沉积学
- 与 沉积学 相关的网络例句 [注:此内容来源于网络,仅供参考]
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Also apply methods of integration of sequence stratigraphy, biostratigraphy, petrostratigraphy and seismic data to found the time-contour stratigraphic framework and reveal time-space distribution of depositional system and meantime clarify oil-source bed, reservoir and overlying distribution regular patterns.
此外,运用层序地层学、生物地层学、岩石地层学与测井、地震资料相结合的方法,建立该区等时地层格架、沉积体系的时空展布,阐明了生、储、盖展布规律。
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Based on the petrological and sedimentological research the paper discusses on tectonic background of the Changcheng System clastic rocks, especially on the syndepositional diastrophism.
本文综合岩石学和沉积环境的研究结果,进一步探讨了长城系碎屑岩的沉积背景,重点讨论了同沉积期的构造活动特点。
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It was the first time the sequence stratigraphy study had been done all across Naimanqi Depression. Jiufotang Formation of Naimanqi Depression was divided into two third-class sequences (SQ1 and SQ2) and five system tracts (SQ1 has LST, TST and HST; SQ2 has TST and HST), and in High System Tract of SQ2, two fourth-class sequences were defined (Ssq1 and Ssq2).2. According to the analysis of core and logging data, we considered that it is the delta fan facies and established the electrofacies model.3. The distribution of reservoir sand bodies had been predicted in the areas without well data by combining the methods of sequence stratigraphy and reservoir inversion. In addition, we summarized the method and process of combining geology and geophysics to predict reservoirs and we made a good prediction by applying it.4. Combining with sequence and depositional types, sandstone thicknesses and reservoir properties, based on Petrel Software platform, we used fuzzy mathematics to comprehensively evaluate reservoirs and define favorable areas. We classified the reservoirs in Naimanqi Depression into five types (TypeⅠ, TypeⅡ, TypeⅢ, TypeⅣand TypeⅤ) and pointed out four favorable areas: Block Nai 1, Block of western Naican 1-Zhangjia Depression, Block Nai 6 and Block of Xinfa-Zhangjia Depression.
其主要创新点如下:1、首次在整个奈曼旗凹陷范围内进行了层序地层学的研究,将奈曼旗凹陷九佛堂组地层分为2个三级层序(SQ1和SQ2)和5个体系域(SQ1由LST、TST和HST组成,SQ2由TST和HST组成),并在SQ2的高位体系域中又识别出两个四级层序(Ssq1和Ssq2)。2、根据岩芯分析和测井资料识别,定义了研究区扇三角洲沉积相类型,并建立了测井相模板。3、通过层序地层学的研究,结合储层反演,对奈曼旗凹陷层序格架内没有井的区域进行了储层砂体的空间展布预测,并总结了地质-地球物理综合储层预测的方法与思路流程,在应用中取得了良好的预测效果。4、结合层序、沉积类型、砂岩厚度和储层物性等方面,以Petrel软件为基础平台,利用模糊数学的方法进行储层综合评价及有利区划分,将奈曼旗凹陷储层划分为五个级别(Ⅰ类、Ⅱ类、Ⅲ类、Ⅳ类和Ⅴ类),并预测了四个有利区块,分别为:奈1区块、奈参1西-张家洼子区块、奈6区块和新发-张家洼子区块
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Firstly, based on the observation and description of a large number of drilling cores in macroscopic and microcosmic aspects, facies marks are summarised, which supplied from the characteristics of lithology, distribution of grain size, sedimentary structvure, ichnology and logging facies.
首先,在对大量岩心宏观和微观特征描述的基础上,从岩石学特征、粒度分布特征、沉积构造特征、遗迹化石特征以及测井相特征等五方面,总结出研究区的各类沉积相的相标志,为沉积相的识别和划分提供了有力的依据。
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The extraction methods of Quaternary pollen and spores are the bases and precondition in Quaternary Palynology. Northern China is in particular physical geography environment. In Quaternary there are many different types of sediments in northern China. And at all times extraction methods of Quaternary pollen and spores from different type of sediments are the difficulties and highlights in North China.
