古

An ancient Greek priest who interpreted sacred mysteries, especially the priest of the Eleusinian mysteries.

古希腊祭司古希腊解译秘密宗教仪式的祭司，特指依洛西斯秘密宗教仪式的祭司

In the late Eopaleozoic period, large-scale concourse movement took place in Palaeo-Asian Ocean, and the combined Kazakhstan Plate was formed. Junggar Basin has become a part of this plate and entered the inter-plate cratonization evolutionary phase.

早古生代后期，古亚洲洋发生了大规模的汇聚运动，哈萨克斯坦联合板块形成，准噶尔成为其一部分，进入板内克拉通化演化阶段。

The permo-carboniferous coal measures in North China Basin were formed under the condition of epicontinental sea which was characterized by the extreme gentle slope and high frequency of sae-level changes, the contemporaneous margin portion of which was probably very far or had been destroyed during the proccess of plate subduction and continental collision. The lowstand systems tract, therefore, has not be discovered up to now.

华北晚古生代内陆表海古地貌上表现出的极缓的基底和海平面的高频变化，具有特殊性，其同期的边缘海部分可能距离很远或在板块消减及大陆碰撞过程中被破坏掉，因而至今未发现低位体系域存在的证据。

For example, the eastern North China tableland is Early Paleozoic restricted oceanic tableland, while the western is the Paleozoic epicontinental tableland.

如华北台地，其中东部为早古生代局限海台地，西部为古生代陆表海台地；四川陆表海台地；塔里木、江南和西藏陆缘海台地。

Chagan sag is a secondary tectonic unit in Chagandelesu Depression, northeastern Yingen-Ejinaqi basin, and the basement of the basin is a Paleozoic fold belt of continental margin or island arc at the connection region of North China plate* Tarim plate and Kazakstan plate, with the character of erogenic belt.

查干凹陷属于银根—额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元，其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带，具有古生代造山带的性质。

It is true that none is etymologically derived from the Old English word n,"one," but the word has been used as both a singular and a plural noun from Old English onward.

事实是这样的： none 根据词源学来自于古英语词汇 an &一，&但是此词从古英语开始既被用作单数名词，又被用作复数名词形式。

The geochemical abnormity are characterized by strong correlation with the eustatic changes of sea level and the significant changes of paleoenvironment in the east Yangtze Gorges area.

结果表明，该区早奥陶世牙形石的REE和微量元素地球化学异常与海平面的升降、古环境的变化有关联，与已有的古生物地层、古地理研究结果一致。

The earliest and reliable Castanopsis fossil records date back at least to Eocene, and subfamily Castaneoideae fossil records found from Paleocene, it is indicated that appearance of Castanopsis is not later than Paleocene . All fossil records of Fagaceae and Castanopsis report from the Northern Hemisphere and their main distribution regions are in the Northern Hemisphere . It can be concluded that the Northern Hemisphere is the center of origin of Fagaceae and Castanopsis . However, owing to the discrepancy between fossil data and results of modern botany research as well as scarcity of fossil data from key area, precise center of origin of Castanopsis cannot be inferred.

栲属在地质历史上有着比现在广泛的分布，最早、最可靠的栲属化石记录发现于始新世地层，栗亚科化石在古新世就有发现，化石记录表明栲属起源的时间不晚于古新世，所有的壳斗科及栲属的化石都发现于北半球，现代分布也主要在北半球，壳斗科及栲属起源于北半球可以确认，由于化石证据与现代植物学的研究结果有较大差异以及关键地区化石证据的不足，具体的起源地尚不能肯定。

In terms of structural characteristics and geochemistry of the granites in conjunction with previous studies, we interpret that the garnet-bearing gneissic granite was formed during the collision between the Tianshuihai terrane and the Southern Kunlun terrane following the closure of a branch of the paleo-Tethyan ocean along the Mazha-Kangxiwa suture zone, the block hornblende-bearing granite was formed during post-orogenic extension. On the other hand, the granites of ca.

根据两个岩体的构造特征，结合前人的研究及地球化学特征，表明含石榴子石片麻状花岗岩形成于同碰撞造山时期，是甜水海地体与西昆仑南带晚古生代岛弧沿麻扎-康西瓦缝合带碰撞峰期的产物，代表了沿麻扎-康西瓦分布的古特提斯洋一个分支的闭合，而228 Ma块状含角闪石花岗岩形成于碰撞造山后的伸展背景。220～190 Ma持续发育的花岗岩是南昆仑地体拼合到北昆仑地体之后在其南部形成的新的深成岩浆弧带。

The writings of the early Gurus were compiled in the Adi Granth, the Sikh sacred book, by Arjun (1563-1606), the fifth Guru.

早期古鲁的著作由第五位古鲁阿尔琼（1563-1606）编纂在《阿第格兰斯》里。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。