玻镁安山岩中辉石枝晶的形貌与晶体生长方式

川西乡城地区的玻镁安山岩基质中辉石微晶具有奇特的枝晶形貌。通过高倍率光学显微镜和扫描电镜观察,较详细地分析了辉石枝晶的形貌细节。辉石枝晶一般发育三级分枝,各分枝间以近于90°和110°交角沿单斜辉石结晶学主轴方位优先生长,各级分校具有整体一致的光学性质,如同单个晶体。玻镁安山岩浆流动性大,呈薄层状。快速冷凝作用和强的结晶能力是辉石枝晶发育的前提条件。初步探讨了在远离平衡态结晶时,辉石枝晶生长方式和界面稳定性对晶体形貌的控制作用。     

ALTERATIONS OF RIVER MORPHOLOGY DUE TO VEGETATION ON SLOPES AND FLOOD PLAINS

LRESEarCHACTIVITIESCharaCtCriedcofunlinedalluvialriVersisthe~linteractionbettVeenwaterflowandmovableriVerbed.Sedimenttransport,bedresistanceandriVermorphologydecisivelydependontheflowconditionsandviceversathesefactorsgovernthehydraulicprocesses.EVenundersimplifiedconditions,e.g.inlaboratorytests,theseillteractionsareeXtremelycomplexandrelldsraliZationmakesengineeringproblemsevenmored~.TomaketheseprocessesmoreunderstandablecomprehensiVeresearchprojectswereconductedatseveralGermanuniv…     

多尺度CB形态学及其在线划图像噪声清除中的应用

介绍了基于轮廓结构元的形态学（简称CB形态学）的概念及其性质,讨论了CB形态运算的快速实现。由于CB形态学处理的对象不是基于目标的形状,而是基于目标的延伸度,因此它可以用来处理线划图像。在本文中,利用CB形态学的这一特性消除线划图像上的噪声,获得了满意的结果。     

数学形态学用于纹理图像的分维估计

首先介绍了灰度图像膨胀与腐蚀的定义，然后给出了数学形态学估计分维的数学模型，进而用于纹理图像的分维估计。实验结果表明：该方法原理简单，算法设计灵活，运算速度快捷，为纹理特征描述提供了一种有效的新途径。     

数学形态学及其在二值影象分析中的应用

本文介绍了数学形态学的基本概念,利用一些简单例子叙述其定义、逻辑变换和形态变换的基本算子及其作用。文中对数学形态学在二值影象如汉字和栅格扫描的地图的数据分析中的应用可能性也进行了探讨。这些讨论对于建立地理信息系统的测量数据库是有益的。     

A Lower Palaeozoic shallow water sequence in the eastern European Variscides (SW Poland): provenance and depositional history

The Gackowa Formation of inferred Cambrian —Ordovician age is part of the metamorphosed pre-Variscan basement of the southern Kaczawa Mountains of the Sudetes region, south-west Poland. Previously variously interpreted as lavas, tuffs and sandstones, it is shown to consist of about 200 m of originally well-sorted siliclastic sedimentary rocks within a sequence of predominantly mafic volcanic rocks. Four facies have been distinguished based on relict sedimentary structures and textures and these suggest that deposition took place on a storm-dominated shelf, mostly above the wave base. The petrography, detrital zircon morphologies and geochemistry suggest affinity with, and derivation in large part from, acid volcanic rocks at a comparable stratigraphic position in a separate tectonostratigraphic unit to the south. The Gackowa Formation and its acid volcanic source rocks have a clear continental geochemical signature, in contrast with the mantle-derived basic/bimodal volcanic rocks below and above; it is suggested that the parent acid magma originated by crustal melting during the ascent of these mantle-derived magmas. A continental crust setting is inferred for the deposition of the Gackowa Formation sandstones, thus suggesting a continental setting for the associated within-plate basalts. The entire volcanic/sedimentary succession resembles elements of the Lower Palaeozoic of Germany, and all may have formed in an initial rift setting during Late Precambrian to Ordovician times.     

巴东县新城区冲沟泥石流危险度评价

根据对巴东城区泥石流特征的调查和分析,本文选取了8个因子评价冲沟泥石危险度,采用模糊数学方法建立危险度评价模型,并对城区三条大型冲沟(白岩沟、铜盆溪、黄家大沟)的泥石流危险度作出评价并得到结果,这对预防和治理巴东新城区的泥石流具有重要意义。     

Characterization and reconstruction of a rock fracture surface by geostatistics

It is well understood that, in studying the mechanical and hydromechanical behaviour of rock joints, their morphology must be taken into account. A geostatistical approach has been developed for characterizing the morphology of fracture surfaces at a decimetre scale. This allows the analysis of the spatial variability of elevations, and their first and second derivatives, with the intention of producing a model that gives a numerical three‐dimensional (3D) representation of the lower and upper surfaces of the fracture. Two samples (I and II) located close together were cored across a natural fracture. The experimental data are the elevations recorded along profiles (using recording steps of 0.5 and 0.02 mm, respectively, for the samples I and II). The goal of this study is to model the surface topography of sample I, so getting estimates for elevations at each node of a square grid whose mesh size will be, for mechanical purposes, no larger than the recording step. Since the fracture surface within the sample core is not strictly horizontal, geostatistical methods are applied to residuals of elevations of sample I. Further, since structural information is necessary at very low scale, theoretical models of variograms of elevations, first and second derivatives are fitted using data of both that sample I and sample II. The geostatistical reconstructions are computed using kriging and conditional simulation methods. In order to validate these reconstructions, variograms and distributions of experimental data are compared with variograms and distributions of the fitted data. Copyright © 2002 John Wiley & Sons, Ltd.