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As everyone knows, since the Chinese Government to lift the ban, brought about a turning point to the Chinese, have the Chinese language schools throughout the country in l966, despite being banned, but the friendship between the alumni are still not absolutely continuous with the Chinese culture is still Needless relationship doubt, as a link in the activities of various alumni lifting of the ban after the Chinese, have sprung up, the Chinese Government attaches importance is reflected not only in the highest levels of policy making, but also for the Chinese to take quite open attitude, in such historical conditions , Alumni play a vital role in the major cities and towns are active in the Chinese one by one from the Chinese community organizations to set up non-professional Chorus and Choir, alumni, such as silver will be the enthusiasm of the growing number of aspects, As people on the amateur requirements of the diverse cultural life, especially Chinese singing is still the largest of the fun of life, the choral music as a form of life as an option, the activities carried out by the chorus, not the pursuit of music career the highest ideals, only enriched the cultural life of Chinese amateur in the chorus of collective experience in the art of choral charm problems, temperament, for the building of a harmonious society.

而他们选择了前者, They chose the former,众所周知,自政府解除对华文的禁令,给华人带来了转机,曾经遍布全国的华文学校虽然在l966年被查禁,但校友之间的情谊仍然绵绵不绝、与中华文化的亲缘关系仍是毋庸置疑,以此为纽带,各类校友的活动在华文解禁之后,如雨后春笋般涌现出来,目前政府对于华文的重视不仅体现在最高决策层,还对于华文采取相当开放的态度,在这样的历史条件下,使校友会发挥巨大的作用,当前各大中城市和乡镇中活跃着一个又一个由华人华社组织兴办非专业合唱团和歌咏团、校友会、银会的热情等方面数量日益增长,也随着人们对业余文化生活要求的多样化,尤其唱歌仍然是华人生活中最大的乐趣,把合唱作为音乐艺术的一种形式,生活的一种选择,通过合唱活动的开展,不追求音乐艺术生涯的最高理想,仅仅丰富了华人的业余文化生活,在合唱的集体中感受合唱艺术的魅力,陶冶性情,为构建和谐社会作出贡献。

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。

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