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The factors affecting postfrac productivity are discussed in the paper. The grey associability ordering indicated that the postfrac productivity was lowly correlated with the permeability interpreted by the original log data and mainly influenced by porosity, then effective thickness, and then shale content and formation pressure. In light of the genetic neural network method, the productivity of gas well was predicted by use of the log data through programing and model training. The error detecting result proved that the model was reliable and a good application effectiveness was obtained.

文章对压后影响产能的因素进行了讨论,灰关联度排序表明,压后产能与原始测井解释的渗透率关联性小,而主要影响因素依次是孔隙度、有效厚度、泥质含量和地层压力;引用遗传神经网络法,编制预测程序,利用测井资料通过模型训练,对气井的产能进行预测,误差检验验证了模型的可靠性,取得了良好的应用效果。

Soil type is coming from the land all materials, such as clay, stone, wood and so on, people feel the earth is a material nature, inclusive and harmonious nature of the familiarity with a strong.

土属类包括所有从土地而来的物料如泥质、石质、木质等,土属材料让人感受到自然界的包容、和谐的特质,具有强烈的亲切感。

Calculation on phase equilibria in the KFMASH and NCKFMASH systems indicates that the phase relations of ferromagnesian minerals are controlled by the KFMASH.

在模拟泥质岩石的KFMASH体系和NCKFMASH体系中的相平衡计算表明,NCKFMASH体系中铁镁矿物的相平衡关系受KFMASH亚体系中矿物相平衡关系的控制,但KFMASH亚体系中固相线位置要比实际的高50-60℃。

According to the space distribution characters of tectonic-sequence-based lithofacies and paleogeography, it is showed that three types of hydrocarbon source-rock including carbonate rock, clay and coal in Permian mainly are developed in transgression and maximal sea flooding of two order sequences, and they deposite respectively on platforms with gentle slope in craton, in rift basins and around old lands.

构造-层序岩相古地理的空间展布特征表明,二级层序的海侵期和最大海泛期是二叠纪烃源岩发育的主要时期,分别在克拉通的缓坡台地上、裂陷槽盆和古陆周缘形成了碳酸盐岩、泥质岩和煤系三类烃源岩。

On the basis of comparison of engineering properties of domestic and foreign Neogene muddy deposits, in the view of whole globe and associated with the geological characteristics of China, the paper demonstrates that the intermediate type of the material between the soil and the rock, named "hard clay/soft rock", which can not be separated abruptly, really exists in China.

本文在国内外上第三系泥质沉积物工程特性对比的基础上,从全球观念出发,结合中国的地质特点,提出在中国确实存在着难以一刀切的过渡类型——"硬土/软岩",并根据其地质成因和分布规律进行了初步分类,这对于促进工程地质学、土力学和岩石力学的融合具有重要意义。

A simulation experiment on the quantitative relation between mudstone content in fault zone and vertical seal of overthrust was carried out. In addition, this paper analyzed the influence of deformation characteristics of rocks on vertical seal of fault.

在正确分析逆掩断层形成的地质条件和封闭机理的基础上,本文认为与逆掩断层相伴生的塑性岩石的变形特征、断面压力和断裂带中泥质含量是影响断层垂向封闭性的主要因素。

Petrographic and REE and trace element geochemical studies of these rocks and Nd isotope analysis of amphibolite indicate that the protoliths of the Mengjiatun Formation complex are sandstone, mud-rich sandstone and island arc tholeiite.

对这些岩石的岩相学,稀土元素,微量元素地球化学的研究和斜长角闪岩Nd同位素的初步分析,表明孟家屯岩组的原岩建造为一套砂岩,富泥质砂岩和岛弧拉斑玄武岩组合。

The sharp difference suggests that they have different origins: the former comes from allochthonous sapropel-type organisms of the lower strata and is the remains of crude oil, and the latter is autochthonous humic-type organic matter of sedimentary rocks between the basalt layers.

玄武岩中铜矿石沥青的δ13CV-PDB为-27.3‰~-33.2‰,平均-31.97‰,沉积岩中铜矿石碳质的δ13Cv-PDB为-20.2‰~-23.2‰,平均-22.11‰,表明二者无明显成因联系,前者属腐泥型,为石油的遗迹,来自下部地层;后者为腐植型,来自原地沉积的陆生高等植物。

The dual water model considered the conductivity of shaly sand as a parallel connection result of conductive free water and clay water in pores.

双水模型把泥质砂岩的导电性看成是孔隙中粘土附近的粘土水和距粘土表面较远的自由水2种导电成份的并联结果。

The dispersion relates to water saturation in shaly sand formations.

在特定的频段,泥质砂岩的复电阻率存在明显的频散现象,这种频散与地层含油饱和度的关系密切,是目前复电阻率测井的基础。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。