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1)  sedimentary facies
沉积相
1.
Study on the sedimentary facies of the member 3 and 4+5 of Yanchang Formation in Jiyuan area;
姬塬地区长3—长4+5油层组沉积相研究
2.
Application of the reservoir stochastic modeling in subdividing sedimentary facies;
应用储层随机建模方法细分沉积相
3.
Application of EMI image logging in studying sedimentary facies;
成像测井在沉积相研究中的应用——以克拉玛依油田八区下乌尔禾组为例
2)  depositional facies
沉积相
1.
An analysis of the depositional facies of T_1j_1~2-T_1j~1 and T_1j_1~5 layers of Lower Triassic Jialingjiang Formation in Chishui area
赤水地区下三叠统嘉陵江组嘉二~1—嘉一段及嘉五~1亚段沉积相分析
2.
Diagram of deposition facies in studied area is an important achievement of depositional facies study.
研究区域的沉积相图,是沉积相研究的重要成果。
3.
Detailed studies on sedimentary facies, petrology and diagenesis of the sandstones as well as their impact on reservoir quality evolution show that the reservoir quality is strongly influenced by the depositional facies,development and dimension of fractures, detrital components and diagenesis of the sandstones.
对蟠龙探区上三叠统长2砂岩进行了沉积相、砂岩岩石学和成岩作用及储层物性演化影响等研究,结果表明:其物性受沉积相、裂缝发育程度与规模、砂岩碎屑成分及成岩作用的控制,辫状河河心砂坝中细-细砂岩具有较高的孔隙度(平均13。
3)  sedimentary face
沉积相
1.
The New Conclusion of Sedimentary Face and Distribution Characteristics for Oil & Gas of Cretaceous in Dinan Uplift,Junggar Basin;
准噶尔盆地滴南凸起白垩系沉积相研究新认识及其油气藏分布特征
2.
The sedimentary face was determined by turbidite fan of remote origin through study of lithology,grading analysis and sedimentary structure,etc.
根据岩性、粒度分析、沉积构造等特点,其沉积相为来自南部物源的远岸浊积扇沉积,中扇的辫状水道微相是主要的含油微相。
3.
this paper takes south shoal zone Mesozoic strata and sedimentary faces as the research object .
黄骅坳陷位于渤海湾盆地北部,是叠置在华北地台基底上从中生代发育的裂谷盆地,其南部滩海区也称埕北斜坡带,位于黄骅坳陷歧口凹陷南缘,为埕宁隆起向歧口凹陷过渡的断阶式斜坡区,论文以南部滩海区地层与沉积相为研究对象。
4)  facies [英]['feiʃiiz]  [美]['feʃɪɪz]
沉积相
1.
The Theory and Study on Logging Facies Analysis;
测井沉积相分析方法研究
2.
Sedimentary Facies analysis of Gaqiu Depress
柴北缘尕丘凹陷沉积相研究
3.
Based on core observation,it is thought that not only single fluvial facies sedimentary system but also a set of braid river delta-shallow lacustrine sedimentary system are developed in He2 and He3 Member.
识别并划分了工区内沉积相、沉积亚相、沉积微相。
5)  sedimentary microfacies
沉积微相
1.
Sedimentary Microfacies of the Chang 6 Oil-bearing Formation in Nanzhuang District,Ordos Basin;
鄂尔多斯盆地南庄地区长6油层组沉积微相研究
2.
Research on sedimentary microfacies of the epicontinental sea platform of Jia 2 Member in Moxi Gas Field;
磨溪气田嘉二段陆表海型台地内沉积微相研究
3.
Quantitative discrimination of sedimentary microfacies by use of log data——Taking the Triassic Yanchang Formation in Jiyuan-Baibao region of Ordos Basin for example;
应用测井资料定量识别沉积微相——以鄂尔多斯盆地姬塬-白豹地区三叠系延长组为例
6)  microfacies
沉积微相
1.
A study of depositional microfacies and method of reservoir prediction by integrating well log and seismic information in dense well pattern——taking Xing 56 block,Xingshugang oil field,Daqing as an example;
密井网区井震结合进行沉积微相研究及储层预测方法探讨——以大庆杏树岗油田杏56区为例
2.
Application of microfacies judge technique of grey system based on wavelet analysis in Zhuang 9 Block;
基于小波变换的灰色沉积微相评判技术——以庄9井区为例
3.
Sedimentary characteristics and microfacies of fluvial deposits of mordern Nen River at Damagang area;
现代嫩江大马岗段河流沉积微相划分及其特征
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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