古

Therapontigonus Miles could walk arm in arm with Vadeboncoeur the grenadier, Damasippus the second-hand dealer would be happy among bric-a-brac merchants, Vincennes could grasp Socrates in its fist as just as Agora could imprison Diderot, Grimod de la Reyniere discovered larded roast beef, as Curtillus invented roast hedgehog, we see the trapeze which figures in Plautus reappear under the vault of the Arc of l'Etoile, the sword-eater of Poecilus encountered by Apuleius is a sword-swallower on the PontNeuf, the nephew of Rameau and Curculio the parasite make a pair, Ergasilus could get himself presented to Cambaceres by d'Aigrefeuille; the four dandies of Rome: Alcesimarchus, Phoedromus, Diabolus, and Argyrippus, descend from Courtille in Labatut's posting-chaise; Aulus Gellius would halt no longer in front of Congrio than would Charles Nodier in front of Punchinello; Marto is not a tigress, but Pardalisca was not a dragon; Pantolabus the wag jeers in the Cafe Anglais at Nomentanus the fast liver, Hermogenus is a tenor in the Champs-Elysees, and round him, Thracius the beggar, clad like Bobeche, takes up a collection; the bore who stops you by the button of your coat in the Tuileries makes you repeat after a lapse of two thousand years Thesprion's apostrophe: Quis properantem me prehendit pallio?

米勒会挽着侍卫华德朋克尔的胳膊，达马西普会在旧货店里流连忘返，万森刺杀苏格拉底正如阿戈拉囚禁狄德罗，格利木·德·拉雷尼埃尔会做油脂牛排正如古尔第吕斯发明烤刺猬。我们见到普劳图斯著作中的高架秋千重现在明星门的气球下面，阿普列乌斯在普西勒遇见的吞剑人便是新桥上的吞刀人，拉穆的侄儿和寄生虫古尔古里翁是一对，埃尔加齐尔请爱格尔弗依把他介绍给康巴色勒斯，罗马的四个纨袴子弟阿尔色西马尔古斯、费德洛木斯、狄阿波吕斯和阿尔吉里帕乘着拉巴突的邮车从拉古尔第①出发，奥吕·热尔在孔格利奥面前没有比查理·诺缔埃在波里希内儿面前待得更长久，马尔东不是母老虎，但是巴尔达里斯卡也绝不是一条龙，滑稽人潘多拉布斯在英格兰咖啡馆里嘲弄享乐人诺曼达纽斯，埃尔摩仁是爱丽舍广场的男高音，并且在他周围有无赖特拉西乌斯扮成波白什②向人募捐，在杜伊勒里广场上掐住你的衣扣、不让你走的那个讨厌人让你在两千年以后还重复着忒斯卜利翁的那句话："在我有急事时谁突然抓住了我的衣襟？"

Mars has two moons, Phobos and Deimos, which are small and oddly-shaped.

大约4000年前，古埃及人称她为"红色之星"；而古巴比伦人则称这颗"红色之星"为"死亡之星"；古希腊人和古罗马人好像对火星也没有好感，认为自己在地球上的一举一动总是被火星上的"人"监视着，所以为她取了一个不太友善的名字：Mars，即古罗马战神的名字，甚至把她视为"星际大战"的恐怖星球。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

On the basis of pollen analysis of surface sample in North China, polynomial function analysis method was applied to establish pollen climate response surface of Pinus, Betula, Quercus, Artemisia, Chenopodiaceae, Compositae, Picea, Ephedra, Gramineae in North China, therefore an easy and applicable method for reconstructing palaeoclimate and palaeoenvironment with data of fossil pollen was founded; Multi-analysis method was applied to analyse the principal elements of surface sample pollen in central Inner Mongolia Steppe, the assemblages of surface sample pollen in steppe area and its relationship with vegetation type were discussed with helps from spore-pollen analysis of a peat section in Chasuqi, Inner Mongolia and 〓C chronometer, fossil pollen data were obtained with high resolution on the peat section in Chasuqi. Vegetation succession and environmental changes since Holocene at resolution of 70 years were primarily reconstructed in south Mount Daqingshan and Plain Tumete. The changes in the area were copmared with those in the neighbouring areas during the same period. It was found that Holocene environmental change had undergone the following stages: cold-arid, temperate-wet, warm-wet, temperate-arid and cold-arid, and the climatical optimum period occurred in 5000-4100 aB.

本文在对中国北方表土花粉研究的基础上，采用多项式函数回归方法建造了中国北方松属、桦属、栎属、蒿属、藜科、菊科、云杉属、麻黄属、禾本科等的花粉——气候趋势面，从而为利用化石花粉资料直接恢复古气候、古环境提供了一种方便易行的方法；采用多元分析方法对内蒙古中部草原区表土花粉进行了主成分分析，探讨了草原区表土花粉组合的规律及与植被类型的关系；本文还应用孢粉分析方法，结合〓C测年技术，通过内蒙古中部察素齐泥炭剖面高分辨率的化石花粉数据，初步恢复了大青山山地南部及土默特平原地区分辨率为70年的全新世以来植被演替和环境变迁的状况，并与邻近地区的全新世古气候、古环境进行了对比研究，研究发现，本区域全新世古环境的变迁序列基本上可以与周围地区及华北地区进行对比，其环境变迁经历了凉干～温湿～暖湿～温干～凉干的变化，且气候最适宜期出现在5000～4100aB.P。

Through investigation of paleoflood deposits on the Xiaolangdi reach of the Yellow River, and by use of the field mark system for deposits judgement , identified are three types of the paleoflood deposits with four characteristics,and four geomorphologic types for the valid kind of slack water deposit.

