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Counties or Shires: Avon, Bedfordshire, Berkshire, Buckinghamshire, Cambridgesshire, Cheshire, Cleveland, Cornwall, Cumbria, Derbyshire, Devon, Dorset, Durham,, Essex, Gloucestershire, Hampshire, Hereford and Worcester, Hertfordshire, Humberside (N.Humberside), Kent, Lancashire, Leicestershire, Lincolnshire, Norfolk, Northamptonshire, Northumberland, Nottinghamshiire, Oxfordshire, Shropshire, Somerset, Staffordshire, Suffolk, Surrey (Kingston-upon-Thames), East Sussex, West Sussex, Warwickshire, Isle of Wight, Wiltshire, North Yorkshire, Clwyd, Dyfed, Gwent, Gwynedd, Mid Glamorgan, Powys, South Glamorgan, West Glamorgan, Borders, Central, Dumfries and Galloway, Fife,Grampian, Highland, Lothian, Strathclyde, Tayside, Western Isles, Orkney, Shetland, Antrim, Ards, Armagh, Ballymoney, Belfast, Carrickfergus, Castlereagh, Coleraine Cookstown, Craigavon, Down, Dungannon, Fermanagh, Larne, Limavady, Lisburn Londonderry, Magherafelt, Moyle, Newtownabbey, Newry and Mourne, North Down, Omagh, Strabane, Northern lreland and Ballymena.

郡:埃文、贝德福、伯克、白金汉、剑桥、柴、克利夫兰、康沃尔、坎布亚、德比、德文、多塞特、达勒姆、埃塞克斯、格罗斯特、汉普、赫福德-伍斯特、哈福德、亨伯塞德、肯特、兰开夏、莱斯特、林肯、诺福克、北安普敦、诺森伯兰、诺丁汉、牛津、什罗普什鲁斯伯)、萨默塞特、斯塔福德、萨福克、萨、东塞萨克斯、西塞萨克斯、沃克、怀特岛、威尔特、北约克(诺萨勒顿、克卢伊德、达费德、格温特、圭内斯、中格拉摩根、波伊斯、南格拉摩根、西格拉摩根、博德斯、中部大区、邓弗斯-盖洛韦、法夫、格兰扁、苏格兰高地、洛锡安、斯特拉斯克莱德、泰赛德、西部群岛、奥克尼群岛、设德兰群岛、安特姆、阿兹、阿尔马、巴利马尼、贝尔法斯特、卡克弗格斯、卡斯尔雷、科尔雷恩、库克敦、克雷加文、唐、邓甘嫩、弗马纳、拉恩、利马瓦迪、利斯本、伦敦德、马拉费尔特、莫勒、纽敦阿比、纽和莫恩、北部丘陵、奥马区、斯特拉斑、北爱尔兰和巴利米纳。

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、首次提出哈尔克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔克山南麓原"居得能组"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、首次提出哈尔克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔克山南麓原&居得能组&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。

Baily's beads 倍里珠 An effect occurring just before second contact or just after third contact of a total solar eclipse, when the Moon's irregular surface makes sunlight appear as beads at certain parts of the disk.

日全食中第二次接触前或第三次接触后发生的现象。当月球凹凸不平的表面几乎完全覆盖太阳时,部份太阳光会被月球凸出的地方分割开,看起来就像一颗颗圆珠般,是为倍珠。

Police are investigating a love米尔斯特里姆Renewable Energy Co., Ltd. based in the southwestern counties of Carlow, a feed processing plant.

爱警方正调查米尔斯特姆能源再生有限公司设在西南部卡洛郡的一家饲料加工厂。

In earlier studies his research team have noted a remarkable absence of cardiovascular disease and diabetes among the traditional population of Kitava, Trobriand Islands,特罗布里恩群岛 Papua(巴布亚岛 New Guinea, where modern agrarian-based food is unavailable.

他带领的研究小组在早期的研究中就注意到新几内亚巴布亚岛和特罗布恩群岛的卡塔瓦民族没有人患心血管疾病和糖尿病。而这两个地区没有耕地为主的食物。

The fourth day in Teneriffa 特纳里夫之行的第四天 Today the weather was quite nice, we decided to hike on the highest mountain in Spain, Volcano Teide (3718m).

今天天气特别好,我们决定去西班牙最高峰,即位于特纳夫海岛中部的海拔3718米的泰德火山进行徒步之旅。

November 16, 1904, a group of Argentine seamen boarded the South Georgia Island; January 1, 1905, they格里特维肯in Hong Kong to set up a weather station. July 4, 1908, the United Kingdom announced to the south of 50 degrees south latitude, 80 degrees West Drive to the east of the majority of the region, including the Falklands, South Georgia Islands and the South Sandwich Islands, South Shetland Islands, Argentina St. Cruz, a province, the southern provinces of Chile, Tierra del Fuego as a whole, and so on, are areas of British rule.

南乔治亚群岛由此得名。1904年11月16日,一批阿根廷海员登上南乔治亚岛;1905年1月1日,他们在格特维肯港设立了一个气象站。1908年7月4日,英国宣布,南纬50度以南、西径80度以东的广大区域,包括马岛、南乔治亚群岛、南桑德韦奇群岛、南设得兰群岛、阿根廷的圣克鲁斯省一部、智利南方各省、整个火地岛等,均为英国统治区。

Buddha is里斯兰north coast, a Germanic tribe, the descendants of people.

斯兰人是北海岸的一个日尔曼人部落的后裔。

Lloyd Nicolson,布里斯托尔(I'm a chartered physio at Bristol City and we had a young lad with aninjury almost identical to your own.

我是布斯托尔的一位特许理疗师。我们以前治疗过一个和你病情相似的小伙子,他是2009年9月最后一周受的伤。

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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。

Chapter Three: Type classification of DE structure in Sino-Tibetan languages.

第三章汉藏语&的&字结构的类型划分。