内尔哈 - 网络例句 - 英语人，englisher

Chris Bangle, Director of Design, BMW Group Peter Barna, Provost, Pratt Institute Yves Behar, Founder, fuseproject Katherine Bennett, IDSA Education Vice-President, and Professor of Product Design, Art Center College of Design Mark Breitenberg, Dean of Undergraduate Education, Art Center College of Design, and Chair of the Education Committee, International Council of Societies of Industrial Design Heather Fraser, Director, Business Design Initiative, Rotman School of Management, University of Toronto Tamara Giltsoff, Live | Work Walter Herbst, Director, Master of Product Development Program, McCormick School of Engineering and Applied Science, and Professor of Marketing, Kellogg School of Management, Northwestern University Barry Jaruzelski, Vice-President, Innovation Practice, Booz Allen Hamilton Chuck Jones, Vice-President, Global Consumer Design, Whirlpool Lorraine Justice, Professor and Head of Hong Kong Polytechnic University, School of Design Larry Keeley, President, Doblin Inc. David Kelley, Founder of IDEO, and Co-founder of Stanford s Hasso Plattner Institute of Design Claus Knapheide, Director of User Experience, Siemens Mick Malisic, Director of Marketing, Frog Design Brian Matt, Founder, CEO, Altitude Dev Patnaik, Founder, Jump Associates Ravi Sawhney, CEO-President, RKS Design Jeff Semenchuk, EVP, Global Consumer Group Innovation, Citigroup RitaSue Siegel, President, RitaSue Siegel Resources Bob Sutton, Professor of Management Science and Engineering, and Co-founder of Stanford s Hasso Plattner Institute of Design Sohrab Vossoughi, President, ZIBA Design Patrick Whitney, Director, Institute of Design, Illinois Institute of Technology Gianfranco Zaccai, President and CEO, Continuum

克里斯手镯，设计，宝马集团董事彼得巴纳，教务长，普拉特学院伊夫贝哈尔，方正，fuseproject 凯瑟琳贝内特，IDSA的教育副总统，以及产品设计，艺术中心设计学院教授马克布赖滕贝格，本科教育，艺术中心设计学院，以及教育委员会，国际工业设计协会理事会主席迪安石南弗雷泽，主任，业务设计倡议，罗特曼管理，多伦多大学塔玛拉Giltsoff，直播|工作沃尔特赫布斯特，主任，产品开发计划，麦考密克工程和应用科学学院硕士，以及市场营销，Kellogg管理，西北大学法学院教授巴里雅鲁泽尔斯基，副总统，创新实践，博思艾伦查琼斯，副总裁，全球消费者设计，惠而浦洛林司法，教授和香港理工大学校长，设计学院拉里开利，总裁，德布林公司大卫凯利，IDEO的创始人兼联合创始人斯坦福虏哈索普拉特纳设计学院克劳斯Knapheide，用户体验，西门子公司董事米克马利希奇，市场营销，青蛙设计总监布赖恩马特，创始人，CEO，海拔 dev的帕特奈克，方正，跳转协会拉维梭尼，首席执行官，总裁，设计可胜杰夫谢缅丘克，执行副总裁，全球消费者集团创新，花旗集团 RitaSue西格尔先生，RitaSue西格尔资源鲍勃萨顿，管理科学与工程学院教授，兼联合创始人斯坦福虏哈索普拉特纳设计学院苏赫拉布Vossoughi，总统，Ziba设计帕特里克惠特尼主任，设计，伊利诺斯技术研究所詹弗兰科扎卡伊，总裁兼首席执行官，连续

In term of techniques and skills: Ronaldo is the best player since Maradona (in the lot of Basten, Baggio, Romario, Stoitchkov, Hagi, Weah, Laudrup, Zidane, Bergkamp, Rivaldo Figo Nedved Raul Henry Ronaldinho and lately Kaka, Messi C.Ronaldo).

-在长期的技术和技能：罗纳尔多是最优秀的球员，因为马拉多纳（在很多巴斯滕，巴乔，罗马里奥，奇科夫，哈吉，维阿，劳德鲁普，齐达内，博格坎普，里瓦尔多，菲戈，内德维德劳尔亨利最近卡卡和罗纳尔迪尼奥，梅西角罗纳尔多）。

Midfielders: Osvaldo Ardiles Ademir Didi Roberto Rivelino Gerson Falcao Clodoaldo Zico Enzo Francescoli Paul Gascoigne Michel Platini Lothar Matthaus (W Germany/Germany) Wolfgang Overath Bobby Charlton Johan Neeskens Frank Rijkaard Ruud Gullit Johnny Rep Rene van der Kerkhof Wim Van Hanegem Grzegorz Lato Gheorghe Hagi Enzo Scifo Dragan Dzajic Nils Liedholm Teofilo Cubillas Michael Laudrup Josef Masopust Carlos Valderrama Junich Inamoto.