孢粉提取方法是第四纪孢粉学研究的基础和前提,中国北方地区具有独特的自然地理条件,第四纪以来形成了特有的沉积物类型,不同沉积物的孢粉提取研究一直以来是中国孢粉学研究的难点和热点。
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Looking through history changes in the whole 20th century,Chinese penology has experience the evolution process other start,the initial establishment and the turning and development stages,from which we get some experiences and enlightenments be—ing very important form Chinese Penology to further develop in the 21the century.
通览20世纪中国历史的演变,中国监狱学经历了肇始、初创、转型发展的进化过程,从中沉积的经验教训给了我们重要的启示,这对21世纪中国监狱学的发展走向是非常重要的。21世纪的中国监狱学,应从继承、移植、创新的战略思路出发,采取综合性研究方法,来求得发展,并随着祖国统一大业的完成,必将成为完全统一的中国监狱学。
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This illustrated online guide from the University of Georgia Stratigraphy Laboratory is primarily aimed at the application of sequence stratigraphy to outcrops. It covers: accommodation space; parasequences; progradational, aggradational, and retrogradational stacking; depositional sequences; surfaces; type 1 and type 2 sequences; application to outcrops; chronostratigraphy; and carbonate sequence stratigraphy.
这个有插图的在线指南是由美国乔治亚州大学地层学实验室创建的,主要是为了将地层次序应用于裸露出地面的岩层,内容包括:调节空间,副次序,延伸、沉积、退化叠加,沉积次序,表面,类型1与类型2的次序,裸露出地面的岩层的应用,年代地层学,碳酸盐地层次序。
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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。
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On the basis of the researching of facies、 petrology、 cathodoluminescence analysis, this paper concludes that the terrigenous clastics in Pingyipu Formation were mostly originated from Motianling palaeo-peninsula lied to its north, and sands in distributary channels、 braidedriver in estuaries、 deltas and in littoral zone in hybrids could be derived from Middle-Sichuan Palaeoland with Peng-Guan Highland.
对早中泥盆世浑水陆源碎屑沉积及混合沉积的沉积相、岩石学、阴极发光等研究分析,作者推测,该区陆源碎屑主要来自北边的摩天岭古半岛,而分流河道、辫状河充填及混积滨岸砂则可能以川中古陆和彭灌高地为主要源区。这一点与过去通常认为的主要来自彭灌岛和轿子顶古岛差别较大。
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In accordance with features of petrology, sedimentary structure, profile structure, electrofacies and seismic facies, underwater distributary channel, frontal sill-like sand, mouth bar, distal bar, front fan-delta mud and mere mud and so on, were identified, and depositional features of them in detail were discussed respectively.
根据羊邑组二段-三段的岩行学、沉积构造、剖面结构、测井相和地震相等特征,进一步识别出水下分流河道、前缘席状砂、河口坝、远砂坝、前扇三角洲泥和浅湖泥等沉积微相,并详述了各微相的沉积特征。
- 推荐网络例句
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And Pharaoh spoke to Joseph, saying, Your father and your brothers have come to you.
47:5 法老对约瑟说,你父亲和你弟兄们到你这里来了。
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Additionally, the approximate flattening of surface strip using lines linking midpoints on perpendicular lines between geodesic curves and the unconditional extreme value method are discussed.
提出了用测地线方程、曲面上两点间短程线来计算膜结构曲面测地线的方法,同时,采用测地线间垂线的中点连线和用无约束极值法进行空间条状曲面近似展开的分析。
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Hey Big Raven, The individual lies dont matter anymore - its ALL a tissue of lies in support of...
嘿大乌鸦,个别谎言的事不要再-其所有的组织的谎言,在支持。