太原组的英文

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• "太原"英文翻译    Taiyuan
• "组"英文翻译    group
• "太原" 英文翻译 :    taiyuan
• "大原组" 英文翻译 :    ohara-gumi
• "原组织" 英文翻译 :    original structure; prior structure
• "太原街" 英文翻译 :    tai yuen street
• "太原郡" 英文翻译 :    taiyuan
• "太原省" 英文翻译 :    thai nguyen province
• "太原市" 英文翻译 :    taiyuan municipality; thai nguyen
• "太原统" 英文翻译 :    taiyuan series
• "太原雪" 英文翻译 :    sessai choro
• "基料；原组分" 英文翻译 :    stock blend
• "胶原组织" 英文翻译 :    collagen tissue; collagenous tissue
• "精原组织" 英文翻译 :    androgonial tissue; spermatogenous tissue
• "抗原组成" 英文翻译 :    antigenic composition
• "蓝舌抗原组" 英文翻译 :    blue tongue antigenic group
• "中原组曲" 英文翻译 :    chinese folk songs
• "孢原组织" 英文翻译 :    archespore; archesporium; archispore
• "山西太原" 英文翻译 :    taiyuan
• "太原大学" 英文翻译 :    taiyuan university
• "太原发电厂" 英文翻译 :    thai nguyen power plant
• "太原工学院" 英文翻译 :    taiyuan engineering institute
• "太原坏学院" 英文翻译 :    taiyuan mechanical engineering institute
• "太原会战" 英文翻译 :    battle of taiyuan
• "太原市爱图" 英文翻译 :    art two

• Practice and understanding in mining seams of taiyuan group
  太原组煤层开采的实践与认识
• Application of air bag support in taiyuan thin coal seam
  气垛支架在太原组薄煤层中的应用
• Coal facies analysis upon no . 16 coal seam in yanzhou coal mining area of shangdong province
  山东兖州矿区太原组16号煤层煤相研究
• Sedimentary characteristics and coal - accumulation regularitie s of taiyuan formaiton in feicheng coal field
  肥城煤田太原组沉积特征与聚煤规律
• Braided - river delta of the taiyuan formation of the upper carboniferous in the hulusitai area of inner mongolia
  内蒙葫鲁斯太上石炭统太原组辫状河三角洲沉积
• According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
  根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。
• Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
  文摘:根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。
• On the basis of realizing the sedimentary system and tectonics , the authors think the sedimentary fades of the taiyuan formation is barrier island , beach and delta facies in tabamiao area in the north of orcios basin by observing cores , analyzing lithofacies and log facies
  摘要在了解区城沉积背景的情况下，综合运用岩心观察、岩相分析、测井相分析等手段，确定鄂尔多斯盆地北部塔巴庙区块太原组为有障壁海岸沉积体系和无障壁海岸沉积体系的滨浅海相沉积与湖泊三角洲相沉积。
• According to the regional geology and the character of the lithofacies and well - logging facies , 4 kinds of sedimentary facies and 3 kinds of depositional system : marine system , delta system and fluvial system have been identified . the sedimentary facies of taiyuan formation is marine faceis , up to sanxi formation , the sedimentary facies is delta facies , the xiashihezi formation hel and he2 member are braided river facies , he3 member is meandering river facies . the mains types of sandstone of taiyuan formation are lithic quartzarenite and quartzarenite ; the mainly types of sandstone of sanxi formation and xiashihezi formation is litharenite
  通过对20余口井2000多米岩心的观察和对40几口井的测井数据解释、对比，在研究区目的层段识别出了12种基本岩相和9种测井相类型，在区域沉积背景和单井相划分的基础上，根据岩相和测井相组合特征，在太原组?下石盒子组划分出4种沉积相和若干沉积微相，并进一步划分为3类沉积体系：滨浅海沉积体系、三角洲沉积体系和河流沉积体系。