发展“三高”果业需重视大生态系统的耗散协调性──剖析龙泉花果山的大生态环境

发展高产优质高效果业，常会涉及到大生态系统的各类环境因子群。龙泉花果山的大生态系统主要是以风化岩体→紫色土容库→蜜桃等构成的向量大系统的综合反映，并呈现非均衡耗散结构的复杂协调性，这些因素直接制约“三高”果业的发展。     

矽卡岩浆型铜矿床特征——以安徽铜陵东狮子山铜矿床为例

东狮子山铜矿床具有下列独特的特征:(1)矽卡岩是高温、高密度、粘稠的岩浆熔融体;(2)矽卡岩体与辉石二长岩体具有同源性;(3)矿体与矽岩体具有同源性;(4)成矿物质来自岩浆源,硫同位素测定的绝对值小于5‰;(5)矽卡岩矿物开始结晶温度为920C,可见熔融包裹体,成矿温度为620C;(6)成矿压力相当于1～2km深度条件;(7)矿石、矽卡岩具有典型的岩浆矿床的结构构造。     

西海固地区近期垂直形变场分析

本文采用分段线性速率整体动态平差法处理了西海固地区七十年代以来的多期水准资料,并用形变场图象及数字特征量等分析了该区垂直形变场变化特征及其与地震活动的关系。认为该区自1981年以后区域应力逐渐增强,再经1990年前后应力场调整,目前已恢复到正常的继承性运动状态。     

农业气候相似原理与农作物引种的气候诊断方法

介绍了农业气候相似原理以及相似程度判别方法,为农作物合理引种提供气候依据。     

关于辽宁地区b值方法定量预测的研究

本文利用地震学分析预报方法程式指南和“八五”攻关成果中提出的地震b值定量预测方法,对辽宁及邻区1969年以来发生的8次地震震例作了回顾性检验研究。在此基础上,根据震前b值的变化特征,总结出了可能适用于辽宁地区半年左右尺度的b值预测方法的异常羊别指标及预报规则。     

鄂西清江下游主要活动断层分段、分形与地震活动

在地质调查的基础上,初步厘定了清江下游主要活动断层的现今几何轨迹结构,并从几何形态、结构特性和现今活动性三方面对其进行自然段划分;进而利用分形分维分析,估算活动断层不同区段轨迹结构的分维值。计算结果表明：每一个断层段具有一个特征性的分维值,轨迹结构越复杂,分维值越高,现今活动性越强;其中,仙女山断层带中段分维值最高, Ｄ＝ １２５７,而松园坪断层北段最低, Ｄ＝ １０１８。结合地震活动分析发现：仙女山断层带是清江下游现今活动最强的活动断裂;仙女山断层带的中小地震活动,具有间歇式 分段振荡迁移的特性;时间上地震活动期为１～５ａ,相对平静期为１０ａ 左右;空间上地震活动从南段开始,振荡迁移到北段,然后又向中段迁移,目前地震活动似乎正在向中南段边界迁移;并且,中南段断裂轨迹结构比北段复杂,分维值也高,地震活动强度相对较大,因此,未来仙女山断层带可能发生的中强地震（ Ｍｓ＝ ５０ 级左右）将主要集中于中南段,而不是北段。     

嵩县雷门沟金矿地质特征及次生富集作用

本文从三条典型含金蚀变破碎带入手 ,通过对其次生富集带的分析、对比、归纳 ,揭示出次生富集带的深度、厚度和品位变化规律 ,并进一步从理论上阐明次生富集带的形成机理。     

MAROS: a decision support system for optimizing monitoring plans

The Monitoring and Remediation Optimization System (MAROS), a decision-support software, was developed to assist in formulating cost-effective ground water long-term monitoring plans. MAROS optimizes an existing ground water monitoring program using both temporal and spatial data analyses to determine the general monitoring system category and the locations and frequency of sampling for future compliance monitoring at the site. The objective of the MAROS optimization is to minimize monitoring locations in the sampling network and reduce sampling frequency without significant loss of information, ensuring adequate future characterization of the contaminant plume. The interpretive trend analysis approach recommends the general monitoring system category for a site based on plume stability and site-specific hydrogeologic information. Plume stability is characterized using primary lines of evidence (i.e., Mann-Kendall analysis and linear regression analysis) based on concentration trends, and secondary lines of evidence based on modeling results and empirical data. The sampling optimization approach, consisting of a two-dimensional spatial sampling reduction method (Delaunay method) and a temporal sampling analysis method (Modified CES method), provides detailed sampling location and frequency results. The Delaunay method is designed to identify and eliminate redundant sampling locations without causing significant information loss in characterizing the plume. The Modified CES method determines the optimal sampling frequency for a sampling location based on the direction, magnitude, and uncertainty in its concentration trend. MAROS addresses a variety of ground water contaminants (fuels, solvents, and metals), allows import of various data formats, and is designed for continual modification of long-term monitoring plans as the plume or site conditions change over time.     

The <Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar geochronology constraint and geological significance of mylonites in Shangyi-Chicheng fault belt on the north of North China Craton

A dating of two biotite samples taken from the meso- and low-temperature mylonites within the Shangyi-Chicheng fault belt on the north of the North China Craton yields ⁴⁰Ar/³⁹Ar isotopic ages of (399 ± 1) Ma and (263 ± 2) Ma, respectively. These data reflect an Early Devonian deformation and a Late Carboniferous retrograde metamorphism event along the fault, suggesting that the tectonic activities of the North China Craton in Paleozoic should be reconsidered.