地层厚度的英文

• bed thickne
• bthi
• formation thickness
• thickness of bed
• zone thickness

• "地层"英文翻译    stratum; layer; serati; geos ...
• "厚度"英文翻译    thickness; land
• "视地层厚度" 英文翻译 :    apparent bed thickness
• "真地层厚度" 英文翻译 :    tbt
• "地层厚度增加" 英文翻译 :    expansion
• "孔隙地层厚度" 英文翻译 :    porosity thickness
• "双程地层厚度" 英文翻译 :    two-way layer thickness
• "真实地层厚度" 英文翻译 :    tst
• "层厚度" 英文翻译 :    frozen layer fraction; layer thickness; layer thinner
• "等厚线，连接相同地层厚度点的线。" 英文翻译 :    isopach
• "半值层厚度" 英文翻译 :    hvt
• "保温层厚度" 英文翻译 :    insulating layer thickness
• "边界层厚度" 英文翻译 :    boundary layer thickness
• "表层厚度" 英文翻译 :    skin thickness
• "采煤层厚度" 英文翻译 :    extracting seam thickness; working bed height
• "产层厚度" 英文翻译 :    pay thickness
• "臭氧层厚度" 英文翻译 :    ozone thickness
• "储层厚度" 英文翻译 :    reservoir thickness
• "磁层厚度" 英文翻译 :    magnetic coating thickness
• "磁涂层厚度" 英文翻译 :    magnetic coating thickness
• "叠层厚度" 英文翻译 :    lamination thickness
• "镀层厚度" 英文翻译 :    coating thickness; depth of coating; plating thickness
• "堆层厚度" 英文翻译 :    cell thickness
• "分层厚度" 英文翻译 :    lift height
• "粉刷层厚度" 英文翻译 :    depth of plastering

