bian Yumei(Geological Environmental Monitoring Center of Liaoning Province,Shenyang 110032,China);Zhang Jing Zoning Haicheng,Liaoning Province,by GeoHazard Risk and Geo-Hazard Assessment(Journal of Geological Hazards and Environment Preservation,ISSN1006-4362,CN51-1467/P,24(3),2013,p.5-9,2 illus.,tables,refs.)