大别山前寒武纪变质地体基本组成

本文以新城－圻春断裂为界将大别山前寒武纪变质地体划分为华北陆块南缘和场子陆块北缘两个次级变质地体，两个次级地体不仅在地球物理，构造变形方面明显不同，而且在物质成分上有显著差异，它们有各自独立的变质地层系统，遭受了不同类型的变质作用，有完全不同的岩浆活动图象，上述差异均可指示华北，扬子两古陆碰掸对接时扬子陆块北缘向北俯冲至华北陆块南缘之下，这可能包括两次合作用，从元古代开始至中生代最终结束的长期复杂     

The Zoulang Nanshan Caledonian Subduct ion Complex in the Northern Qilian Mountains and Its Dynamics

The front of the Zoulang Nanshan Caledonian volcanic island arc zone in the northern Qilian Mountains is a forearc accretionary terrane, composed of multiple accretionary volcanic island arcs, flysch accretionary wedges,high-pressure metamorphosed detachment zones and remnants of ophiolites. It resulted from the northeastward subduction of the Early Palaeozoic Qilan oceanic crust beneath the Alxa block. High-pressure metamorphism, which occurred during the subduction, progressed through three stages: the initial stage of medium T-high P,the main stage of temperature decrease and pressure increase, and the lag stage of pressure decrease and temperature increase. Finally the paper presents a retrotrench subduction dynamic model indicative of northward subduction of the central Qilian block and southward accretion of the Alxa block during the period of 450-500 Ma.     

Geological - Geophysical - Geochemical Exploration Models of Copper - Iron Deposits in Southeastern Hubei

This paper discusses geological-geophysical-geochemical models of such typical deposits as the Tieshan-type Fe-Cu deposit, the Tonglushan-type Cu-Fe deposit, the Yehuaxiang-type Cu deposit, the Jiguanzui-type Cu-Au deposit, and the Tongshankou-type Cu (Mo) deposit. The models were established based on practical data of the polymetallic deposits dominated by copper ore in southeastern Hubei. These models, which are graphically illustrated in the paper, systematically summarize the metallogenic geological conditions and the geophysical-geochemical characteristics of copper deposits in this area. The models are of practical significance for studying copper deposits, predicting mineral resources, choosing exploration methods, and searching for ore deposits based on existing ones in the study area.     

宝顶石刻区污染地下水对造像岩体的破坏作用

污染地下水渗入大佛湾摩岩造像群，在石刻表面积聚可溶盐，加剧了石刻的侵蚀破坏，其中尤以泥质细粒长石砂岩风化剥落最为严重。研究渗水病害对石刻保护有重要意义。     

白牛厂银多金属矿床银的赋存形式及银矿物特征

矿床产在燕山期花岗岩外接触带，受北西向层间滑动构造破碎带控制。含矿热液沿构造破碎带充填，形成规模很大的、连续性极好的、银锡铅锌均分别达到大型的复合矿体。成矿具多成因、多期、多阶段的特点。银主要呈银矿物形式存在，银矿物又主要是多阶段的银锑－银铜锑－银铅锑等硫盐矿物。银矿物粒度很细，多呈包嵌形式存在，与方铅矿关系特别密切。经矿相配合能谱系统研究，辅以部分单矿物分析，初步查明其分布、富集、相互关系及矿物物性特征。     

利用SPACE LAB彩色红外影像及数据复合技术对藏北牧草资源进行计算机分类的研究

本文就在藏北草资源调查中,应用空间实验室量测摄影机(MC)摄得的彩色红外影像,及根据遥感影像目视判读所利用的信息空间特点和草场分类原理进行计算机自动分类的理论与方法,对利用辅助数据和影像数据复合技术的几种尝试进行了讨论,并依实地调查资料和专家判读结果对各种分类结果进行了评价。说明利用这种航天遥感资料,辅以Landsat影像生物量指标、DTM和坡度、坡向数据以及计算机自动分类技术,进行资源调查是可行的,可以达到最佳效果。     

On the enhanced confining pressure aproach to the mechanics of reinforced soil

Summary A review is presented of conceptual approaches that are currently in use for interpreting the operation of reinforced soil. The concepts of enhanced confining pressure and of reduced normal tensile strains are found to be closely related to current experimental and theoretical investigations as well as to the design methodologies available at present for reinforced soil applications. Focusing on the enhanced confining pressure concept, analytical expressions are developed that allow the estimation of the value of equivalent confining stress increase when the properties of soil and reinforcement and the state of stresses acting on a cylindrical reinforced soil element are known. The derived expressions can also be utilized for estimating the soil-reinforcement friction angle from the results of triaxial tests on cylindrical samples reinforced with horizontal layers of reinforcement.     

用石灰桩加固软弱地基

石灰桩作为一种技术可靠、经济快速的软弱地基加固方法已得到了广泛应用。本文介绍了武汉岩土力学研究所近一年来利用石灰桩处理软弱地基的成功经验。现场检测表明，对于单层和多层工业与民用建筑而言，采用石灰桩可以使软弱地基获得良好加固且满足设计要求。文中还对石灰桩的加固机理进行了简要分析。     

北京密云麻粒岩相区变质作用演化及PTt轨迹的研究

北京密云麻粒岩相区在早前寒武纪时期主要经历了两期变质作用。每期变质作用又可划分为三个连续的变质阶段，峰期阶段的Ｐ－Ｔ条件均达到了麻粒岩相．第一期变质作用约结束于２５００Ｍａ，具有与造山带相似的顺时针ＰＴｔ轨迹，峰期阶段Ｔ为８００～９００℃，Ｐ＝０．９８～１．０２ＧＰａ，这种轨迹主要与早期平卧褶皱和推覆构造使地壳大幅度增厚有密切关系。第二期变质作用约发生在１８００Ｍａ，ＰＴｔ轨迹为具近等压加热（ＩＢＨ）特点的顺时针轨迹，峰期阶段Ｔ为７６０～８１０℃，Ｐ为０．９６～１．０４ＧＰａ，这种轨迹与大陆地壳的拉伸作用有密切关系。