胶东昆嵛山二长花岗岩副矿物成因矿物学研究

根据胶东昆嵛山二长花岗岩主要的副矿物组合（磁铁矿、榍石、绿帘石、褐帘石、磷灰石、锆石及自然金等）及相应的含量，结合有关矿物的形态、成分，特别是３２６粒锆石群形态学的研究，对岩石成因与金矿化的关系等，提出了矿物学标志。确定昆嵛山岩体为岩浆成因，岩浆物质来源为胶东群部分重熔，物质组成以壳源为主，为Ⅰ型磁铁矿系列花岗岩类；确定岩体结晶温度跨度大，因而富含水分，岩体富含Ｓ及其他挥发分，富含碱质，早期矿物结晶处于较氧化碱性环境，以上条件对形成金矿有利。对胶东三大主要含金岩体，即昆嵛山、郭家岭及玲珑岩体副矿物特点进行了对比。     

基于流形拓扑的三维空间实体形式化描述

阐述了三维空间实体语义概念及空间实体之间拓扑性质形式化描述的意义，以组合及点集拓扑理论为基础，给出了基于ｋ－维伪流形的三维空间实体的语义定义。将单纯同调理论用于流形，通过单纯形和单纯复形间的几何构造关系，揭示出三维空间实体的拓扑性质并给出三维空间实体的形式化描述方法。     

最强伴随拓扑与最弱伴随拓扑

本文给出了最强伴随拓扑的一个具体表达形式，得出若于最弱伴随拓扑存在的条件，讨论半开集族的包含关系与其最弱伴随拓扑的包含关系之间的联系。     

完备格间的保交并映射

本文探讨了格的代数同态的性质和应用,证明了从完备格L_1到L_2的保交、保并的满射φ将L_1的邻元系、滤敛关系、网敛关系分别映成L_2的邻元系、滤剑关系、网敛关系。     

Evolving fluid composition during prograde metamorphism in subduction zones: A new approach using carbonate-bearing assemblages in the pelitic system

The changing XCO₂ in fluids during the progressive metamorphism in Sanbagawa belt of the Cretaceous subduction zone, Japan, was estimated by a newly proposed method. The subduction zone meta-sediments are characterized commonly by four-phase assemblages in the CaO–NaAlO₂–KAlO₂–Al₂O₃ system with excess quartz and a CO₂–H₂O binary fluid phase. Using the common assemblage of calcite–albite–muscovite–clinozoisite, XCO₂ of the fluid was estimated to be from about 0.0001–0.0005 (the lowest grade chlorite zone), through 0.004–0.01 (garnet zone), 0.01–0.05 (albite–biotite zone) to 0.06–0.2 (oligoclase–biotite zone).The paragenetic relationship of meta-sediments from the subduction zones was compared in a wide P–T range to cover the stability fields of aragonite and jadeite. As a result, an excellent P–T–XCO₂ relationship was delineated to serve as a quantitative monitor for the evolving fluid composition during the progressive metamorphism in subduction zones.     

一种基于网络拓扑关系的地图匹配算法

地图匹配是车辆导航定位系统中提高定位精度的一种方法,其精度受定位数据、地图数据质量及坐标系转换关系的影响。在分析现有算法的基础上,提出了一种基于网络拓扑关系的地图匹配算法。该算法只需将GPS定位数据和G IS数据相结合,即可用算法的形式解决地图匹配中一些常见的问题。实验证明:该算法是一种精度高、效率好、实用性强的地图匹配算法,具有较好的实用价值。     

地图空间关系认知元素分析

分析了目前地图空间认知的几种理论研究。从地图学史的角度出发,应用几幅著名的中外古地图,指出符号、注记以及空间拓扑关系在地图发展变化中的不变性,认为这3种元素构成了地图空间关系认知的基本元素,并分析了这3种元素在地图空间关系构建方面所起的作用。最后提出了在网络环境下,这3种元素在大众制图中的指导意义。     

Comparison of relative permeability–fluid saturation–capillary pressure relations in the modelling of non-aqueous phase liquid infiltration in variably saturated,layered media

The characteristic functions relating relative permeabilities and capillary pressures to fluid saturations (k_r–S–P_c models) are of great importance for the modelling of sub-surface multi-phase flow and transport. In order to test their performance and to identify their important parameters, four well-known three-phase k_r–S–P_c models have been tested against published experimental data on non-aqueous phase liquid (NAPL) migration in the unsaturated zone. Both homogenous systems and systems with embedded heterogeneities have been analysed.     

空间方向关系形式化描述模型研究

空间方向关系形式化描述模型是空间关系研究的难点和重点，目前尚无完善的模型出现，因此进行其模型的研究意义重大。首先论述运用平面目标Voronoi图描述方向关系在理论上的可行性；然后详细阐述基于Voronoi图的空间方向关系形式化描述模型建立；为了验证模型的正确性，给出几个典型的算例；最后指出模型的优、缺点。     

Calculated Phase Relations in High-Pressure Metapelites in the System NKFMASH (Na2O-K2O-FeO-MgO-Al2O3-SiO2-H2O)

Using an internally consistent thermodynamic dataset and updatedmodels of activity–composition relation for solid solutions,petrogenetic grids in the system NKFMASH (Na₂O–K₂O–FeO–MgO–Al₂O₃–SiO₂–H₂O)and the subsystems NKMASH and NKFASH have been calculated withthe software THERMOCALC 3.1 in the P–T range 5–36kbar and 400–810°C, involving garnet, chloritoid,biotite, carpholite, talc, chlorite, kyanite/sillimanite, staurolite,phengite, paragonite, albite, glaucophane, jadeite, with quartz/coesiteand H₂O in excess. These grids, together with calculated AFMcompatibility diagrams and P–T pseudosections, are shownto be powerful tools for delineating the phase equilibria andP–T conditions of Na-bearing pelitic assemblages for avariety of bulk compositions from high-P terranes around theworld. These calculated equilibria are in good agreement withpetrological studies. Moreover, contours of the calculated phengiteSi isopleths in P–T pseudosections for different bulkcompositions confirm that phengite barometry is highly dependenton mineral assemblage. KEY WORDS: phase relations; HP metapelite; NKFMASH; THERMOCALC; phengite geobarometry