向西

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？"

The Corinthians declared war on Corcyra, who then appealed for help to Athens.

科林斯人向科西拉宣战，科西拉就向雅典求助。

In thessaly there once lived a king by the name of ixion.he was both handsome and mighty.he went to woo the beautiful maiden dia and won her love,but her old father was most reluctant to part with his child.only when ixion swore to let him have his royal treasure house did the father agree to give the king the hand of dia in marriage .ixion took dia home with him.but he was in no mood to keep his promise,for a long time passed and no treasure ever came to the old man.impatient to have his promised wealth,the old father went to see ixion and gave him no peace,until at last ixion decided to get rid of him once and for all .opening the door of his treasure house,he pushed the old man in and there burnt him to death.

以前有个叫伊克西翁的国王居住在色萨利。他既英俊潇洒又力大无穷。他向美丽的姑娘黛求婚。黛和他一见倾心，但是她的父亲却极不情愿离开他的孩子。最后只有当伊克西翁发誓让黛的父亲得到王室的金库时，这位父亲才答应把黛嫁给了国王。伊克西翁把黛领回家。但他却丝毫没有履行诺言的意思。很长时间过去了，老人没有得到半厘钱。于是老人迫不及待地去找伊克西翁，絮絮叨叨搅得他不得安宁。终于伊克西翁决定索性彻底除掉老头。

But the geological and geochemical analyses showed that there existed a set of high quality marine source rock in the platform slope facies of Middle Ordovician Pingliang Formation. The oil and gas generated from the source rock of Pingliang Formation was accumulated firstly in the central Palaeo-uplift and its surrounding regions. The thermogenic asphalt in palaeo-uplift carbonate reservoir indicated that oil accumulation completed transition from oil to gas in the Lower Crataceous. Along with the palaeo-uplift axis convection and the formation of westward monocline in the Late Crataceous, gas from the palaeo-reservoir was finally accumulated in the weathering crust of Majiagou carbonate reservoir.

地质和地球化学分析证实，盆地西、南缘台缘深水斜坡相的中奥陶统平凉组存在优质海相烃源岩，其形成的油气最早富集在中央古隆起及其周围；伴随着中央古隆起带轴部的向东迁移和早白垩世末盆地西倾大单斜的定型，平凉组烃源岩在早白垩世生烃高峰期生成的天然气和早期古油藏裂解气，由中央古隆起带向北东方向发生二次运聚，最终在盆地中部奥陶系马家沟组风化壳中聚集成藏，即形成靖边大气田。

Tertiary basin is mainly controlled by northwestward fault and so it trends northwestward. Quaternary basin is mainly controlled by north-southward fault and so it trends noth-southward.

第三纪盆地主要受北西向断裂控制，因而呈北西向展布；第四纪盆地主要受南北向断裂控制，所以盆地呈南北向展布。

As for coseismic deformation of Chi-Chi earthquake, the footwall of Chelungpu Fault moved southeastwards 0.3-1.5 m, and the value was increasing toward the fault; the hanging wall moved northwestwards 1.4-7.0 m, but the value was smaller south of the Choshui River. After the Chi-Chi earthquake, the hanging wall of Chelungpu Fault was still moving west-northwestwards and kept uplifting, while the footwall gradually changed direction from ESE to WSW or even WNW, clockwise resuming to inter-seismic deformation pattern. It is interesting to notice that despite the largest coseismic deformation in the northernmost segment of Chelungpu Fault, the post-seismic deformation peaked around the epicenter of Chi-Chi earthquake.

集集地震之同震变形，在车笼埔断层下盘向东南方向位移0.30~1.5 m，且越靠近断层位移量越大；车笼埔断层上盘则向西北方向大幅位移约1.4~7.0 m，浊水溪以南的位移量较小；集集地震以后之震后变形型态，以车笼埔断层为分界，上盘在震后向西北西方向位移的型态仍与同震时相同，下盘由同震时一致性的向东南东方向，逐步向西北西或西南西方向位移，亦即在车笼埔断层下盘有逐步依顺时针方向回归至震间的滑移型态；另就位移速率而言，虽然同震变形最大地区在车笼埔断层北端，但其震后的变形量最大地区，却集中於震央位置附近；就地震循环而言，震后的6年期间仍处於地层压密重整阶段，尚未回归至该区震间阶段的位移状态。

The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.

