陆表海的英文

• continental sea
• eperic sea

• "陆"英文翻译    land
• "表"英文翻译    outside; surface; external
• "陆表海沉积" 英文翻译 :    epicontinental deposit
• "陆表海域" 英文翻译 :    epicontinental marine domain
• "陆表海 内海 内陆海" 英文翻译 :    continentalsea
• "陆表海沉积作用" 英文翻译 :    epicontinental sedimentation
• "陆表的" 英文翻译 :    epicontinental
• "陆表相" 英文翻译 :    epicontinental facies
• "表海他西林" 英文翻译 :    epihetacillin
• "陆表地槽" 英文翻译 :    epigeosyncline
• "陆表盆地" 英文翻译 :    epicontinental basin
• "陆表浅海相" 英文翻译 :    epicontinental neritic facies
• "表海面层群落" 英文翻译 :    epipelagic community
• "陆标交叉方位" 英文翻译 :    terrestrial cross bearings
• "陆标定位时多观测一个方位以供核对" 英文翻译 :    bearing for check
• "陆标定位法" 英文翻译 :    fixing by landmarks; position by terrestrial observation

• In the taiyuan stage of the early permian , north china sea is connected with qilian sea to form uniform epicontinental sea deposit
  早二叠世太原期，华北海与祁连海贯通，形成统一陆表海沉积阶段。
• Started from benxi stage of late carboniferous , deposits of epiric sea were developed in this area along with the spreading of west - east direction and gentle depression of the basement
  从晚石炭世本溪期开始，由于东西向拉张，基底缓慢下沉，本区广泛发育陆表海沉积。
• Calculation of transition probability matrix and fixed vector of the well profiles in the area shows , from a quantitative point of view , the vertical evolution law of the sedimentary series and the transversal environmental difference
  通过多步转移概率矩阵和固定向量计算，从定量的角度说明了研究区内部分钻井剖面陆表海沉积在垂向上演化的规律性及反映在横向上的古环境差异性。
• It is considered that the sequence evolution in the palaeozoic went through the following three stages , the filling of evaporate platform , the filling of carbonate and detrital rock mixed deposits in epiric sea , and the filling of detrital deposits of lake - deltas in paralic inland sag
  认为研宄区古生界层序演化经历了以下三个阶段：蒸发台地充填阶段、陆表海碳酸盐岩与碎屑岩混合沉积阶段，以及近岸内陆坳陷的湖泊三角洲碎屑岩沉积阶段。
• 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。
• The sedimentary formation can be summarized as rift bay filling sequence , epicontinental sea filling sequence , offshore debris lake basin sequence and inner continental lake basin sequence . a framework of sequence stratigraphy for the upper palaeozic strata is established in the area . the helan aulacogen of upper carboniferous in the west margin of ordos can be divided into 12 sequences , and most of the upper palaeozoic strata in the area can be divided into 15 sequences
  本文对研究区内上古生界进行了层序地层学探讨，将本区沉积建造概括为裂陷海湾充填层序、陆表海充填层序、近岸碎屑湖盆层序和内陆湖盆层序，建立了研究区上古生界层序地层学格架，西缘贺兰拗拉槽上石炭统划分为12个层序，本区大部分地区上古生界可划分出15个层序，并全面地概括了层序演化各阶段的具体特征。
• So it had the long distance controlling effect on the sediment in the ordos . it is generally supposed that on the ramp of cratonic basin , the sequence of the epicontinental sea in the ordos is mainly composed of the transgressive system tract and the high stand system tract . this paper shows that it is possible that the incised valley of the low stand system tract can exist on the continental shelf in the basin
  鄂尔多斯地区上古生界具有克拉通盆地陆表海缓坡沉积的一般特征，层序构成一般以海侵和高位体系域为主，本次研究认为在陆表海沉积背景下，除在大陆边缘附近，在盆地内古大陆架上也可以发育低位体系域的下切河谷充填沉积。