• Through the analysis attributes inof time and frequency zone , we can find when the thickness is less than / 4 the relationship between thickness and attribute is liner
  通过常用的时频域分析，可以看出，属性与地层厚度在调谐厚度内时近似的呈线性关系。
• Methods based on comprehensive analysis of isopaches , sadstone percentage , paleocurrent and sadstone content , a reaserch is made on the sedimentary environment of upper permian shiqianfeng formation in the southern of north china
  方法根据岩石碎屑组分基本数据，运用地层厚度、砂岩百分含量、古水流、砂岩成分的系统分析方法。
• The holocene stratum of quzhou district is quite different from other areas of hebei plain in terms of the buried depth , thickness , depletion rate , color , grain size , structure and pollen assemblages
  摘要河北平原南部曲周地区的全新世地层，在埋藏深度、地层厚度、堆积速率和颜色、粒度结构、孢粉含量与种属等方面，与河北平原其他地区不同。
• The stratigraphic analysis reveals that the upper part of kongdian formation is characterized by thickness range from 461 - 744 m and average of thickness of 602 . 5 m . the number quantity of sandstone increased to the north and northwest , indicating more sand bodied are found at these directions
  地层学分析表明南斜坡主要发育孔店组上段，地层自南向北逐渐增厚，地层厚度一般为461 - 744m ，平均厚602 . 5m 。
• The principle of this method is that we can regard the time stratum unit as three - dimension sedimentary body , when the stratum formed in a certain geological epoch , there was a definite proportion relationship between the thickness of the stratum and the thickness of the time stratum unit
  其理论依据是：等时地层单元内，由某一地质历史时期所形成地层厚度与沉积时间具有一一对应的关系，据此对某一等时界面上的沉积特征进行数字化的描述。
• Because of the work mentioned above , a new method of renewing ancient thickness is brought forward , the method of the continuing tendency of the uneroded stratum thickness , the method of the variety rate of the reference layer thickness and the method of the ratio of the contiguous layer thickness are used to renew the erosion thickness in ludong area for the first time and the method of fuzzy synthetic evaluation is used to prioritize the favorable places for prospecting for oil and gas
  在此基础之上，提出了一种恢复古厚度的新方法，并首次在陆东地区采用未被剥蚀地层厚度趋势延伸法、参考层厚度变化率法和邻层厚度比值法进行剥蚀厚度恢复，以及采用模糊综合评判方法优选出了有利的勘探目标。
• Based on the analysis of sedimentary facies in individual wells and the correlation of three cross sections of sedimentary facies , it is elaborated that sedimentary facies of jianglingjiang formation are vertically and laterally developed within qianwei area . by the method of single - factor analysis , it is pointed out facies distribution of four key formations after thorough study of four geologic factors that could embody sedimentary environment and facies , that is the thickness of formation , grainstone and dolostone , and lithofacies . with the above results , combining with reservoir and structural features , of which the emphasis is the reservoir characteristics of different rock and microfacies types , it is pointed out favorable reservoir zones , by the method of multi - factors superposition
  采用单因素分析法，选取并研究地层厚度、颗粒岩厚度、白云岩厚度和区域岩相等四种能反映沉积环境和沉积相的地质因素，指出了四个重点层段的沉积相平面分布特征；根据沉积相的研究成果，结合储层特征和构造发育特征，着重讨论了不同岩石类型和微相类型的储集特征，采用多因素叠合法对犍为地区嘉陵江组有利储集相带进行了预测，指出了有利储集相带的分布。
• Through the correlation of nww - see and sn , the thickness and limestone intervals of matuo formation gradually increase from west to east . this represent the center of sedimentation is possible located in east of the region . the matuo formation thickness gradually increase and then reduce from north to south
  通过北西西?南东尔向和南北向剖面对比，玛托组地层横向变化表现为由西往东，玛托组地层厚度逐渐加大，灰岩夹层也增多，反映当时沉积中心在研究区东部，而由北往南，厚度先逐渐增大，后减小，灰岩夹层增多，由北往南的古地理格架为滨面?碳酸盐台地?斜坡环境。
• On the basis of areal geological background , the distribution pattern of sedimentary microfacies in the chang - 6 oil - bearing beds was distinguished and the palaeogeographic environment was reconstructed by the analysis of geology facies , logging facies , stratum thickness , sandstone thickness and sandstone percent and other sedimentary characteristic . the method of digital sedimentary microfacies was applied in part of the research area for the first time , and acquired the satisfying effect . the digital sedimentary microfacies realized the description of the sedimentary evolution from chang - 62 to chang - 61
  在区域沉积背景的墓础上，结合地质相特征与测井相分析，对地层厚度、砂体厚度以及砂地比(砂岩含量)等在平面上的分布规律进行了综合分析，并结合沉积序列与沉积特征等，判别了沉积微相在平面上的分布格局，恢复出长6油层组各沉积期的古地理环境。
• On the base of fully utilizing the available data about tectonic maps and structural elements , the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis , and combined seismic - data interpretation , review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system , and combined region and location , plane and profile and time and spatial . by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin , the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift . the formation and evolution of the hetian paleo - uplift experienced three stages , that is , the uplifting and eroding stage of the caledonian period , the depositional stage of the hercynian period and the destroying stage of the himalayan period , and evolved from paleo - lift to inclining strap at last
  本文采用地质和地球物理相结合的研究思路，运用多种技术手段和方法；在充分利用已有构造图资料和构造要素资料的基础上，运用地层层序边界不整合分析法、地层厚度对比分析法，结合地震资料的精细解释、古构造和古地貌的恢复、构造演化史研究、含油气系统的研究，和区域和局部、平面和剖面、时间和空间的结合研究，对塔里木盆地和田古隆起构造演化及油气关系进行了综合分析，认为： ( 1 )和田古隆起为一沉积?剥蚀性古隆起；形成于志留-泥盆纪；其构造演化可分为三个阶段，即加里东期的抬升剥蚀阶段、海西期的沉积阶段和喜山期的破坏阶段，最终由古隆起演变为一斜坡带。