商城岩体岩石学特征及其成因探讨

本文以同源岩浆演化理论为指导思想，对组成商城岩体的楼坊湾、石鼓洼、肆顾墩三个单元，从其地质特征、岩石结构、构造、矿物成分及岩石地球化学特征等方面的演化规律，进行了较为详细的研究。认为其是由同一构造－热事件所产生的同源岩浆，经过三次涌动上侵所形成的复杂深成岩体。并且在岩石成因类型上为具有Ｉ型花岗岩地球化学特征的Ｓ型花岗岩。     

A computerized geologic mapping system based on logical models of geologic structures

In this article we describe the basic framework of the computerized geologic mapping system cigma. The system, whic is based on a mathematical formulation of geologic concepts, consists of the following six subsystems: (1) input of geologic data set; (2) inference of stratigraphic sequence; (3) construction of logical models of geologic structures; (4) determination of three-dimensional geologic boundary surfaces; (5) construction of three-dimensional solid model of geologic structures; and (6) graphical presentation. Geologic structures are summarized in several tables called logical models of geologic structures. Each model is constructed automatically from input data on structural relations between geologic bodies. The model interprets the data automatically to create data files necessary to determine the shapes of geologic boundaries; it also provides a threedimensional solid model of geologic structures referring to the shapes of boundaries. As a prototype, we introduce two types of contacts corresponding to conformity and unconformity into the logical model and show that it is possible to draw a geologic map automatically. More complex geologic structures can be introduced into the geologic mapping system through further formulation of geologic structures.     

基于MBR的多边形内点自动生成算法

在分析传统多边形内点生成方法的基础上,提出一种基于MBR（MinimumBoundingRectangle,最小外切矩形）的内点自动生成算法,该方法不仅适用于凹、凸多边形,而且可保证在多边形具有“岛屿”时,内点正确。     

利用Voronoi图形式化描述和判断GIS中的方向关系

方向关系在 GIS中占据着十分重要的地位 ,由于它的模糊性和依赖空间实体形状的特殊性 ,使得它的形式化描述和判断比较困难。文中在 CDR方法的基础上 ,利用 MBR四边的 Voronoi多边形及其边界 ,形式化描述了方向关系 ,进而将方向关系分为主方向关系和次方向关系 ,并分别给出了两者利用 MBR四边 Voronoi多边形及其边界判断的算法。     

Uncertainities in estimation of extrapolated annual occurrence rate of earthquakes using logical tree

The logical tree methods are used for evaluate quantitatively relationship between frequency and magnitude, and deduce uncertainties of annual occurrence rate of earthquakes in the periods of lower magnitude earthquake. The uncertainties include deviations from the self-similarity of frequency-magnitude relations, different fitting methods, different methods obtained the annual occurrence rate, magnitude step used in fitting, start magnitude, error of magnitude and so on. Taking Xianshuihe River source zone as an example, we analyze uncertainties of occurrence rate of earthquakes M ≥ 4, which is needed in risk evaluation extrapolating from frequency-magnitude relations of stronger earthquakes. The annual occurrence rate of M ≥ 4 is usually required for seismic hazard assessment. The sensitivity analysis and examinations indicate that, in the same frequency-magnitude relations fitting method, the most sensitive factor is annual occurrence rate, the second is magnitude step and the following is start magnitude. Effect of magnitude error is rather small. Procedure of estimating the uncertainties is as follows: (1) Establishing a logical tree described uncertainties in frequency-magnitude relations by available data and knowledge about studied region. (2) Calculating frequency-magnitude relations for each end branches. (3) Examining sensitivities of each uncertainty factors, amending structure of logical tree and adjusting original weights. (4) Recalculating frequency-magnitude relations of end branches and complementary cumulative distribution function (CCDF) in each magnitude intervals. (5) Obtaining an annual occurrence rate of M ≥ 4 earthquakes under given fractiles. Taking fractiles as 20% and 80%, annual occurrence rate of M ≥ 4 events in Xianshuihe seismic zone is 0.643 0. The annual occurrence rate is 0.631 8 under fractiles of 50%, which is very close to that under fractiles 20% and 80%.     

中国数字化地震台网(CDSN)台站地震波形数据转储技术的研究与实现

在迎来中国数字地震台网运行１０周年之际,９个台站设备的二期技术改造工作业已胜利完成。目前,这些台站配置了先进的计算机系统——ＳＵＮ公司的ＳＰＡＲＣ系列台式工作站。其上安装了相应的地震分析软件,使得应用高质量的数字化数据进行地震分析成为可能,并弥补了模拟记录的许多不足。这无疑为台站工作人员及其它科研人员在台站现场进行地震分析工作,提供了十分便利的条件。但波形数据在ＳＵＮ工作站上的驻留是一个动态的过程,一般只能保存３～４天,这给研究人员进行从容细致的应用分析造成了巨大的困难。本文着重介绍对这一问题的研究和解决方法。     

Phase relations and P–T conditions of the Ryoke pelitic and psammitic metamorphic rocks in the Ina district, Central Japan

The Ina district of the Ryoke Belt is divided into two mineral zones, based on the mineral parageneses of the pelitic and psammitic rocks at the peak metamorphism. A biotite–muscovite zone (quartz + plagioclase + biotite + muscovite with or without K-feldspar) constitutes the northwestern part, and a biotite–cordierite–K-feldspar zone (quartz + plagioclase + biotite + cordierite + K-feldspar) comprises the central to southern and eastern parts. The isograd reaction between two mineral zones is defined by a divariant reaction: Mg-rich biotite + muscovite + quartz = Fe-rich biotite + cordierite + K-feldspar + H₂O (1), which, in the K₂O–FeO–MgO–Al₂O₃–SiO₂–H₂O (KFMASH) system, occurs at ∼ 590 °C at 0.2 GPa and 660 °C at 0.4 GPa. Fibrolite accompanied by andalusite porphyroblasts in aluminous pelitic rocks of the biotite–muscovite zone and the low-grade part of the biotite–cordierite–K-feldspar zone, suggests that sillimanite was the stable aluminosilicate at the peak metamorphic condition throughout the area. In the high-grade part of the biotite–cordierite–K-feldspar zone, fibrolite mostly occurs as inclusions in cordierite or in plagioclase. The phase relations and the compositional zoning of plagioclase in relation to fibrolite inclusions suggest that fibrolite was formed under relatively high-pressure conditions, and that partial melting took place.     

运用能谱测量相关系数的统计检验法确定岩体的侵入关系

本文介绍应用铀,钍相关系数的统计检验法,来判断某两经岗岩侵入体的侵入关系。方法简便,准确度高。     

旅游者行为规律与旅游地图编制关系的探讨

旅游者行为规律是旅游地理研究的一个方面,行,吃,住,游,娱,购行为是旅游者空间行为的重要方面,它与旅游地图有着双向导的密切关系,是旅游地图的主要内涵。旅游实施行为指导旅游地图编制,旅游地图为旅游者引导旅游实施行为,为其提供服务。因此,研究旅游者行为规律对旅游地图编制和产品开发有着重要意义。     

复合地基沉降的复合本构有限元分析

提出了平面应变条件下复合地基沉降计算的复合本构有限元法。根据桩土界面处力的平衡条件和竖向变形协调条件,由桩、土材料各自的本构方程形成复合地基的本构方程,桩和桩周土可以采用任意非线性本构模型。工程实例分析表明,所建议的方法是有效的。