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Summarizing and analysing the stability of stratigraphy and the basic characteristics of geological hazard at the Three Gorges Reservoir,the authors put forward the dangerous slope mainly includes bedding slope,hard and soft rock alternation gentle slope,loose accumulative slop,karst breccia slop and layer cataclastic rock slop.The loose accumulative slopes from Fengjie to Badong are most dangerous and need to control.

在总结分析三峡水库区岩层稳定性及地质灾害基本特征的基础上,根据岩性和结构特征,提出三峡水库区存在较为严重失稳隐患的边坡主要有顺层边坡、平缓软硬岩层互层边坡、松散堆积体边坡、岩溶角砾岩边坡和层状碎裂岩边坡等5种类型,其中分布于奉节至巴东段的松散堆积体边坡危险性最大,是需工程防护的重中之重。

Through the investigation of massive literatural materials related to researching area,the thesis has carried out comprehensive analysis for the features of lithology and logging curves,on the basement of having clarified the regional geological background and epigeic geological characteristics.

本论文通过调研大量有关研究区的文献资料,在弄清了塔中地区的区域地质背景、构造作用史等地质特征的基础上,进行了岩性特征、测井曲线特征综合分析,将塔中地区下奥陶统地层划分为鹰山组和蓬莱坝组,并在此基础上进行了地层的进一步划分和对比,将鹰山组划分为鹰一~鹰四段。

The lithologic characters changed from fluviolacustrine sandstone to aeolian Red Clay with thin interval of greyish-white sand layers at the depth of 602 m. It can be inferred from the rock strata and age that the development age of aeolian sequence in Lanzhou area was 7 Ma at least, which is in accordance with the bottom age (7~8 Ma) of the aeolian sequence of the eastern and central Loess Plateau, suggesting that their accumulation processes are unitary.

皋兰山剖面深度602 m处出现由河湖相砂岩向以风成红粘土为主常夹有薄层砂岩的地层转变,通过岩性地层及年代的推断,兰州地区的风尘序列堆积发育的年代至少为7 Ma,与黄土高原风尘序列堆积底界8~7 Ma基本一致,说明了兰州地区与黄土高原在风尘序列堆积过程中具有统一性。

Five types of traps, including compressional, extensional, shearing, gravitative and strata litholoical types, were divided on studying the feature of different tectonic movements , seismic sequences and depositional property in Wan an Basin.

作者在分析该含油气区地质构造特征、地层划分和沉积特征的基础上,划分了压缩型、伸展型、剪切型3 种构造类圈闭和重力、地层-岩性两种非构造型的圈闭,并选用南、北两条典型地震剖面模拟了典型圈闭形成过程及其与构造运动之间的演化关系,可为在该区中寻找同类型含油气圈闭和进行构造演化史的研究提供可靠依据。

Spatial distribution characteristics of dolomite sandification in the research area is inducted. Macroscopic mechanism of dolomite sandification is deeply studied. The effect of dolomite sandification to lithologic association, geological structure condition, hydrodynamic conditions of groundwater, hydrochemistry condition and so on is systematically analysed.

对研究区白云岩砂化的空间分布特征进行了归纳,并深入探讨了白云岩砂化的宏观机理,系统的分析了岩性组合、地质构造条件、地下水动力条件、水化学条件等对白云岩砂化的影响。

In addition, it is one important basic research for exploration and development of lithologic oil and gas reservoirs in deep-water areas.

深水细粒沉积层系的层序地层单元细分和对比,是建立合理的层序地层格架的关键,也是进行深水区岩性油气藏勘探开发的一项重要基础研究工作。

Because of intense structure compression many times, continuous weathering and ground water seepage later in parent rock of coal, the mudding intercalations were usually formed a along shearing rupture of clay intercalations.

边坡所发育的煤系地层母岩体经多期强烈的构造挤压与研磨,各种风化的长期作用及地下水不断渗入,形成层间剪切破碎带产出、岩性较为复杂的泥化夹层岩组。

There are two evolutional trends for sodic basalts: alkaline basalt to sub-alkaline basalt and to the contrary. The fact that alkaline basalt has the higher concentration of incompatible elements and the sub-alkaline lower indicates the increasing degree of the partial melting in the mantle sources. The variety of Sr, Nd isotope compositions in different types of rocks shows their different mantle sources.

钠质玄武岩存在着碱性玄武岩到亚碱性玄武岩和亚碱性玄武岩到碱性玄武岩的变化序列;碱性玄武岩到亚碱性玄武岩不相容元素丰度逐渐降低,表明为部分熔融程度逐渐增高的产物;Sr、Nd同位素组成与岩性之间的相关性表明,各种岩浆是不同地幔源区部分熔融的产物。

The gas migrated from deep formation to structural high of Suining formation and formed compound gas pools of structural-lithology, and syngenetic fracture is crucial to gas production.

自深层运移上来的天然气至上侏罗统遂宁组储层中占高点运移和聚集,形成构造-岩性复合型次生气藏,原生裂缝的发育对产量的增加起着至关重要的作用。

Based on the geological background , ore?deposit and structural geology, the paper analyzed the geological character istics and metallogenic mechanism of the gold deposit and suggests that the deposit occurring in the limestone and metamorphic siliceous rocks in the third litholog ic unit of Devonian Tuokesalei formation is controlled by the Duolanasayi shear zone characteristic of secondary shear deformation, mineralizaion and multiphased vei n mineralization?.

笔者从地质背景、矿床地质,以及控矿构造分析了多拉纳萨依金矿矿床特征及其成矿机理;明确了矿床产于泥盆系托克萨雷组第三岩性段的灰岩-浅变质-硅质岩系,受控于多拉纳萨依韧性剪切带;控矿构造具有二次韧性剪切变形、矿化和多期次脉体矿化的特征,显示出构造活动的多期次性与复杂性,阐明了构造期次与矿化之间的关系。?

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