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Using maximum flooding surface and local explosure erosion surface as the correlation framework surface in the 4-th hierarchical base-level cycles, sand-body in the 3-th hierarchical base-level cycles formed in the 4-th hierarchical base-level cycles may be correlated layer by layer. The law of the sand-body and the characters of reservoir heterogeneity formed in the 4-th hierarchical base-level cycles are discussed. The study shows:①During early period of the 4-th hierarchical base-level cycle rising, subaqueous distributary channel formed, continuously stacked vertically, and migrated in limit range laterally, and channel sand-body stretches farther longitudinally, and lacks interbeds of mud rock and siltsand in sand rock, reservoir heterogeneity is relatively weak.②During mid-period of the 4-th hierarchical base-level cycle rising, subsaqueous distributary channel migrated actively, channel divided and converged strongly to form netted sand-body and sand sheet mainly, but interbeds of mud rock and siltsand increases gradually in sand-body, reservoir heterogeneity increased.③During later period of the 4-th hierarchical base-level rising and early period of the 4-th hierarchical base-level falling, reservoir sand-body was poor, and only form thin sand-body of subsaqueous distributary channel, subsaqeuous creveas and distal mouth bar, sand-bodys are surrounded by mud and silt rock.

进一步采用以第4层次基准面旋回中相当最大湖泛面的相转换面和具有区域性暴露侵蚀作用的层序边界面为等时地层对比框架的边界,对发育于MSC2—MSC4三个第4层次基准面旋回的第3层次基准面旋回内砂体进行了逐层等时对比,探讨第4层次等时地层对比格架内储集砂体发育分布规律,及储集砂体的非均质性特点,研究发现:①第4层次基准面上升初期发育的水下分流河道,砂体呈连续叠置、侧向迁移受限,纵向上呈长距离延伸的带状产出,砂体间泥、粉砂岩夹层少,储层非均质性相对较弱;②在第4层次基准面上升中期发育的水下分流河道侧向迁移活跃,纵向延伸过程中分流汇合作用强烈,以形成网状或席状连片砂体为主,但砂体间泥、粉砂岩夹层逐渐增多,储层非均质性增强;③第4层次基准面上升晚期和下降早期,不利于储集砂体发育,仅出现少量薄的水下分流河道、水下决口扇、远—河口砂坝砂体。

During early and middle Jurassic period, as a northern boundary, the fault zone controlled a seires of sedimentation of coal basins and magma activity. A lot of nappes developed during Ⅰ,Ⅱ and Ⅲ phase of the Yanshan movement. The strongest structural activity during the Yanshan movement is the Ⅱ phase, It had three pulsation and formed large-scale tectonic system with dextral strike slip.

早、中侏罗世,断裂带作为北界,控制了由西向东一系列煤系盆地的沉积作用和岩浆活动;在燕山运动的Ⅰ、Ⅱ、Ⅲ幕中分别形成了一系列逆冲构造;其中,以燕山Ⅱ幕构造活动最强,并至少经历了三次脉动作用,形成的逆冲构造不是由盆缘到盆内的&对冲&,而是受本断裂带限制,并以之为主滑面构成了区域上的大型右行走滑斜压式构造系统。

It is key point to understand how to restore the sporters'energy after they exercise during train seasons.After swimmers took supplement of the beverage compounded taurine designed for swimmers during training,their hemanalysis and kinesiology experiment were carried on. The experiment result testifies swimming sporters' tolerant and kinetic capability had been improved, did not have the overfatigued during the winter training.

运动训练中如何更好地促进运动员机能的恢复是训练中的重要环节,针对游泳运动员的特点,在训练中进行牛磺酸复合功能性饮料的补充,并在补充前后进行有氧功率自行车的运动测试和血样的分析,结果表明运动员有氧耐力水平和运动能力都有一定的提高,冬训期间未出现过度疲劳的现象。

As a whole, during Authoritarian Regime period Wu San-Lian and《Independent Evening News》were performed as a "miserable hero", that is to say, during the enlightenment period of Taiwan democratics , Wu San-Lian and 《Independent Evening News》is the symbol of Taiwan democratic politics, during the pursuing of democratic politics and freedom of speech, Wu San-Lian and 《Independent Evening News》can be said as "sacrifying themselves and lighting up democratic system".

整体而言,吴三连与《自立晚报》在威权体制时期是一个「悲剧英雄」的角色,也就是在台湾民主启蒙阶段与风起云涌时,吴三连与《自立晚报》是台湾民主政治的象徵橱窗,在追求民主政治与言论自由的历程中,吴三连与《自立晚报》可说是「燃烧自己、照亮民主制度」,最后是油尽灯枯,随著威权体制的解体而逐步走入了历史。

The data showed that the HRV and the sympathetic activity indices of the worry group were lower during the mental task stage than during the fearful movie stage. Moreover, the HRV and sympathetic activity indices of the members of the worry group were also lower than those of the re-exposure group during the mental task stage.

结果发现,在忧虑组各实验操弄之组内比较上,受试在的作业期之HRV与交感神经活性指标显著低於电影期;且三组受试在作业期之组间比较上,忧虑组的HRV与交感神经活性指标显著低於回忆组。

Based on aforementioned findings, the author disclosed China have gone through three wave of marketing since the open policy reform in the end of seventies in the last century: the first wave taken place from the end of seventies to the end of eighties of last century, during this period of time, enterprises commonly took a marketing tactics mix of unitary product, high gross-profit pricing, wholesale and information notification; the second wave happened from the end of eighties to the end of nineties in the last century, during the second wave, enterprises often took a marketing tactics mix of serialized products, medium gross profit pricing, regional distribution and advertisement on mass media; the third wave occurred from the end of nineties of last century to now, during the third wave, enterprises usually adopted a marketing tactics mix of segmented products, low gross profit pricing, outlet interception and tangible benefits promotion.

