CFG桩与碎石桩复合桩型在液化地层中的应用

在北京三一产业园工程中采用了CFG桩与碎石桩复合地基新技术，尤其为适应消除地层液化和承载力设计需要，又为了便于施工，采用了CFG桩与碎石桩相间的布桩方案，既消除地层的液化，满足了承载力的要求，又节约了投资，实践证明这是一种既安全可靠又经济实用的方法。还对复合地基的设计计算进行了专门讨论。     

CFG桩复合地基处理技术在华电曹妃甸重工装备制造基地一期项目的应用

针对天然地基承载力较低而设计要求的承载力较高,采用CFG桩复合地基可以达到良好的效果。结合具体工程实践,对CFG桩复合地基设计计算、施工技术、处理效果方面做了较全面的介绍。     

CFG桩复合地基处理技术在北京澳洲康都住宅小区中的应用

针对天然地基承载力较低而设计要求的承载力较高、沉降变形要求又比较严格的地质条件，采用CFG桩复合地基可以达到良好的效果。结合具体工程实践，对CFG桩复合地基设计计算、施工技术、处理效果等方面作了较全面的介绍。     

CFG桩复合地基承载力计算新公式研究

CFG桩复合地基作为一种用材经济、施工便捷、加固效果良好的地基处理手段,在工程实践中得到了广泛地应用。针对CFG桩复合地基的承载力计算,分析现行《建筑地基处理技术规范》JGJ 79—2012和《建筑地基基础设计规范》GB 50007—2011中在地基承载力计算方面存在的较大差别、复合地基承载力计算过于保守等问题;以传统太沙基地基承载力理论为基础并结合工程实践经验,提出先进行桩间土深度修正再进行复合的复合地基承载力计算新方法。     

CFG桩复合地基边桩效应分析

CFG桩复合地基是软土地基处理中的一种较为有效的方法,近年来得到广泛的应用。通过有限元分析程序对CFG桩复合地基边桩效应进行分析,讨论边桩对CFG桩复合地基沉降、土体应力和承载力的影响。分析表明由于边桩的存在,限制了桩间土体的侧向挤出,减小了土体的竖向位移。同时,边桩增大了附加应力影响范围,能够在一定程度上提高复合地基的承载力,并促进了桩间土承载潜力的发挥。     

CFG桩复合地基褥垫层的设计与施工体会

根据褥垫层在CFG桩复合地基中的承载机理和特性，提出了褥垫层是复合地基的核心技术，结合工程实例，证明了通过合理的褥垫层设计和精心施工，可达到降低工程造价，提高CFG桩承载力性能和抗变形能力的目的。     

CFG桩和碎石桩复合处理液化土层的设计与施工

采用CFG桩和碎石桩相结合的复合地基方法处理黄河冲积平原新近沉积液化粉土地层，CFG桩属刚性桩，主要提高地基承载力，碎石桩则主要消除粉土层液化问题，通过该工程设计及实践，该复合地基方法处理黄河冲积平原液化地层的方法是可行的。     

CFG桩复合地基承载力工程应用分析

CFG桩复合地基作为一种新型的软弱地基处理技术，能够较好地发挥桩土共同作用，目前已被广泛应用于地基处理工程中。本文结合贵州省首例CFG桩复合地基工程，采用ANSYS软件建立复合地基模型，并考虑褥垫层影响，把计算结果与荷载试验结果进行了对比分析，得出CFG桩复合地基桩土共同作用效果明显，但目前设计桩承担荷载的比例过高的结论。据此对CFG桩复合地基的改进方向提出了建议。     

基于有限元计算的岩溶区CFG桩复合地基分析

分析了岩溶区复合地基的形成机理,并采用Plaxis有限元软件对岩溶区CFG桩复合地基的加固机理进行了研究,同时结合相关资料对岩溶区CFG桩复合地基在应用中存在的一些问题进行了探讨,得出的主要结论有:岩溶区CFG桩复合地基具有较高的承载力和有效控制沉降的能力;支承于基岩面的桩体属于摩擦端承桩或端承桩,倾斜基岩面对单桩承载力具有较大影响,建议在条件允许的情况下按照摩擦桩进行单桩承载力计算;岩溶区上覆土层土性变化大,地基处理规范中第9.2.5条CFG桩复合地基承载力的设计计算公式尚值得商榷,且规范中第9.2.8条加固区复合土层压缩模量计算公式亦值得商榷,建议采用桩长范围内土层承载力特征值的加权平均值f_sk计算复合地基承载力f_spk。      

新建城区大面积填土地基基础方案分析

某新建城区拟修建于大面积填土上,针对该新建城区的复杂工程地质条件,对天然地基、复合地基等地基基础方案的经济、技术、工期等综合分析和比较,最终采用CFG桩复合地基方案对该区独立基础和条形基础进行计算并设计布桩。CFG桩复合地基是CFG桩、桩间土、碎石垫层联合构成的复合地基,其桩身质量好,承载力可达350 kPa以上。当最大柱荷载小于或等于4 000 kN或土层中有强透水砂卵石层时,均宜采用独立柱基下CFG桩复合地基。     

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