纪

His history is recorded in 1 Kings 1-11 and 2 Chr.

他的历史记录在列王纪上1月11日和2染色体。1-9。

Chronicles are the words of the days, 1 Kings 14:19; 1 Chr.

纳尼亚是的话，天，（列王纪上14：19 ； 1染色体。

Before his death David gave parting instructions to his son 1 Kings 2:1-9; 1 Chr.

他去世之前大卫临别指示了他的儿子（列王纪上2：1-9 ； 1染色体。

They reached their height in the 5th 4th century. B.C.; thereafter they became more and more professionalized until, in the Roman period. they provoked much censure. They were eventually discontinued by Emperor Theodosius I of Rome at the end of the 4th century A.D.

在公元前5世纪纪公元前4世纪，古代奥运会发展到最高阶段，以后这种奥运会变得越来越职业化了，直到罗马帝国时代，奥运会引来众多责难，最后在公元4世纪被罗马皇帝狄奥多西一世废除了。

The two lovers continued long together, as they were wont, all unwitting of Tancred; but at length they saw fit to get out of bed, when Guiscardo went back to the grotto, and the lady hie d her forth of the room.

那一对情人像往常一样，温存了半天，直到不得不分手的时候，这才走下床来，全不知道唐克莱正躲在他们身边。纪斯卡多从洞里出去，她自己也走出了卧房。

Such was the lamentable end of the loves of Guiscardo and Ghismonda; whom Tancred, tardily repentant of his harshness, mourned not a little, as did also all the folk of Salerno, and had honourably inter red side by side in the same tomb.

这就是纪斯卡多和绮思梦达这一对苦命的情人的结局。唐克莱哭也无用，悔也太迟，于是把他们二人很隆重地合葬在一处，全萨莱诺的人民听到他们的事迹，无不感到悲恸。

In Tengchong ,the diatom was occurred in several Cenozoic lake basin formed by the intensive structural movement after Eogene.

古近纪之后，强烈的构造运动在腾冲形成数个新生代湖盆，成为硅藻生存场所。

They correspond respectively to two phases of extensional activities in Late Cretaceous and Eogene as well as development of the Qianshan fault-controlled basin to the east of the Tan-Lu fault zone.

这两次快速冷却事件分别对应于断裂带晚白垩世、古近纪两次伸展活动，并控制发育了断裂带东侧的潜山断陷盆地。

The U-P dating data of zircons imply that topography was low in the west and high in the east of East China Sea shelf during the development of Eogene basin.

根据上述砂岩锆石U-P年龄，可以推测古近纪东海陆架盆地发育过程中，东海陆架东部地势较高。

The Well Fu 1 is a regional exploration well in Fula Depression , M Basin, in which the high production commercial oil was obtained.

穆格莱德盆地福拉凹陷是在中非剪切带剪切应力场背景下形成的以中生代沉积为主的裂谷凹陷，裂陷活动可分为早白垩世、晚白垩世和古近纪3个阶段，主要形成南北和北西-南东走向两组断裂。

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。