通过分析古洪水沉积的环境及应用沉积物识别的野外特征指标体系，指出黄河小浪底河段的古洪水沉积分为 3种类型，具有 4个特点，其中赋存古洪水平流沉积的地貌类型有 4种。这一研究成果为在野外寻找及判断黄河小浪底河段的古洪水沉积提供了科学依据，对古洪水研究具有普遍指导意

Deep studies on the Holocene loess-palaeosol sequences and the slack water deposits profiles, identifying and obtaining the information of paleoflood recorded in them, ensuring the amount, frequency, time and scale of the extreme Holocene paleofloods, are very helpful in revealing the characters and rules of the environment change during Holocene in this drainage basin and the middle reach of the Yellow River.

深入研究古遗址周围的黄土——古土壤地层和古洪水平流沉积物，识别和获取蕴藏其中的古洪水信息，并以此确定全新世特大古洪水事件发生的次数、频率、时间及规模，有助于揭示伊洛河流域及黄河中游地区全新世环境演变的特点和规律。

In the early Paleozoic and Indosinian cycle, the tectonic movement is weak, and the rock has acoustic emission once, whose maximum paleo-stress is 13.3MPa and 24MPa, moreover the Majiang ancient reservoir is in the mainly accumulation period; the high frequency and intensity paleo-stress correspond to the Majiang ancient reservoir's reservoir comes into being or destruction. The single Neopaleozoic acoustic emission whose maximum paleo-stress is 92.6MPa means the reservoir comes into being.

在早古生代末期和印支期构造运动较弱，测试岩石的发声一次，古应力值分别为13.3MPa和24MPa，是麻江古油藏的主要成藏期；声发射次数较多或者古应力值较大时的时期，主要对应于麻江古油藏储层的发育期和油藏大规模破坏期。

The reason included five aspects:①the effect of physical environment: the open geographical environment and barren soil urge the Greeks to look for development outward while the close geographical environment and advantaged condition for agriculture shaped the Chinese conservative thought and obstructed their steps of going out.②the advancing and blocking of the economic: the frequent trade offered an abundant living supply and open view while the self-sufficient agriculture with restraining trade rigidified the thought.③ the difference in politic institute and situation: the democracy polis of ancient Greece is exclusive in the ancient world. It shaped the atmosphere of freedom, democracy and adversary. While the monarchy in ancient China pursued the "united country" and shaped the atmosphere serving for politic and consolidating thoughts.④the guiding of traditional culture: the Greeks pursued freedom and wisdom and were curious about nature while the Chinese adored ancestor and obeyed the authority and prefer to pragmatism.

出现这种关系的原因本文从以下五点进行分析：①自然环境的影响：古希腊开放的地理环境和贫瘠的土壤种植条件促使古希腊人向外寻求发展，而古代中国封闭的地理环境和优越的农业环境阻碍了中华民族外出的脚步和开放的思维；②经济条件的推动与束缚：工商业发展的农业经济和自给自足的小农经济所创造的物质条件和对思维影响的差别是很大的；③政治制度和政治形势的差异：古希腊民主城邦制在古代世界是独树一帜的，它所营造的自由、民主的氛围和古代中国追求&大一统&的君主专制下为政治服务、思想趋向统一的氛围截然不同；④传统文化的引导：古希腊人在长期的城邦生活和参与海外贸易的生活中形成的开放、自由、对自然充满好奇、追求智慧等民族文化传统与中国保守崇古、讲究实用的文化传统形成了鲜明的对比；⑤思想家本身目的不同：古希腊思想家为了变得智慧而获取知识，享受知识带来的乐趣，而古代中国思想家的一切动机都是为了&成化天下&、&以政裕民&服务。

The company's main ancient furniture, ancient wood carvings, ancient stone inscriptions, ancient stone cylinder, and other customers, as well as tailor-made antique furniture, antique stone, run antique porcelain, pottery, jade, bronze, ancient calligraphy and painting, and a variety of miscellaneous items, such as, China's western region the size of the largest and richest collections of ancient furniture collection of ancient stone inscriptions operating companies.

公司主营古家具、古木雕、古石刻、古石缸等以及为客户量身定做仿古家具、仿古石刻，兼营古玩瓷器、陶器、玉器、铜器、字画古籍、以及各类杂件等，为中国西部规模最大、藏品最丰富的古家具古石刻收藏经营公司之一。

The paleochannel-Ⅱ might form during the Holocene Optimal period.

古河道-Ⅴ形成于风沙-Ⅱ和Ⅲ期形成之前，可能是末次冰期之前，即中更新世或更早，这时河流能够进入古松辽大湖；古河道-Ⅳ形成于风沙-Ⅱ和Ⅲ期形成之时，可能是末次冰期时期，这时河流与松辽大湖萎缩，规模减小，河流已不能进入松辽大湖，而是消失在沙地之中；古河道-Ⅲ形成于风沙-Ⅱ和Ⅲ期形成之后，可能是末次冰期末期的冰消期，这时气温升高，大量的冰雪融水进入河流，促使河水漫流，流入沙垅垅间洼地，开始造成古西拉木伦河、古老哈河与教来河水文网之间的相互联系；古河道-Ⅱ形成于全新世适宜期时期，统一的西辽河形成，伴随气候变化，出现多次风沙进退，对应于风沙-Ⅰ期；河道-Ⅰ是现在，同属于风沙-Ⅰ期，活动沙地集中在翁牛特等地。

Do you know, i need you to come back

你知道吗，我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书，王祥生，李德昌。安徽省首次发现嗜群血蜱。