里奥 - 网络例句 - 英语人，englisher

In the furious struggle between newly established Aristotelianism and Augustinianism which insisted the tradition of Platonism, two great theologians and philosophers, Thomas Aquinas and Bonaventure presented themselves, who stood for the highest level of theology and philosophy system at that time. The former one successfully established a new philosophy system using Aristotelianism, and the latter one developed the Platonism-Augustinianism to the peak.

在新兴的亚里士多德主义与坚持柏拉图传统的奥古斯丁主义之间的激烈斗争中，产生了代表那一时代创立神学－哲学综合体系最高水平的两位伟大的神学家、哲学家，即托马斯·阿奎那和波纳文图拉，前者成功地利用亚里士多德理论建立起新的神哲学体系，后者则将柏拉图传统的奥古斯丁主义发展到顶峰。

It was the period of the conflict of the republics of South America with the King of Spain, of Bolivar against Morillo.

那正是南美洲的一些共和国和西班牙国王斗争的时期，也就是玻利瓦尔①和莫里耳奥②斗争的时期，窄边帽是保王党的标志，那种帽子就叫做莫里耳奥，自由党人戴的阔边帽子就叫做玻利瓦尔。

Cast :, Ben Chaplin as George Coulouris , Claire Danes as Sonja Jones , Zac Efron as Richard Samuels , Zoe Kazan as Gretta Alder , Eddie Marsan as John Houseman , Christian McKay as Orson Welles , Kelly Reilly as Muriel Brassler , James Tupper as Joseph Cotten rest of expel listed alphabetically:, Thomas Arnold as George Duthie, Leo Bill as Norman Lloyd, Shane James Bordas as Elliott Reid, Michael Brandon as Les Tremayne, Aaron Brown as Longchamps Child, Janie Dee as Mrs .

演员：，班卓别林乔治Coulouris，克莱尔丹尼斯的宋雅琼斯，醋氨己酸锌埃弗龙的理查德塞缪尔斯，佐伊喀山的Gretta桤木，艾迪玛珊作为奥森韦尔斯，凯利赖利约翰豪斯曼，基督教麦凯的穆里尔Brassler，詹姆斯约瑟夫科顿的其余部分按字母顺序列出驱逐百乐：托马斯阿诺德乔治达西，狮子条例草案诺曼劳埃德，巴蒂尔詹姆斯博尔达斯在Les Tremayne，阿龙的隆尚儿童，珍妮迪布朗的埃利奥特里德，迈克尔布兰登正如刚才。

The roster of composers and conductors who have led the Philharmonic includes such historic figures as Theodore Thomas, Pyotr Ilyich Tchaikovsky, Antonín Dvoák, Gustav Mahler (Music Director, 1909–11), Otto Klemperer, Richard Strauss, Willem Mengelberg (Music Director, 1922–30), Wilhelm Furtwngler, Arturo Toscanini (Music Director, 1928–36), Igor Stravinsky, Aaron Copland, Bruno Walter (Music Advisor, 1947–49), Dimitri Mitropoulos (Music Director, 1949–58), Klaus Tennstedt, George Szell (Music Advisor, 1969–70), and Erich Leinsdorf.

曾与乐团合作过的史上著名作曲家和指挥包括：西奥多托马斯、柴科夫斯基、德沃夏克、马勒、奥托克伦佩勒、理查施特劳斯、威廉孟高贝格、富尔特文格勒、托斯卡尼尼、斯特拉文斯基、科普兰、布鲁诺瓦尔特、迪米特里米特罗普洛斯、克劳斯腾斯泰德、乔治塞尔、埃里克雷恩斯朵夫。

Napoleon: The First Emperor of France, has undergone seven Coalition, the campaign Lvjun Italy, Austria, Putin, Russia, the West and other countries, has experienced Marengo, Ulm, Teli Ci oris, Leipzig, Waterloo, such as war, lost his life more than a small victory, the European Mingzhen, so that the sovereign countries shudder.

拿破仑：法兰西第一帝国皇帝，先后经历了七次反法同盟，率军征战意、奥、普、俄、西等国，经历了马伦哥、乌尔姆、奥里斯特里茨、莱比锡、滑铁卢等战，一生胜多败少，名震欧陆，让各国君主不寒而栗。

Mario Balotelli is unhappy at Inter because of Jose Mourinho, according to his agent Mino Raiola.

经纪人拉伊奥拉称：巴罗特里在国米和穆里尼奥有矛盾，他在国米不开心

It is overall a monoclinal structure dipping to south, on which three group faulted structures with the directions of E-W, NEE, and NE-SW are developed, and they are tensional faults. The Orinoco heavy oil belt has been divided into two tectonic zones by one regional fault with the trend of NE in the plane, and the characteristics are different in the two tectonic zones.

奥里诺科重油带是目前世界上唯一一个还基本未开发的大规模重油富集带，它位于东委内瑞拉盆地边缘隆起带，总体是一北倾单斜，其上主要发育E-W向、NEE向和NE-SW向三组断裂，且以张性断裂为主，其中有一条北东向区域性大断裂将奥里诺科重油带在平面上划分为两大构造区，其各自的构造特征不同。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究，精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现，把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带；初步确定该区的变质作用属于中温-低压型，变质作用发生的时代为290Ma左右，是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原"居里得能组"岩屑砂岩的碎屑锆石SHRIMP U-Pb定年，确认这套地层的沉积不早于晚泥盆世，很可能是石炭纪，而不是前人所说的前寒武纪；结合对其区域地质背景、源区位置和沉积环境分析，推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料，结合该区已有相关资料的综合研究，确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪，不存在泥盆纪的岩浆岩，进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料，把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%，相应的地壳缩短量分别为4.3km、9km和11.3km。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究，精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现，把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带；初步确定该区的变质作用属于中温-低压型，变质作用发生的时代为290Ma左右，是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原&居里得能组&岩屑砂岩的碎屑锆石SHRIMP U-Pb定年，确认这套地层的沉积不早于晚泥盆世，很可能是石炭纪，而不是前人所说的前寒武纪；结合对其区域地质背景、源区位置和沉积环境分析，推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料，结合该区已有相关资料的综合研究，确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪，不存在泥盆纪的岩浆岩，进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料，把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%，相应的地壳缩短量分别为4.3km、9km和11.3km。

The Mishnah is extant in many editions, although only the earlier ones can be mentioned here: first edition, Naples, 1492, fol., with the Hebrew commentary of Maimonides; Venice, Justiniani, 1546-50, fol.; Venice, 1549, 4to, with the commentary of Obadiah Bertinoro; Riva di Trento, 1559, fol., with the commentaries of Maimonides and Obadiah; Sabbionetta and Mantua, 1559-63, 4to; Venice, 1606, fol., with the same two commentaries.

该米示拿是现存的许多版本，但只有以前的可以在这里提及：第一版，那不勒斯， 1492年，奥德耶克。与希伯来文评迈蒙尼德；威尼斯， Justiniani ， 1546年至1550年，奥德耶克。；威尼斯， 1549年， 4to ，以评俄巴底亚Bertinoro ；里瓦娣特伦托， 1559奥德耶克。与评论迈蒙尼德和俄巴底亚； Sabbionetta和曼图亚， 1559年至1563年， 4to ；威尼斯， 1606年，奥德耶克。，同两评注。