南沙岩石圈新生代微板块及板内层块构造的动力演化过程，在多元动力等因素(如块体之外的欧-太-印三大板块运动边界力和地幔深部活动因素、块体内部软弱层滑面以及地球自转变化)控制下，大致经历了4个阶段的演化：从前晚白垩世的裂前活动陆-洋板块边缘阶段因太平洋俯冲带向东跃迁、原向NNW俯冲消亡的板片的拆沉、幔隆而进入晚白垩世-早始新世的隆升剥蚀、剪切伸展演化阶段，南沙超壳层块顺超壳层滑面祥东南运移、安渡-毕生与礼乐-半月基底层块沿上壳层滑面拆离，西布增生带形成；继而先后在中始新世-早渐新世期间受印-欧板块碰撞滑线场、地球自转加速影响出现西南海盆NW-SE向海底扩张和曾母前陆盆地的发育，和晚渐新世-早中新世期间南—东南向地幔流牵引造成的中央次海盆近NS向单剪伸展与海底扩张、壳体层块向南差异滑移、米里增生带形成；中中新世以来，印度-澳洲板块快速向北俯冲，构成今日南海格局。

The major deposits in the Sanzhou ore field are related to Yanshanian or later tectonic activity,which is divisible into six sequences represented by:1the Upper Triassic-Lower Jurassic low-angle normal slip fault and associated structures near or immediately occurring on the unconformity between the Lower Carboniferous and the Upper Triassic;2the longitudinally bucking fold in Devonian-Carboniferous and Upper Triassic-Lower Jurassic strata;3the earlier phase thrusts toward northwest;4the transcurrent fault toward northeast;5the later phase thrusts toward northwest;and 6the extensional normal slip minor faults.

彭少梅 ，杨坤光，姚淑梅三洲矿田内主要矿床与燕山期或更晚的构造活动有关。燕山期构造活动可分为六个序列：1下石炭统与上三叠统不整合面附近和不整合面之上的上三叠统―下侏罗统中的低角度正滑断层及伴生构造，2泥盆系―石炭系及上三叠统―下侏罗统中的纵弯褶皱，3北西向逆冲断层，4北东向平移断层，5第二次北西向逆冲断层，6伸展性正滑小断层。

The main rivers are Lechang into the county from the northeast corner, by the flow of Shaoguan Wu Gui Town rivers; originated in the northwest and the Yangshan county border Ah fork top and flows from west to east Nanshui reservoir, through the county, import Beijiang rivers of milk; originated in the north-west county and the junction of Yizhang County, Hunan Province Meng Hang Shi Dong Lu, from northwest to southeast through the Daping, bridges, Bibei, Gui Yang, head into the Wujiang River ; originated in the northern foot of the courtyard of the ant hill rock, from north to south flow through Luoyang, large cloth imported Anglo-German city of Tai Tam River.

主要河流有由乐昌流入县境东北角，经桂头镇流向韶关的武江河；发源于县境西北与阳山交界的丫叉顶，由西向东流入南水水库，穿过县城，汇入北江的乳江河；发源于县境西北面与湖南省宜章县交界的猛坑石东麓，由西北向东南经大坪、大桥、必背、桂头流入武江的杨溪河；发源于天井山北麓的蚁岩，由北向南流经洛阳、大布汇入英德市的大潭河。

A study on physical mechanism responsible for these differences reveals that the principal factor controlling the midnight-morning westward electrojet is ionospheric conductivities, while the principal factor controlling the afternoon eastward electrojet is electric field, instead of conductivities.

电动力学分析表明，在不同地方时段，控制电流的主要因素不同，因而，电流及其磁扰有不同的特点：下午—黄昏东向电集流和晨侧西向电集流组成了DP2电流体系，主要受控于磁层对流电场，反映了&驱动过程&的行为；而子夜—凌晨西向电集流是DP1电流体系的基本部分，主要受控于电导率，反映了&卸载过程&的特点。

For a big chunk of credit-card losses; the number of filings (and thus charge-off rates) would be rising again, whether

年美国个人破产法的一个改动使得破产登记急速下降，而后引起了信用卡大规模的亏损。

Eph. 4:23 And that you be renewed in the spirit of your mind

弗四23 而在你们心思的灵里得以更新