Interaction of fluid dynamic factors in the migration and accumulation of natural gas

The migration of fluid petroleum gas, described as fluid potential, depends only on gravity, fluid pressure controlled by depression and capillary force during tectonically stable period; but on tectonic stress during the tectonically active period with severe compression. This method is applied in the Junggar Basin, showing that the migration of Jurassic gas during Cretaceous and Eocene and the migration of Permian gas from Jurassic till the present are determined by capillary force and fluid pressure (including overpressure) which is controlled by depression; the migration of Jurassic gas from Eocene till the present and the migration of Permian gas during Triassic are controlled by tectonic stress.     

Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China

The petrological characteristics and heavy mineral assembly of the Jurassic System in Kuqa Basin are consistent with the tectonic evolution, which is the major factor controlling the filling process of Kuqa Basin. Controlled by the source areas at the both sides of the Basin, the matrixes are dominated by sedimentary rock, high-grade metamorphic rock, acid magmatic rock, and the highest heavy mineral assemblage of zircon-garnet-magnetite in the content. According to heavy mineral indexes, the Jurassic strata can be classified into three rhythmic units of heavy mineral. The lower sequence contains abundant heavy minerals and relatively high content of detritus and its matrixes primarily came form the recycling orogen. The assemblage of “zircon-garnet-magnetite” indicates that the sedimentary area in the early evolution period of the basin is relatively near the provenance. The middle sequence is different from the lower sequence in the heavy mineral assemblage and has the different characteristics from that of source rock. The heavy mineral assemblage is “garnet-zircon” with the highest content of garnet and its main matrices are the high-grade metamorphic rock, acid magmatic rock and hydrothermal vein at the northeastern edge of the basin. The middle and upper sequences are characterized by the clast provenance, which is primarily from the recycling orogen at the northern edge of the basin and secondarily from the southern uplift. As a result of the two provenances, the strata with apparent changes of heavy mineral assemblage and index better coincides with the interfaces of the secondary strata sequences, which reflects the denudation history and the filling process of the orogen at the northern edge of the basin.     

Helium isotopic compositions in fluid inclusions of the Gangxi fault belt in the Huanghua Depression, Bohai Bay Basin

Helium is a trace constituent in natural gases and is the lightest element of all rare gases. Formed during natural nuclear processes, helium is chemically stable. Due to its strong diffusibility and permeability, helium can be used as a very sensitive tracer. Helium has two natural stable isotopes, 3He and 4He. 3He originates from the universal nebulae when the earth was formed, and 4He mainly originates from the radioactive disintegration of elements in the crust, such as U and Th [1]. In…     

浅析软式排球在全民健身运动中的发展前景

软式排球是一种寓竞技、娱乐和健身于一体的新兴体育项目,具有柔软、重量轻、气压小的特点.游戏规则、比赛规则和技术要求简单,对场地、网高等要求不高,便于推广开展.适合不同年龄、性别、体质和技能的人参与,经常参加软式排球活动有利于促进青少年生长发育,提高人体身体素质和运动能力,同时为硬式排球的发展打好基础,是一项适合全民开展的健身运动.     

正畸牙移动过程中龈沟液白细胞介素-8的变化

细胞因子白细胞介素-8(Interleukin-8,IL-8)被认为是重要的牙槽骨吸收调节因子,为评价正畸牙移动过程中牙周组织IL-8的水平,选择17颗需远中移动的正畸尖牙,酶联免疫吸附测定法定量分析加力前与加力后1 h、24 h、7 d、14 d及30 d龈沟液中IL-8含量的变化.结果显示:牙受力后1 h、24 h及7 d IL-8含量均较受力前显著增加(p<0.05),且在24 h达到峰值(p<0.01).表明在正畸加力初期,牙周组织IL-8含量显著增加.说明牙周组织对正畸力的生物应答反应导致IL-8增加和中性粒细胞聚集,这可能是骨改建的触发因素之一.     

香山群沉积岩浆记录及其反映的大地构造环境

目的探讨鄂尔多斯西南边缘香山群形成的大地构造环境,为鄂尔多斯盆地西南缘早古生代大地构造背景的恢复和确定提供佐证。方法通过香山群地层的岩石学、沉积学、砂岩和火山岩的岩石地球化学特征的系统研究,综合分析香山群形成的大地构造环境。结果香山群的时代划归为中晚寒武世较合适;香山群主体是一套由板岩、细、粉砂岩和砂岩组成的浊积岩系,其砂岩类型主要是长石石英砂岩、细粒石英砂岩和粉砂质石英砂岩,前寒武纪变沉积岩和花岗片麻岩为主要碎屑来源和物源区组成;砂岩的岩石地球化学特征指示香山群属发育在被动大陆边缘斜坡环境中的沉积物,火山岩岩石地球化学特征反映其应属大洋扩张构造环境下的大洋拉斑玄武岩系列。结论香山群形成于伸展构造背景下的被动大陆边缘中的大陆斜坡和深海平原环境。     

大倾角厚煤层综放开采颗粒元分析

应用PFC2D计算程序,对某矿水平与倾斜联合布置的折线型综采面,分析了散体顶煤和破碎直接顶的落放过程及落放形态,揭示了不同放煤步距连续推进模式下的煤损动态特征,并对不同放煤顺序的顶煤回收率及支架受力工况进行了优化分析. 研究表明:折线型综采面采用自上而下的回采顺序,顶煤回收率高,支架受力均匀;低位单口放煤时,放出体形态向采空区侧偏转;在支架连续推进过程中,煤损形态节律性变化;大倾角厚煤层综放开采,采用中档放煤步距的经济技术效果较好.     

略论《在延安文艺座谈会上的讲话》之前中国共产党的抗战文艺政策

《在延安文艺座谈会上的讲话》被学界认为是中国共产党的第1部正式的文艺政策文献,是中国共产党在处理重大文艺问题上承前启后的一份重要文件。在《讲话》出现之前,中国共产党的抗战文艺政策同样具有重要的研究价值,这一段时期的准文艺政策主要体现在重要领导人的著作和讲话中,其内容最终成为《讲话》的重要组成部分。     

龙门山造山带中生代花岗岩带成因及其构造意义

总结了龙门山造山带印支末 -燕山期花岗岩带地质地球化学特征及演化规律。在探讨其成因及构造意义的基础上 ,将龙门山造山带与传统的 A型与 B型俯冲带的岩浆作用进行了对比 ,指出龙门山造山带的岩浆作用的不同特点是其区别于传统 A型、B型及其他的一些内陆挤压俯冲带的重要证据     

羌塘盆地构造单元划分及含油气远景评价

对14条近4000km的大地电磁测探资料进行了一维及二维连续介质反演，根据反演结果及地面地质资料解释确定了侏罗系、上三叠统底界面海拨高度图以及前泥盆系顶界面海拔高度图，并根据以上研究结果以及地质资料对羌塘盆地进行了构造单元划分以及含油气远景评价。