carbonate platform造句

• In places on crationic edges, giant carbonate platforms may develop .
  在克拉通（稳定地块）边缘的某些地区，可发现巨大的碳酸盐台地。
• The northeastern sichuan area is evaporative carbonate platform
  在川东北地区演化为碳酸盐蒸发台地。
• Sedimentary facies of evaporative carbonate platform of the feixianguan formation of lower triassic in northeastern sichuan basin
  四川盆地东北部下三叠统飞仙关组碳酸盐蒸发台地沉积相
• The feixianguan formation of evaporative carbonate platform is a set of sulfate - bearing evaporative tidal sediments with aboundant dolomite
  飞仙关组蒸发台地为一套含硫酸盐的富白云岩的蒸发潮坪沉积层系。
• The reservoirs mainly exist in the oolitic bank facies in the carbonate platforms , which were deposited in high energy environment and mainly controlled by tidal action
  其沉积相属碳酸盐台地的鲕粒滩相，为台地潮下较高能环境沉积，主要受潮汐作用的控制。
• There are four principal palaeogeographic units in the late sinian in the middle yangtze region , i . e . carbonate tidal flat , open carbonate platform , platform - margin slopes and a basin in the south
  由于地壳差异性升降运动，晚震旦世陡山沱期岩相古地理格局发生了急剧变化。
• Important gas - bearing reservoirs included sand bodies of distributary channels and subaquatic distributary channels in deltas and braided deltas , dolomitite in carbonate platform , and sand bodies in tidal flat and barrier island
  重要的储集层有：三角洲和辫状河三角洲分流河道和水下分流河道砂体、碳酸盐岩台地的白云岩以及潮坪、障壁岛砂体。
• The land disappeared during the late canglangpu age and longwangmiao age ( early cambrian ) and the framework of palaeogeography consisted of tidal flat , open carbonate platform , platform - margin slopes and basin in the south
  早寒蝉寒武世中晚期岩相古地理格局由碳酸盐潮坪、开阔台地、台缘斜坡和台缘盆地组成，该地区主体进入碳酸盐台地演化阶段。
• The main sedimentary facies of the upper carboniferous on the margin of the xuefeng anicient land can be divided into submarine alluvial , foreshore siliciclastic , shallow beach carbonate , carbonate platform and backshore restrict carbonate facies
  摘要湖南沅陵雪峰古陆边缘上石炭统主要包括下列岩相类型：冲积扇砂砾岩相、前滨海滩砂岩相、浅滩碳酸盐相及混积岩相、潮下碳酸盐岩相及滩后局限碳酸盐岩相。
• Based on the detailed research on the sedimentary rocks of northwest ordos basin in their textures , structures , vertical sequences and logging response , six kinds of sedimentary facies can be recognized in this work , i . e . , alluvial fan , stream , fan delta , braided delta , delta , lake , barrier beach and carbonate platform , respectively , and more detailed classification of sedimentary subfacies and microfacies for each sedimentary facies are also made in the work
  本文通过对鄂尔多斯盆地西北部沉积岩沉积结构、沉积构造、垂向序列及测井响应的深入研究，识别出冲积扇、河流、扇三角洲、辫状河三角洲、曲流河三角洲、湖泊、障壁海岸及碳酸盐台地等8种沉积相类型。在此基础上，对每一种沉积相又进行了详细的沉积亚相和微相的划分。
• 2 . the new idea about classification of oil and gas accumulation unit for exploration have been put forward , which holds the sound basis for the perpendicular and plane position and prediction of carbonate reservoir in feixianguan guan group . 3 . the depositional systems of feixianguanguan group in taphrogenic consist of carbonate platform facies ( include oolitic bar , oolitic beach , lagoon , flats ) , margin shelf and trough . there are five development staged in taphrogenic trough
  3 、指出裂陷槽中飞仙关组沉积体系在平面上由碳酸盐岩台地相(包括滩坝相、鲕滩相、泻湖相、潮坪相) 、陆棚相、裂陷槽相组成，裂陷槽经历了发生期、发展期、稳定期、过渡期及衰亡期五大发展演化阶段，每一阶段各发育不同的沉积相，且以一种沉积相为主。
• The transitional facies can also be divided as estuarine , tidal flat and lagoon ; the depositional envirnononents of clastic rock marine facies include offshore , shallow water continental shelf , deep water continental shelf , slop as well as the deep water basin ; the carbonate facies can also be divided into a carbonate platform and ramp
  海陆过渡相又分为河口湾、潮坪、泻湖；海相碎屑岩沉积环境包括滨海、浅水陆棚、深水陆棚、斜坡以及深水盆地；碳酸盐岩海相又可分为碳酸盐台地、碳酸盐缓坡。
• By use of new theory , views and methods of modern sedimentology and through the analasis of core , well logging and log data of approximately twenty well in manxi area , six kinds of sedimentary facies such as wave - dominated littoral , tide - dominated littoral , mixing littoral , shallow marine r shelf , carbonate platform facies and others are recognized and elaborated
  运用现代沉积学的新理论、新观点与新方法，通过对满西地区20余口井岩芯、录井和测井资料的分析，识别并阐述区内石炭系浪控滨岸、潮控滨岸、混积滨岸、浅海陆棚和碳酸盐岩台地等六种沉积相。
• Based on the synthetic research of field outcrops , drilling section , well log and office compilation , combined with analyses of geological background , lithological association , sedimentary texture , sedimentary structure , geochemical and palaeobiological features , the researched area in the palaeozoic can be divided into deltas , braided deltas , lacus , barrier coast , continental shelf and carbonate platform etc . six kinds of sedimentary facies
  在野外露头、钻井剖面及测井曲线的综合研究和室内编图基础上，综合地质背景、岩性组合、沉积结构、沉积构造、地球化学及古生物学特征，研究区古生界被划分为三角洲、辫状河三角洲、湖泊、障壁海岸、陆棚及碳酸盐台地等6种沉积相类型。
• The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous
  古地理分析表明，研究区晚三叠世古地理轮廓是一个从东南向西北和东北方向由浅水碳酸盐台地及深水陆层海底扇沉积共同发育的沉积盆地；早中侏罗世，演变成为一个由深水砂质浊积岩和细屑浊积岩组成的水下席状体沉积；进入中晚侏罗世，其古地理表现为一个陆屑浅海有障壁海岸；到了晚白垩世，研究区表现为以含煤沉积为特征的三角洲相沉积。