长时间尺度珠江口河网水下地形演变过程三维可视化实现及分析

阐述了长时间尺度珠江口河网水下地形演变过程中的三维可视化实现过程及空间分析方法,进一步揭示了珠江口河网水下地形演变机理。将收集的地形图进行数字化,建立不规则三角网,实现三维可视化,并在此基础上进行剖面分析,为不同年份的地形比较从而揭示珠江河网水下地形演化过程奠定基础。针对遇到的高程值转换问题,介绍了零值线法,采用点射线法作为判断依据达到高程转换的目的,同时针对该方法工作量大等不足,提出了字段标识法这一行之有效的方法。     

地质曲面“三维联动编辑”的一种实现方法

为提高地质曲面建模的精确度和合理性,完善三维地质建模软件的平、剖面三维联动编辑功能,针对"地质工程师三维助手"建模软件中构建的不规则三角网模型,提出了三角网交换边算法,并在此软件中编码实现并验证了此算法的可行性。结果显示:三角网交换边算法在编辑二维和三维三角网的同时,能够联动编辑对应的等高线平面图和剖面图,并自动更新三角网的拓扑关系。      

基于Open GL条件随机模拟三维模型可视化

利用两阶段建模思路建立条件随机模拟模型。第一阶段在地质体表面利用Denaunay三角网剖分算法实现三角网网格化，第二阶段用Denaunay四面体剖分算实现地质体的四面体网格化，并对四面体单元进行三角面插值，进而得到三角网，最后用OpenGL实现地质体三维模型的可视化。     

MAPGIS高程模型网格化参数的确定及网格化模型的选择

介绍了在MAPGIS系统里1：20万重力编图的技术方法，包括数据准备、不同投影坐标转换、数据格式转换、异常等值线勾绘、标准图框的生成、图框裁剪、误差校正合成等一整套技术方法。针对1：20万重力场特点，对三角网法和格网法实际效果进行对比、选择，详细讨论了MAPGIS高程模型网格化方法选择，网格化的范围、网格间距和网格线数所需参数的设定，搜索类型和搜索半径的确定等。说明了利用MAPGIS系统的高程模型绘制出符合出版要求的1：20万重力系列图件是可行的。     

三维地面模型的可视化研究

对于地形模型的构造有多种方法，如；规则格网法（GRID）、不规则三角网（TIN）和混合法（GRID－TIN）等。GRID模型具有较小的存储量和简单的数据结构，便于存储和管理。在对这些已有的三维地面模型进行分析的基础上，着重以DEM矩形格网法为例探讨了地面模型的构造，并在此基础上实现了三维地面模型的动态显示和交互操作等功能，最后给出了具体实例。     

面向对象的层状矿床三维地质模型构造方法

从模型的数据结构、地质模型的构建、模型实现的行为等三个方面阐述了面向对象的层状矿床的三维地质模型的构造方法。模型数据结构设计简单,可以通过三角形查询此面上的点的厚度、倾角、走向和高程等属性,通过三角网的顶点可以查询顶点座标和法向量等属性;模型的构建采用插入法使得模型在编辑修改时变得简单。以多边形界内体积计算、三角网模型切割的折线描述以及等值线绘制等为例,介绍了构造模型的应用情况。     

RTKGPS技术应用于湖泊资源保护的研究

介绍了GPS的实时差分在湖泊资源保护中的应用，研究了RTK技术进行湖泊堤岸测定，水下地形测量和湖泊水容量的计算，阐述了该技术应用于湖泊资源保护的有效性和实时性。     

地学三维模型光照与动态显示

介绍了一种具有真实感的地学三维模型光照显示的新方法,给出了三角网构建和曲面样条函数插值方法,讨论了适应三维模型光照显示的可见性测试、光照模型等算法和方法,实现了模型动态显示和剖面绘制。      

基于GADS工具箱的GPS高程拟合方法

针对GPS高程拟合问题,把遗传算法和神经网络智能技术相结合,利用神经网络作为模型,以遗传算法作为权值进化算法进行GPS高程转换,提出了该算法的基本设计思想和算法实现过程,并通过MATLAB7．x中GADS工具箱实现模型计算。结合实例进行计算,结果表明该算法用于GPS高程转换具有较高的精度,用于拟合GPS高程是可行和有效的,具有一定的应用参考价值。     

系统滤波模型在滇池水质预测中的应用

根据滇池水深较浅，流场比较稳定等特点，对湖泊进行了单元划分，考虑计算误差和观测误差干扰的存在，建立了系统滤波模型，用吉尔算法求解微分方程，对ＢＯＤ，ＣＯＤ多点连续模拟预测，经用１９８８年实测资料检验，取得满意结果。     

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