沉积结构的英文

• depositional fabric
• depositional texture
• depositionalfabric
• sedimentary texture

• "沉积"英文翻译    deposit; sedimentation; depo ...
• "结构"英文翻译    structure; composition; cons ...
• "沉积结构面" 英文翻译 :    sedimentary discontinuity
• "外沉积结构" 英文翻译 :    extrnal sedimentary texture
• "无规沉积结构" 英文翻译 :    random depositional texture
• "无序沉积结构" 英文翻译 :    random depositional texture
• "沉积结垢" 英文翻译 :    deposit
• "沉积结晶的" 英文翻译 :    epicrystalline
• "堆积结构" 英文翻译 :    cumulate texture
• "密堆积结构" 英文翻译 :    close-packed structure
• "紧密堆积结构" 英文翻译 :    close packed structure
• "六角密积结构" 英文翻译 :    hexagonal close packed structure
• "斜交前积结构" 英文翻译 :    oblique progradation configuration
• "正交堆积结构" 英文翻译 :    crescumulate texture
• "六方紧密堆积结构" 英文翻译 :    hexagonal close-packed structure
• "六角密堆积结构" 英文翻译 :    hexagonal close-packed structure
• "拓扑密堆积结构" 英文翻译 :    topologically close packed structures
• "最紧密堆积结构" 英文翻译 :    closestpacked structure
• "六方最紧密堆积结构" 英文翻译 :    hexagonal close-packed structure
• "沉积床结构" 英文翻译 :    sedimentary structure
• "隐晶结构(沉积岩)" 英文翻译 :    aphanocrystalling texture
• "累积结余" 英文翻译 :    accumulated value
• "里实积结" 英文翻译 :    interior excess due to accumulation of pathogens
• "皮壳积结" 英文翻译 :    crustification
• "容积结晶度" 英文翻译 :    volume crystallinity

• Sediment microfacies , micro - construction , the variation iri sandbody rhythm and structures , and micro - pore configuration non - uniformity are main factors that affect or control the forming of remaining oil and its distribution in different scale reservoir rock
  沉积微相、微构造的变化、砂体不同韵律性及沉积结构的变化、以及微观孔隙系统的非均质性等是控制和影响不同规模储层中剩余油形成和分布的重要因素。
• The fluvial , delta , and lacustrine sedimentary system was realized according to the analysis of the fossils , sedimentary structure , sedimentary cycle , rhythmic bedding and other criteria in the yanchang formation . the sedimentary microfacies of the chang - 6 oil - bearing beds was identified through its fine description , and the evolution of palaeogeography was revealed
  通过古生物、沉积结构与构造、沉积韵律、沉积厚度与沉积旋回特征和测井相分析等，在延长组中识别出河流、三角洲、湖泊沉积体系，以及长6油层组的沉积微相，并对长6油层组各小层的沉积微相进行了精细描述，反演出其古地理的演化历程。
• The occurrence ofland crack is the results of the asymmetry land subsidence . therefore , application the 3stechnology in studying these problems is a realistic and tough matter for expertise . recently gis as a newly - developed technology for dealing and storing spatialinformation has been wildly used in a various fields , geology field without exception
  论文重点研究了arcgis平台下基岩构造模型、第四纪沉积结构模型、地下水含水系统结构模型的三维可视化实现方法,并利用comgis在通用开发环境下嵌入了gis功能;在ao的二次开发研究中,利用activex技术实现了3s数据信息在arcgis环境中的无缝结合。
• 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。
• Based on the direction of sources and the ratios of sandstone to formation of sedimentary rocks , together with the sedimentary structures and textures , paleocurrent direction and the characteristics of paleontology , etc . , the planimetric maps of sedimentary facies of each stages in the studied area are compiled in order to recognized the extension of dominant facies and the evlotionary history of sedimentary environment , hi the stage of benxi and taiyuan , lagoon - tidal flat sediments are widespread in the area , and the deposits of estuary , lagoon and small delta in the northwest margin of ordos
  以物源方向和沉积岩砂地比值为基础，结合沉积结构构造、古水流方向及古生物特征等，编制了研究区各期次的沉积相平面图，以识别优势相展布和沉积环境演化。本溪期和太原期研究区泻湖?潮坪沉积分布广泛，西北缘发育河口湾、泻湖及小型三角洲沉积。
• The sediments of the incised valleys show an upward - fining succession , and can be grouped into four sedimentary fades : gravel lag - deposit of in - channel to partly over bank sediments of a meandering river , flood plain - estuary , estuary - shallow marine , and estuary sand bar , based on lithology , paleontology , and sedimentary textures and structures
  根据岩石学、沉积结构和沉积构造特征，本区下切河谷充填沉积物具有向上变细的沉积层序，可以划分为4个沉积相类型：河床滞留沉积物到部分曲流河沉积体系的边滩沉积、河漫滩河口湾沉积、河口湾浅海沉积和河口湾砂坝沉积。
• 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。
• O curve of dsdp607 v30 - 97 show that loess began to deposit on the terrace of the yellow river about 1 . 20 ma b p , and passed thirteen climatic changes from drier and cooler to warmer and wetter later . the turn of sedimentation from alluvium to loess , an event of transformation from accumulation to down - cut of the yellow river , indicates a sharp tectonic uplift occurred around 1 . 2 ma b p . key words : loess - paleosol ; susceptibility ; climatic changes ; tectonic movement ; yellow river ; yangfan section
  通过对杨范剖面黄土地层岩性特征沉积结构质量磁化率和频率磁化率的分析及与深海氧同位素曲线的对比，划分了剖面地层，初步确定了黄土沉积始于1 . 20 ma b p ,黄土沉积以来该区发生了13次大的干冷暖湿气候变化沉积转型指示河流强烈加积转变为河流侵蚀，代表约在1 . 20 ma b p发生过一次强烈的构造抬升事件。