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Based on the measuring of out section and the analysis of inner data,the petrologic character,lithologic association,sedimentary structure,palaeourrent directions,and distribution of sandstone, the sedimentary character of the Jinci sandstone in Baode area is studied systematically.

在野外剖面实测和室内资料分析的基础上,结合对砂岩的岩石学特征、岩性组合、沉积构造和古流向特征以及砂体的空间展布规律等方面的综合研究,探讨了保德地区晋祠砂岩的沉积特征,认为晋祠砂岩为曲流河沉积。

The method of 90°-phase inversion gives stratigraphic meaning to seismic phase,and is used to interpret high frequency sequences;the technology of stratal slicing is a series of slices along the surfaces inserted proportionally between two time-surfaces and this technology is used to study the planar distribution of depositional systems.

国外上世纪80年代开始出现地震沉积学这个名词,但由于地震分辨率和研究手段的限制,没有形成一套系统的理论体系和完整的学科,国内近几年虽然广泛开展利用地震资料进行沉积相、地层岩性识别的研究,但还没有出现有关地震沉积学的系统研究。

Tectonic condition is the key factor for igneous rock reservoir, which produce crack and improve reservoir character, abundant generating rock is the foundation for igneous rock reservoir, lithology condition is the important supplement for igneous rock reservoir, it is easy for trachyte to produce crack.

综合分析构造条件是火山岩成藏的关键,其产生的裂缝改善了火山岩储层的储集性能;充足的油源条件是火山岩成藏的基础;岩性条件是火山岩成藏的重要补充,即粗面岩容易在构造作用下形成构造裂缝,最终形成火山岩油气藏。

It is an uncontinuous plane between the grey gneisses and Jingangku formation complex undergone later many strong deformations, especially the near-horizontal ductile shearing.

在恒山和五台山区大体上金岗库岩组的不同岩性或层位与灰色片麻岩相接触,受到后期多次强烈的构造改造,特别是近水平的韧性剪切使二者之间呈一不连续面,年轻的表壳岩覆盖在老片麻岩系之上,属剥离断层性质,应为低角度的大型正断层。

The writer simplifies and induces thin-bedding medium in the East of China to several seismogeologic models: wedge model; thin-bedding group in which two mediums have equal thickness, thin-bedding group in which two mediums have not equal thickness and formations whose thickness orderly gradates from top to bottom.

本文通过对某油田的若干口钻井的测井曲线和岩性资料进行分析研究,认为我国东部油区的薄互层地层的地质特征为:①大多数地层为低于目前地震勘探分辨率的薄层或超薄层;②地层在横向上相变剧烈;③地层结构具有多种类型。

The mechanism of energy accumulation and dissipation of rock masses during loading is analyzed to establish the qualitative and quantitative relations between the composition and texture and the burst potential of rock masses of coal-bearing formation.

煤岩体的冲击倾向性是发生冲击地压的固有属性和必要条件,且影响煤岩体冲击倾向性的因素很多;而煤岩体的物质成分、岩性组构是煤岩体的内在属性,是决定煤岩冲击倾向性的内在因素。

The rock composition, material disperse, structure characteristic, boundary condi tion, movement mode and forming mechanism of plane rotation slope are completely differ nt from the slope deformation and destroy people usually thought, which moves frorn top to bottom, callapsing or ratating vertical around horizontal axis under the outside load tak ing gravitational force as primaty factor.

平面旋转坡体的岩性组成、物质分布、结构特征、边界条件、运动方式及形成机理等与过去人们习惯上认识的那种在以重力为主的外荷作用下,自上而下同步位移、崩落或绕水平轴的立面旋转坡体的破坏类型完全不同。

On the basis of deep research on fault sealing property and its main influence factors, the functional relation of mud content in fault infills with fault displacement and faulted mudstone thickness is described quantitatively through the analysis of lithology influence factors in fracture belt.

在深入研究断层封闭性及其主要影响因素的基础上,根据对断裂带中岩性影响因素的分析,定量描述了断裂带填充物中泥质所占百分含量的大小与其断层位移和被错断泥岩厚度之间的函数关系,并提出了根据断裂带填充物中泥质含量的大小来判断断层封闭性的标准。

By studying the inorganic CO〓 and helium isotopes in Yinggehai Basin, and investigating the Tertiary lithology and geothermal condition, combined with the results of thermal simulation test, it was suggested that inorganic CO〓 gas principally came from thermal decomposition of Tertiary calcareous shales and Pre-Tertiary carbonate under the burial depth of 6000m, approximately at a strata temperature of about 250℃.

通过系统地剖析莺歌海底辟带气田无机CO〓的碳、稀有气体同位素特征与第三系及古生界基底的岩性及热源条件,结合热模拟实验资料,认为无机CO〓主要来深埋的梅山-三亚组钙质泥岩热分解和前第三系基底碳酸岩的热变质,这种钙质泥岩和碳酸岩热分解产生CO〓的初始温度大约为250℃,相当于埋深约6000m。

Because the velocity of the ore bed in the fault trough is different with the velocity of the both sides layers, so for the sake of designing demand we should full use the action of calibrating lithologic character of the refraction wave.

由于在地堑内的矿层和两侧的地层速度不同,为了满足设计要求,在施工过程中,充分利用折射波视速度的岩性标定作用,也就是说根据折射波不同的视速度反映,可以准确判断地震测线是否已控制到地堑的边界断层,并及时调整反射波测线布置,大大缩短了现场处理时间,提高了勘探效率。

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