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1)  sedimentary facies feature
沉积相特征
2)  sedimentary characteristics
沉积特征
1.
Reservoir sedimentary characteristics and heterogeneity of block Cao 4,member 4 of Shahejie formation in Lean Oilfield;
乐安油田草4块沙四段储层沉积特征与非均质性研究
2.
Mesozoic sedimentary characteristics and tectonic evolution in the eastern part of the Qiangtang basin;
羌塘盆地东部中生代沉积特征与构造演化
3.
Sedimentary characteristics of the shallow Jurassic braided river delta,the Junggar Basin;
准噶尔盆地侏罗系辫状河三角洲沉积特征
3)  sedimentary features
沉积特征
1.
Tertiary sedimentary features and environment of the Lanzhou-Minhe basin;
兰州—民和盆地第三纪沉积特征及环境
2.
This paper deals with the sedimentary features of the Mesozoic Fanjiatang coal-bearing strata in the southwestern part of Wuwei county in terms of the composition of rocks,the texture and structure of sediments and fossils Combined with logging curves the early, middle and late periods of sedimentary environment are delimited and coal accumulation law is conclude
从岩石成分 ,沉积物结构、构造、古生物化石等方面对无为县西南部中生代范家塘期含煤地层的沉积特征进行分析研究 ,并结合测井曲线对范家塘早、中、晚三个时期的沉积环境进行划分 ,总结其聚煤规
4)  sedimentary feature
沉积特征
1.
Fan delta sedimentary features and its controls over subtle hydrocarbon reservoirs of Liu-1 Member in Weixinan sag;
涠西南凹陷流一段扇三角洲沉积特征及其对隐蔽油气藏形成的控制作用
2.
On the basis of drilling geology, core analysis and production test data, this paper studies the sedimentary feature and controlling factors of volcanic reservoirs in Kongdian formation of Gaoqing oilfield through measures such as log constrained inversion.
以钻井地质、岩心分析化验及试油资料为依据,采用测井约束反演等技术手段,研究高青油田孔店组火山岩沉积特征及储层发育控制因素;结合油气成藏条件分析,指出该区火山岩油气分布的有利部位,为指导该区火山岩下一步滚动勘探开发提供了地质依据。
3.
To gain a clear idea of the sedimentary environment and its sedimentary feature of a sand body is the basis and key to understanding the heterogeneity, evaluating the exploitation effect and making further adjustment.
搞清砂体的沉积环境及其沉积特征是正确认识其非均质特征、估计其开发效果以及进一步加密调整的基础和关键。
5)  depositional feature
沉积特征
1.
According to the analysis of a large number of rock thin-sections and cast thin-sections,the depositional features,pore structure and rock physical properties of clastic rocks in Yanchang Formation,Triassic system,Changwu Region,Erdos Basin has been researched.
根据大量岩石薄片和铸体薄片分析,对鄂尔多斯盆地长武地区三叠系延长组碎屑岩的沉积特征、储层孔隙结构及岩石物理性质进行了研究,认为延长组砂岩体有利相带为三角洲前缘水下分流河道微相和河口砂坝沉积微相,属于低孔隙度、特低渗透率砂岩储层。
2.
Aim In order to find out depositional feature and distribution law.
目的 了解长6储层的沉积特征,储层的分布规律。
3.
Based on the analysis of sealing core drilling and log analysis, the reservoir type of Sa-0 reservoir in Duanxi of Bei-1 Area in Daqing oil field is identified and the depositional environment and depositional feature of Sa-0 member are studied, the physical property parameters of this reservoir are determined.
分析了密闭取心和测井资料 ,确定了大庆北一区断西萨零组储集层的类型 ,研究了萨零组油层的沉积背景和沉积特征 ,测定了储层物性参数 ,计算了地质储量和可采储量 ;结合试油试采结果 ,阐述了萨零组储层开发的可行性 。
6)  sedimentary characteristic
沉积特征
1.
The study of sedimentary microfacies and facies marker classifications is made by means of sedimentary characteristic of Jurassic Toutunhe formation (J2t2),integrated with well logs and comprehensive logging data.
在岩心详细观察的基础上,结合测井资料及综合录井资料,对石南油气田侏罗系头屯河组J2t2砂层组的沉积特征、相标志、沉积相微相划分进行了研究。
2.
This paper mainly studies the sedimentary characteristics and sedimentary facies,the features of hydrocarbon resource rock,the production time of ejectment hydrocarbon and the condition of movement.
主要对塔里木盆地孔雀河斜坡带寒武—奥陶系的沉积特征和沉积相、烃源岩的特征以及生烃时间、运移条件等进行了研究,认为该地区油气源充足,具备了形成大型油气藏的基础,指出塔东一井东、北、西北一带,其次是群克1井以南地段,是重点寻找寒武—奥陶系油气的远景区块。
3.
This paper studies its genesis,sedimentary characteristic and pattern,spatial distribution and significance in oil field development.
对以往研究较少 ,并在油田勘探阶段及开发初、中期地质研究中被遗漏或忽视的决口水道的成因、沉积特征与模式、空间分布及在油田开发中的意义进行了研究与探讨。
补充资料:沉积相
沉积相
sedimentary facies 

   沉积物的特征及其生成环境的总和。简称相或岩相。沉积相的概念是1838年瑞士地质学家A.格雷斯利(1814~1865)建立的。他认为相有两个要点:①地层单元中的岩石面貌和古生物组合要一致。②在相同的古生物组合中,要明显地含有不同于其他相中的一些生物种属。并认为沉积相反映着沉积物形成地理位置和地理环境。美国学者R.C.莫尔1948年提出沉积相的定义为“沉积相是沉积剖面中任何空间上独立的,与该剖面的其它部分有显著区别的部分”,强调了地层学的概念。苏联学者L.V.鲁欣1958年认为“把相理解为沉积物的特征及其生成环境的总和更加确切”。R.C.塞利1970年主张相可用5个参数来确定,即岩体的几何形态、岩性、古生物、沉积构造和古水流形式。1985年中国学者翟淳把沉积相分为5级。即相组、相、亚相、微相和相素。先根据自然地理条件分为大陆相组、海陆过渡相组和海相组,它们属一级相。再根据自然地理条件的局部变异划分出二级相,如大陆相组分为河流相、湖泊相、沼泽相、冲积扇相、残积坡积相、沙漠相、冰川相;海陆过渡相组分为三角洲相、河口湾相;海相组分为无障壁海岸相、有障壁海岸相、浅海陆棚相、次深海相和深海相。二级相下再分出三级相,或叫亚相,如河流相下再分为河床亚相、堤岸亚相、河漫滩亚相和牛轭湖亚相。再根据微地貌或岩性、古生物特征细分出第四级相,或叫微相,微相下再根据岩性分出若干相素。
   沉积相反映着地质时期地理环境的特征及其演变过程,因此研究它对了解各地质时代古地理环境和地壳的历史演变有着重大的理论意义,对沉积矿产的普查勘探,查明地下水、油、气的分布规律,对工程建设的设计和规划均有重要的实际意义。
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