中场：阿迪莱斯，阿德米尔、迪迪、利维里尼、贾尔森、法尔考、克罗多亚尔队储济科，弗朗西斯科利，加斯科茵、博比·查尔顿，普拉蒂尼，马特乌斯、奥弗拉特，内斯肯斯、里杰卡尔德、古力特、约翰尼·雷普、范德科克霍夫、范哈内亨，拉托，哈吉，希福，德拉甘·德扎季奇，利德霍尔姆，库比拉斯，迈克尔·劳德鲁普，，巴尔德拉马，稻本润一日本

Midfielders: Osvaldo Ardiles, Ademir, Didi, Roberto Rivelino, Gerson, Falcao, Clodoaldo, Zico, Enzo Francescoli, Paul Gascoigne, Michel Platini, Lothar Matthaus (W Germany/Germany), Wolfgang Overath, Bobby Charlton, Johan Neeskens, Frank Rijkaard, Ruud Gullit, Johnny Rep, Rene van der Kerkhof, Wim Van Hanegem, Grzegorz Lato, Gheorghe Hagi, Enzo Scifo, Dragan Dzajic, Nils Liedholm, Teofilo Cubillas, Michael Laudrup, Josef Masopust, Carlos Valderrama, Junich Inamoto.

中场：阿迪莱斯，阿德米尔、迪迪、利维里尼、贾尔森、法尔考、克罗多亚尔多、济科，弗朗西斯科利，加斯科因、博比·查尔顿，普拉蒂尼，马特乌斯、奥弗拉特，内斯肯斯、里杰卡尔德、古力特、约翰尼·雷普、范德科克霍夫、范哈内亨，拉托，哈吉，希福，德拉甘·德扎季奇，利德霍尔姆，库比拉斯，迈克尔·劳德鲁普，，巴尔德拉马，稻本润一日本

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 number of CD〓 and CD〓 lymphocytes subpopulation, ANAE〓 T cells and IgG, IgM, IgA antibody-producing cells in the local immune tissues (cecal tonsils and Harderian glands), the content of IgA, lgM, IgG in the local fluid (tear, tracheal fluid, intestinal fluid and bile) of chicks infected with CIAV were significantly decreased compared with controls 7～28 days PI.

1日龄雏鸡感染CIAV后28天内，哈德尔腺和盲肠扁桃体的ANAE〓及CD〓、CD〓T细胞和IgA、IgM、IgG抗体生成细胞数量以及泪液、气管液、肠液、胆汁的IgA、IgM、IgG含量均明显低于对照雏鸡，表明CIAV感染雏鸡后，其呼吸道和消化道局部粘膜的细胞免疫和体液免疫机能均下降，这与CIAV感染雏鸡对其它某些病原易感性提高密切相关。

Philipp Lenard even claimed that the massenergy equivalence formula of Einstein should be credited to Friedrich Hasenohrl if it had to made an Aryan creation.

菲利普。莱纳德甚至宣称，如果爱因斯坦的质能当量公式确实创造了一个雅利安时代，那也应归功于弗里德里希。哈泽内尔。

Midfielders: Osvaldo Ardiles, Ademir, Didi, Roberto Rivelino, Gerson, Falcao, Clodoaldo, Zico, Enzo Francescoli, Paul Gascoigne, Michel Platini, Lothar Matthaus (W Germany/Germany), Wolfgang Overath, Bobby Charlton, Johan Neeskens, Frank Rijkaard, Ruud Gullit, Johnny Rep, Rene van der Kerkhof, Wim Van Hanegem, Grzegorz Lato, Gheorghe Hagi, Enzo Scifo, Dragan Dzajic, Nils Liedholm, Teofilo Cubillas, Michael Laudrup, Josef Masopust, Carlos Valderrama, Junich Inamoto.

中场：阿迪莱斯，阿德米尔、迪迪、利维里尼、贾尔森、法尔考、克罗多亚尔多、济科，弗朗西斯科利，加斯科因、博比·查尔顿，普拉蒂尼，马特乌斯、奥弗拉特，内斯肯斯、里杰卡尔德、古力特、约翰尼·雷普、范德科克霍夫、范哈内亨，拉托，哈吉，希福，德拉甘·德扎季奇，利德霍尔姆，库比拉斯，迈克尔·劳德鲁普，，巴尔德拉马，稻本润一

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。

In 1991 she founded Irma Boom Office, which works nationally and internationally in both the cultural and commercial sectors. Clients include the Rijksmuseum Amsterdam, Paul Fentener van Vlissingen (1941-2006), Inside Outside, Museum, Boijmans Van Beuningen, Zumtobel, Ferrari, Vitra International, NAi Publishers, United Nations and OMA/Rem Koolhaas, Koninklijke Tichelaar, and Camper.

她的客户有阿姆斯特丹市立美术馆、保罗·范特内尔·弗利辛根(1941-2006)，内外、波伊曼·凡·布宁根博物馆、克劳斯亲王基金会、奥地利Zumtobel 集团、法拉利、维特拉国际集团、NAi Publishers 出版社、美国、OMA/瑞姆·库哈斯、Koninklijke Tichelaar Makkum、日内瓦阿加汗基金会；西班牙看步集团、马略卡、纽约现代艺术博物馆、伦敦耶鲁报、纽约Bard Graduate Centre。