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The study of the mineralization degree ,water type and ion combination coefficient of the Pre-Tertiary formation water in Chaluhe fault depression,Yitong Basin,reveals that total mineralization degree of the water is relatively low,and NaHCO3 water type,while the formation water has obvious vertical mineralization zonation with a high metamorphic grade.

对伊通盆地岔路河断陷古近系地层水的矿化度、水型及变质系数、脱硫系数的研究表明,该区地层水总体为NaHCO3型水;总矿化度偏低;平面上,孤店斜坡的油气保存条件最差,梁家构造带最好,垂向上,具明显的垂向分带性,万昌组保存条件最差;变质程度高。

Thereinto, the function of IAA on blocking the formation of stolons and the function of JA on tuber formation were prominent, and both maybe involved into the expansion of tuber.

其中IAA在抑制匍匐茎的形成,JA在促进块茎发生的作用上更为明显,两者还与块茎的膨大有关。

Theoretical analysis reveals that the formation of flower-like splats results from the interaction of surface tension, inhomogeneity of thermal contact resistance between flattening drop and substrate and substrate crater. The formation of the craters on the substrate is mainly controlled by substrate melting.

理论分析表明,&花瓣状&层片的形成是熔体表面张力、熔体与基底接触热阻的不均匀性和基底凹坑相互作用的结果;基底凹坑的形成主要由基底熔化所控制。

Relatively, Cr2O3 is higher in spherules of the Changzhougou Formation but FeO higher in the Dahongyu Formation.

相对比较Cr2O3在常州沟组中较多一些,而FeO在大红峪组中稍多一些。

Numerous iron spherules have been found from coarse sandstone in the bottom of the Changzhougou Formation (1.8Ga) and silicified carbonate rock of the Dahongyu Formation (1.6Ga) of Proterozoic strata of the Ming Tombs District, Beijing.

北京十三陵中元古代常州沟组底部的粗砂岩(l.8Ga)和大红峪组硅化碳酸盐岩(1.6Ga)中都发现了众多铁质宇宙球粒。

In view of a little thickness and limited oil-forming potential of source rock of Member 2 of the Shahejie Formation, the source rock in Member 3 of the Shahejie Formation is considered as the main source of oil and gas.

考虑到沙二段烃源岩厚度小,生油能力有限,唐家河油田沙三段烃源岩是最主要的油气来源。

During the last three decades, several models have been proposed to explain the formation of somites, including the clock and wavefront model, the reaction-diffusion type model, clock and induction model, clock and trail model etc. Although some of them are satisfactory in the different aspects of somitogenesis, no one can explain the formation and regulation of somites perfectly.

近三十年来,研究者们就体节的发生和发育提出了多种解释模型,这包括时钟波阵面模型,反应扩散模型,时钟诱导模型,时钟痕迹模型等,虽然这些模型能从不同角度不同程度来解释动物体节发生和发育的不同现象,但无一能够解释体节发生和发育的全部。

CO2 and H2S exist in the hydrocarbon zone and foramtion water,as the accompany gases of petroleum and nature gaso or components of formation water,which will cause corrostion to the cement sheath under certain conditions of humidity and pressure.It will decrease the cement sheath's alkalinity,which results in the decrease of cement sheath's strength,permeability increase,and places a premium on fluid channeling and borehole wall sloughs accident in plastic formation,shortening the oil- gas well's production lifetime and giving rise to tremendous ecomonic losses.

CO2和H2S作为石油和天然气的伴生气或地层水的组分存在于油气层或地层水中,在一定的湿度及压力条件下会对固井水泥环产生腐蚀作用,从而降低水泥环的碱性,使水泥环强度下降,渗透率增大,并诱发流体窜流、塑性地层井壁跨塌等事故,从而缩短油气井的生产寿命,造成巨大的经济损失。

In this thesis, nano-scale particles of metals, metal sulfides, selenides, oxides and nano-composites of metals/polymer, semiconductor sulfides/polymer have been successfully prepared by γ-ray irradiation technique in sorts of systems including water system, alcohol system, ethylenediamine system, microemulsion and emulsion system at room temperature and under ambient pressure. The possible formation mechanisms of nano-scale materials were suggested, and some factors of affecting the formation of nano-materials were studied.

本论文使用〓Co-γ射线辐射技术,在常温常压下分别于水体系、乙醇体系、乙二胺体系、微乳液和乳液体系中,成功地制备了纳米金属、硫化物、硒化物、氧化物以及金属/聚合物、半导体硫化物/聚合物纳米复合材料,并初步探讨了纳米材料形成的可能机理和影响因素。

During later Paleogene and early Neogene, Jiyang Depression undergone from rifting activity to depression activity. During early Guantao Formation, fault active, highland eroded, slope overlapped and sags filled, and then when later Guantao Formation begin sedimented, paleotopography became plainness, new stratum overlaid all old stratum, intensity of fault activity gradually got in weaken, and developed the sedimentary system of alluvial-fluvial-freshwater shallow lake.

济阳坳陷在古近纪晚期,新近纪早期由断陷活动转为坳陷活动,经过馆陶早期的断剥超覆和填凹补平作用,到馆陶晚期古地形渐趋平缓,新地层覆盖在所有老地层之上,断层活动强度逐渐减弱,发育冲积扇-河流-淡水极浅湖沉积体系,具有良好的生储盖配置关系。

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The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应,而且减少跟风的可能性。

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