基于上述认识,本书进而揭示出,中国市场自上个世纪70年代末改革开放以来,已经经历了三次营销浪潮:第一次营销浪潮发生在20世纪70年代末至80年代末,期间,企业界普遍采取的是&单一化产品+高毛利政策+批发销售+信息告知&的链接标记营销策略组合。第二次营销浪潮发生在20世纪80年代末至90年代末,期间,企业界普遍采取的是&系列化产品+中毛利政策+区域链接标记分销+大众链接标记广告&的营销策略组合。第三次营销浪潮发生在20世纪90年代末至今,期间,企业界普遍采取的是&细分化产品+低毛利政策+链接标记终端拦截+实惠促销&的营销策略组合。

Based on aforementioned findings, the author disclosed China have gone through three wave of marketing since the open policy reform in the end of seventies in the last century: the fi rst wave taken place from the end of seventies to the end of eighties of last century, during this period of time, enterprises commonly took a marketing tactics mix of unitary product, high gross-profit pricing, wholesale and information notification; the second wave happened from the end of eighties to the end of nineties in the last century, during the second wave, enterprises often took a marketing tactics mix of serialized products, medium gross profit pricing, regional distribution and advertisement on mass media; the third wave occurred from the end of nineties of last century to now, during the third wave, enterprises usually adopted a marketing tactics mix of segmented products, low gross profit pricing, outlet interception and tangible benefits promotion.

基于上述认识,本书进而揭示出,中国市场自上个世纪70年代末改革开放以来,已经经历了三次营销浪潮:第一次营销浪潮发生在20世纪70年代末至80年代末,期间,企业界普遍采取的是&单一化产品+高毛利政策+批发销售+信息告知&的营销策略组合。第二次营销浪潮发生在20世纪80年代末至90年代末,期间,企业界普遍采取的是&系列化产品+中毛利政策+区域分销+大众广告&的营销策略组合。第三次营销浪潮发生在20世纪90年代末至今,期间,企业界普遍采取的是&细分化产品+低毛利政策+终端拦截+实惠促销&的营销策略组合。

Based on aforementioned findings, the author disclosed China have gone through three wave of marketing since the open policy reform in the end of seventies in the last century: the first wave taken place from the end of seventies to the end of eighties of last century, during this period of time, enterprises commonly took a marketing tactics mix of unitary product, high gross-profit pricing, wholesale and information notification; the second wave happened from the end of eighties to the end of nineties in the last century, during the second wave, enterprises often took a marketing tactics mix of serialized products, medium gross profit pricing, regional distribution and advertisement on mass media; the third wave occurred from the end of nineties of last century to now, during the third wave, enterprises usually adopted a marketing tactics mix of segmented products, low gross profit pricing, outlet interception and tangible benefits promotion.

基于上述认识,本书进而揭示出,中国市场自上个世纪70年代末改革开放以来,已经经历了三次营销浪潮:第一次营销浪潮发生在20世纪70年代末至80年代末,期间,企业界普遍采取的是&单一化产品+高毛利政策+批发销售+信息告知&的营销策略组合。第二次营销浪潮发生在20世纪80年代末至90年代末,期间,企业界普遍采取的是&系列化产品+中毛利政策+区域分销+大众广告&的营销策略组合。第三次营销浪潮发生在20世纪90年代末至今,期间,企业界普遍采取的是&细分化产品+低毛利政策+终端拦截+实惠促销&的营销策略组合。

In this study we use logbooks of purse-seine fishery during 1986 ~ 2002, AVHRR SST at a 4 km grid during 1986 ~ 2002 and SeaWiFS Chla at a 1 km grid during 1998 ~ 2002 as data availability permitted.

三类密度资源(CPUE1.0 t/网次、1.0≤CPUE2.0 t/网次、CPUE≥2.0 t/网次)出现面积的逐月变化各不相同,高密度资源出现面积最大的时间在3月及8 ~ 9月。

The relationship between mantle fluid and U ore-forming was studied preliminarily,according to the results,the author considered theΣCO_2 of mineralizer and heat source came from mantle,which is because upwelling mantle forced by crustal extention and deep-seated faulting produced melt blending with lower crust,during this process,mantle provided the heat and releaseΣCO_2 to crust through outgassing.U mainly came from mantle-curst fluid formed by mantle-curst melt blending and the wall rock during fluid uplift.H_2O mainly generated from mantle fluid and the wall rock during mantle fluid uplift,and partly from atmospheric water in the late period of ore-forming.

初步探讨了地幔流体与铀成矿作用的关系,认为矿化剂∑CO_2和热源来源于地幔,是地壳拉张和深大断裂活动导致部分熔融地幔上涌,与下地壳产生壳幔混熔作用,在混熔过程中提供热量和向地壳&去气&释放∑CO_2;U主要来源于壳幔混熔形成的壳幔混合流体和流体上升途经的围岩;H_2O主要来源于地幔流体、地幔流体上升途经的围岩,在成矿晚期有部分来源于大气降水。

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Lugalbanda was a god and shepherd king of Uruk where he was worshipped for over a thousand years.

Lugalbanda 是神和被崇拜了一千年多 Uruk古埃及喜克索王朝国王。

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